Taphofacies from the lower Eocene Naredi Formation of Kutch Basin, western India, and their significance

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While the formation has been studied from sedimentological, paleontological, and geochemical perspectives, taphonomy remains largely unexplored. This study presents a novel classification of sedimentary rocks based on the taphonomic characteristics of embedded fossils, with the focus on Larger Benthic Foraminifera and Mollusca. Six Taphofacies are identified using the following criteria: fragmentation, imbrication, diagenetic alteration, type of preservation and packing, distribution of sizes, bioturbation, and articulation. The taphofacies, along with a detailed study of the existing horizons, indicate a more intricate depositional picture of the Naredi Formation than previously recognized. Notably, five transient regressive phases are identified, four of which coincide with Taphofacies C, marked by evaporite presence and lagoonal restriction, challenging earlier interpretations of a single transgressive–regressive cycle. Taphonomic evidence also captures intra-horizon variability, including current-induced fragmentation in middle ramp deposits, microbial micritization of LBF tests, and soft-sediment deformation features. Overall, the integration of taphonomic, sedimentological, and paleontological data refines the lagoonal-to-open marine depositional model and highlights the utility of taphofacies analysis as a tool for reconstructing palaeoenvironmental and diagenetic histories. Geology Climate Analysis and Modeling Taphofacies taphonomy larger benthic foraminifera Naredi Formation Eocene Kutch Basin Figures Figure 1 Figure 2 Figure 3 Figure 4 Figure 5 Figure 6 Figure 7 Figure 8 Figure 9 Figure 10 Figure 11 1. Introduction Taphofacies analysis is crucial in interpreting ancient environments because it captures the full spectrum of post-mortem processes affecting fossils, offering insights that go beyond traditional sedimentological and taxonomic approaches. A taphofacies is defined as a body of sedimentary rock distinguished from surrounding units by its unique suite of taphonomic properties (Boessenecker et al., 2014 ), reflecting both pre-burial processes—such as bioerosion, disarticulation, transport, fragmentation, and post-burial changes like compaction, mineral replacement, fossil dissolution, and reworking. These combined processes imprint distinct signatures on fossil assemblages, enabling the identification of specific fossil-bearing horizons that correspond to past depositional environments. Despite its potential, this method remains underutilized in key paleogeographic regions such as the Indian subcontinent. So, this study tests the hypothesis whether systematic variations in the taphonomic characteristics of larger benthic foraminifera and associated mega-invertebrates within the Naredi Formation correspond to distinct depositional settings, allowing the differentiation of taphofacies that can serve as independent indicators of paleoenvironmental conditions. This leads to answering the question: Can taphofacies analysis of the Naredi Formation in the Kutch Basin provide a reliable and independent framework for reconstructing paleoenvironmental settings beyond traditional lithological and taxonomic methods? The Kutch Basin in western India, a pericratonic rift basin (Fig. 1 ), bounded by three faults with a well-preserved Cenozoic sequence, including the fossil-rich lower Eocene Naredi Formation, presents an ideal case for applying taphofacies analysis. The goal is to establish a taphofacies framework that serves as an independent proxy for reconstructing paleoenvironmental conditions, ultimately enhancing and refining existing interpretations based on lithology and fossil taxonomy. Global studies show the importance of taphonomy in paleoenvironmental interpretation. Beavington-Penney ( 2004 ), Nebelsick et al. ( 2011 ), and Ćosović et al. ( 2012 ) linked taphonomic features to transport, facies variation, and carbonate platform architecture. Lipps ( 1988 ) and Loubere and Gary ( 1990 ) highlighted biological and post-burial alterations in foraminifera through taphonomy. Babazadeh and Alavi ( 2013 ) and Tomassetti and Benedetti ( 2020 ) used microfacies and reworked assemblages to reconstruct Eocene carbonate systems. Despite India’s key Paleogene role, such frameworks are lacking. This study of the Naredi Formation helps fill that gap. The Eocene succession of Kutch is well-studied for stratigraphy, sedimentology, and paleontology. Wynne (1872) was the first to study the Cenozoic rocks of Kutch Basin. Biswas ( 1965 ) did a detailed mapping along with the stratigraphy of the basin. Further studies were conducted in the subsequent years to establish a formal stratigraphy and time correlation by Biswas and Raju ( 1971 , 1973 ) and Biswas ( 1971 , 1973 , 1977 , 1992 ). The Eocene fauna, including foraminifera, vertebrates, and invertebrates, is quite well studied (for example, Kumar and Sahni, 1986 ; Bajpai and Thewissen, 2000 ; Sengupta et al., 2011 ; Keller et al., 2013 ; Halder and Sinha, 2014 ; Khanolkar and Saraswati, 2019 ; Banerjee et al., 2019 ; Halder and Das, 2019 ; Chakraborty and Sengupta, 2023 ). Previous workers have also done substantial work on sedimentology, stratigraphy, and sequence stratigraphy (for example, Sarkar et al. 2012 ; Saraswati et al. 2016 , 2018 ; Catuneanu and Dave 2017 ; Srivastava and Singh, 2017 ; Srivastava et al., 2019 ; Banerjee et al., 2018 ; Srivastava and Singh, 2019 ; Srivastava et al., 2022 ). However, hardly any work has been done on the biota's taphonomy present in the Kutch Basin's Cenozoic deposits. The Eocene rocks of the Kutch Basin predominantly represent marginal marine to open marine settings and are well exposed near Baranda, Nareda, Harudi, and Lakhpat. The Naredi Formation, especially well developed near Nareda village (23°34'32.6"N, 068°38'36.2"E), consists of near-horizontal beds exposed as vertical sections along shallow river valleys. North of Harudi village, a river section marks the contact between the Naredi and overlying Harudi Formations. The lower part of the Naredi Formation comprises green, grey, and brown shales with intercalated gypsum layers, while the upper part includes foraminiferal limestones and ferruginous claystone (Biswas, 1992 ; Srivastava and Singh, 2017 ). Following Biswas ( 1992 ), the formation has been divided into three members: a Gypseous Shale Member (grey, brown, green shales and concretions with interlayered gypsum), an Assilina Limestone Member (dirty white limestone and marl), and a Ferruginous Claystone Member (brown and grey claystones, and a red laterite bed capping the sequence). However, a revised and more detailed litholog (Fig. 2 ) was constructed based on new field observations and fossil content to support the taphofacies analysis. As the uppermost horizons are barren, the present study focuses exclusively on the fossiliferous interval from the base to the topmost Assilina -bearing horizon. 2. Materials and Methods The Naredi Formation has been studied at two locations in and around the type section (23° 34' 32.6" N, 068° 38' 36.2" E) to revise the lithology and study the taphofacies. Three other locations near the type section of the Harudi Formation (23° 31’27.0” N, 068° 41’11.0” E) were also studied to complete the lithology of the topmost part of the formation (above the Assilina limestone) as shown by black dots in Fig. 1 . Rock samples were collected at 1-meter intervals because the exposure in these sections was continuous, with a generally homogeneous lithology. The majority of the formation comprises shale, with a gradual transition to limestone and ferruginous claystone towards the top. Most of the beds in the studied sections range from 1 to 4 meters in thickness, making a 1-meter interval an effective resolution for capturing vertical variations without oversampling. This sampling resolution also allowed for consistent recording of key sedimentary features, such as thin gypsum interlayers within the shale, as well as subtle changes in rock colour and fossil occurrence. In cases where individual beds were thinner than 1 meter, samples were taken from both the base and top of the unit to ensure internal variation was documented. Limestones have been named according to the Dunham classification of rocks (Dunham, 1962 ). The rock samples were sent to Lab Crystals, Lucknow, Uttar Pradesh, India, for the preparation of slides. A total of 29 thin sections were prepared from separate rock samples collected across different fossiliferous horizons of the Naredi Formation (Fig. 2 ). These thin sections collectively represent approximately 5 meters of fossiliferous intervals distributed across key horizons within the 25 m thick succession (marked in Fig. 2 ). Of the 29 thin sections, 5 measured 26 × 47 mm and the rest 50 × 75 mm, as the splintery green shale prevented preparation of larger thin sections. In cases where a single fossiliferous horizon was laterally extensive, samples were taken about 10 meters apart to capture lateral variation, with each thin section representing a unique point and not repeated from the same rock sample. Thin sections were examined under a Leica DVM6 M digital microscope to study the internal and external taphonomic features of foraminifera, which require microscopic analysis due to their small size. In contrast, horizons containing only macrofossils were studied using hand specimens, also from rock samples at an interval of 10 meters apart to capture the lateral variation, as their larger size allowed for detailed observation without thin-sectioning. Fossil extraction for hand specimen studies was carried out with great care to minimize damage to specimens. Only parts of the horizons where fossils could be retrieved without the use of chemical treatments were selected for extraction. Mechanical methods were limited to gentle techniques, using distilled water, a small hammer, and a fine chisel when necessary to dislodge fossils from the matrix. This approach ensured the preservation of delicate taphonomic features critical to the analysis. And if samples got damaged during extraction, even after extreme caution, they have been studied accordingly. Taphonomic attributes such as fragmentation, test shape, and wall alteration were assessed in both thin sections (microscopic scale) and hand specimens (macroscopic scale). Figure 2 shows the sampling levels and represents the composite litholog of the Naredi Formation. SEM (Scanning Electron Microscope) studies were conducted on the thin sections of rocks and fossil specimens at the Geology Department, Presidency University, Kolkata, West Bengal, India. Taxonomy, diversity (the increase or decrease in the number of different groups of fossils occurring within a bed per unit area), and sedimentological characters have been considered for an accurate interpretation of the environment of deposition. The taphonomic changes occurring in the fossiliferous layers and the changing environment were also recorded. Different taphonomic features have been observed within the fossiliferous rock units of the Naredi Formation of Kutch Basin, India. The major characters used to describe each taphofacies include: Fragmentation – The level of fragmentation in foraminifera and Mollusca has been divided into Stages 0–3. Stage 0 corresponds to an intact fossil, and the level of fragmentation increases from Stage 1 to Stage 3. Figure 3 gives a pictorial description of the different stages. This feature is also calculated as a percentage, showing how many of the total number of fossils are fragmented in each taphofacies and comprises a pre-burial feature. Articulation – This pre-burial character is only applicable for bivalves and has been calculated as the percentage of the total bivalves found in an articulated state. An articulated bivalve has both valves joined together. Abundance – This feature is studied by calculating the total number of fossils in a designated area. Fossil abundance was calculated per unit area (cm²) using both exposed surfaces of rock slabs and thin sections, allowing detection of both larger and smaller fossils. While volumetric estimates would have been ideal, the hard matrix and fossil composition made fossil separation and chemical treatments ineffective. Thus, area-based counts provide a more consistent and reliable measure. There are three grades – Low ( 4 fossils per sq cm). The unitary method was used to standardize fossil counts to a common unit area, enabling accurate abundance comparison across uneven sampling areas. Throughout the Naredi Formation, there is a wide variation in the abundance of fossils. In some of the taphofacies, variation is observed even within a single fossiliferous horizon. Mineral alteration – This character includes sparitization and micritization of fossils. Micritization occurs syndepositionally and in the early stages of burial and is biogenic. It alters the fossils by weakening the test walls in fossils such as foraminifera, often contributing to fragmentation. Micritization has been divided into 3 stages: Stage 0 – No micritization, Stage 1 – Partial wall micritization with infilled chambers, Stage 2 - Heavy micritization with internal structures obscured. Sparitization occurs post-depositionally in early to late stages of diagenesis due to compaction, fluid movement, and chemical alteration. It has also been divided into 3 stages: Stage 0 – No sparitization, Stage 1 – Slight recrystallization, wall textures preserved and chambers infilled, Stage 2 – Majority of the test recrystallized, internal structure obliterated. Special characters – Features such as soft sediment deformation (a post-depositional but pre-lithification process) and concretion formation (a post-burial process) were also recorded. These processes can distort fossil orientation, enhance fragmentation, or create localized zones of diagenetic overprint. Imbrication of fossils – This character indicates the orientation of the fossils within a litho unit (1 & 2 – pre-burial feature, 3 - post-depositional but pre-lithification feature). The observed fossil orientations in this study include: (1) a unidirectional, layer-parallel alignment of specimens; (2) a bidirectional, layer-parallel orientation corresponding to cross-laminated structures; and (3) a concentric or swirl-like pattern indicative of localized hydrodynamic vortices or soft sediment deformation. Diversity and Assemblage – Diversity is known to increase from a lagoonal to an open marine setting. A qualitative study on diversity gives a better insight into the environment of deposition of the taphofacies. In this study, the diversity measurement has been taken as the number of species per cm². If only the genus could be identified for a fossil group, it was considered Genus sp. to avoid bias. And this data has been generated by studying area grids in hand specimens (10 x 10 cm 2 for Taphofacies A and C, whereas a 2.5 x 2.5 cm 2 for Taphofacies B, D-F due to the difference in size and distribution of fossils). Diversity has then been standardized and represented as species per cm². Studying the fossil assemblage is a key element in understanding the paleoenvironment because certain organisms can only survive in specific environmental conditions. For example, Assilina occurs only in warm shallow marine environments (Dinçer, 2016 ); it cannot be found in lagoonal or brackish water conditions. Table 1. Major characteristics of six identified taphofacies within the Naredi Formation, Kutch Basin, India Size and shape of the fossils – Fossil shape and size were assessed using both hand specimens and petrographic thin sections. Given the consistent orientation of the fossils, thin sections were prepared to capture vertical cross-sections for measurement. To validate the accuracy of these measurements and account for potential sectional bias, complementary measurements were also obtained from loose specimens that could be dislodged from the fossiliferous litho units. 3. Taphofacies of the Naredi Formation The Naredi Formation has been subdivided into six distinct taphofacies (A–F) based on a combination of taphonomic attributes such as fragmentation, micritization, biofabric, fossil articulation, spatial arrangement, and associated sedimentological features. These taphofacies represent specific microenvironments within the broader transition from a lagoonal to a middle ramp setting. The defining characteristics of each taphofacies are summarized in Table 1, and detailed descriptions are provided below. 3.1. Taphofacies A: The lower part of the Naredi Formation contains two fossiliferous concretionary horizons, approximately 0.4 m and 0.2 m thick (Fig. 2 ), composed of fossil-bearing grey and brown limestone concretions embedded within shale, with gypsum interlayers. These concretions exhibit concentric colour changes, typically light brown at the margins, transitioning to darker brown or grey toward the centre. A total of 37 individual molluscan specimens were studied from nine concretions, showing low diversity (0.01 species per cm 2 ) and low abundance, dominated by Corbula (bivalves) and rarely Turritella (gastropods). Taphonomic data indicate that 78.4% of the fossils are fragmented (stages 1 & 2, Fig. 3 ), and 47% of bivalves remain articulated. In this taphofacies, some bivalves show fragmentation even in their articulated form, which may reflect post-mortem compaction within partially cemented concretions, rather than transport-induced breakage. Fragmented shells, both articulated and disarticulated, are more common near the concretion margins (Fig. 4 a–b), while intact, articulated bivalves are typically found at the centers (Fig. 4 c). Turritella are usually intact and located near the periphery (Fig. 4 d). A bimodal size distribution is observed, with both large (avg. 42.9 mm) and small (avg. 9.3 mm) specimens occurring at both core and margin positions. Turritellids are often found in shallow marine habitats but also in very shallow (i.e., marginal marine) and deep marine environments (Scholz et al., 2024). However, the presence of low-diversity, low-abundance assemblages dominated by Corbula , a taxon tolerant of brackish, low-oxygen conditions (Anderson & Roopnarine, 2003 ; Naugolnykh, 2017 ), supports deposition in a marginal marine to restricted lagoonal setting. Table 1 outlines the taphofacies characteristics. 3.2. Taphofacies B: In the lower part of the Naredi Formation, two glauconitic green shale horizons (~ 0.2 m thick each) occur, interlayered with gypsum and clay showing cross-laminations (Fig. 2 , Fig. 5 ). These beds contain high glauconite pellet content, visible in both thin sections and SEM and exhibit variable pellet maturity (Srivastava & Singh, 2017 ). Fossils comprise of Nummulites and disarticulated molluscan shells, with occasional coral fragments, and show moderate abundance with Stage 1 sparitization, and moderate diversity (0.64 species per cm 2 ). A total of 273 fossils were recorded for taphonomic studies from these horizons, including 230 Nummulites (84.2%), 39 molluscs (14.3%), and 4 coral/unknown fragments (1.5%). 219 fossil specimens were documented in thin sections, while 54 specimens that could be extracted from rock samples were examined using high-magnification microscopy (Leica DVM6 M). Nummulites are well preserved, with 96.5% showing Stage 0 fragmentation, while molluscs are heavily fragmented and disarticulated (Stages 2–3), with only 12.8% intact. The molluscs include probable corbulids, known for inhabiting low-energy marginal marine environments (Anderson & Roopnarine, 2003 ). Overall fragmentation is 16.8%, and fossil size distribution is bimodal, with smaller Nummulites (avg. 0.8 mm) and larger mollusc fragments (avg. 1.3 mm). The lens shape of Nummulites (as observed in hand specimens, as well as in thin sections) provides hydrodynamic stability and resistance to fragmentation, while the larger, curved molluscan shells were more prone to mechanical breakage (Tasdemir, 2009 ). This is consistent with studies showing that larger bioclasts have a higher likelihood of fragmentation under hydraulic stress (Kidwell & Flessa, 1995 ). Fossils exhibit bidirectional paleocurrent imbrication matching the direction of cross-lamination, indicating bottom currents and limited post-mortem transport. The green shale’s colour and the abundance of glauconite pellets indicate a phase of reduced siliciclastic sedimentation, a key condition for glauconitisation (Odin & Matter, 2003 ; Amorosi, 1997 ). Such conditions typically arise during marine transgressions, when sediment input slows relative to accommodation space, allowing prolonged residence time necessary for glauconite formation. The interbedded gypsum layers further support low sedimentation and episodic restriction, suggesting deposition in a marginal marine to inner shelf setting under periodically evaporitic conditions (Srivastava & Singh, 2017 ). The fossil assemblage in this horizon reinforces the transgressive interpretation. The dominance of well-preserved, low-fragmentation Nummulites , particularly N. burdigalensis burdigalensis and N. globulus nanus , which are known from transgressive, mid-shelf to lagoonal settings (Racey, 2001 ; Keller et al., 2014; Shahzad et al., 2024), supports deposition under open but shallow marine conditions. Molluscan taphonomy, characterized by higher fragmentation and low articulation, alongside features such as cross-laminations and imbricated bioclasts, indicates intermittent higher-energy events that may have accompanied early stages of transgression. Therefore, the glauconite-bearing horizon reflects a transgressive surface, likely representing a temporary sediment starvation phase within a shallow marine lagoonal system. The presence of interbedded gypsum points to episodic restriction and hypersalinity (Srivastava and Singh 2017 ), suggesting fluctuating connectivity with the open marine system during early transgression. 3.3. Taphofacies C: This taphofacies is defined by brown shale horizons containing sporadic, low-abundance mollusc shells and interlayered gypsum (Fig. 7 a–b). Four such horizons, measuring approximately 3.5 m, 2.0 m, 1.8 m, and 1.5 m in thickness (in ascending stratigraphic order), exhibit horizontal planar lamination and a splintery texture—features indicative of restricted, low-energy depositional conditions. An additional 0.8 m thick horizon near the base of the formation comprises grey-brown shale with patchy, poorly developed gypsum and similarly sporadic mollusc shells. A total of 45 mollusca fossils were recorded in the field, averaging 2.3 cm in length. Only seven were recovered intact; the rest disintegrated during extraction due to their fragile preservation. Prior to collection, outlines of all specimens were measured in situ, revealing that 95.5% (43 out of 45) were already fragmented. The surviving shells display Stage 1 fragmentation (Fig. 3 ), with consistent breakage along exposed edges, suggesting weathering as the primary agent rather than post-mortem transport. Despite this, the shells remained articulated, reinforcing deposition under calm, low-energy conditions. Taxonomic identification was limited due to fragmentation, low abundance, and low diversity (0.01 species per cm 2 ), though some specimens could be assigned to Corbulidae. The presence of thick continuous laminated gypsum interlayers within four of the five brown shale horizons (Fig. 7 a) strongly supports episodic regression and evaporitic conditions typical of a restricted lagoonal environment. These gypsum layers reflect increased salinity under evaporative stress; conditions commonly associated with sea-level fall and reduced circulation. The repeated alternation of shale and gypsum suggests cyclic changes in salinity and water depth, driven by frequent sea-level fluctuations. This interpretation partially aligns with previous findings by Srivastava and Singh ( 2017 ), who reported a single gypsum-bearing shale horizon in the Naredi Formation and interpreted it as evidence of lagoonal regression. In contrast, the current study identifies five such horizons, of which four contain bioclasts and are assigned to Taphofacies C. This expanded dataset indicates that the Naredi Formation recorded at least five distinct regressive episodes. However, the fifth gypsum-bearing shale horizon does not contain bioclasts and is thus excluded from Taphofacies C. Furthermore, the grey-brown shale horizon near the base of the formation, with its sparse and patchy gypsum, presents a more complex case. The nature of gypsum in this interval – thin, poorly laminated, and irregularly distributed, raises the possibility of a diagenetic origin rather than primary evaporitic deposition. Such gypsum may have formed through brine seepage along weathered fractures or by dissolution and reprecipitation from underlying grit beds, as suggested by Gontharet et al. ( 2007 ). This possibility introduces an important caveat: while well-laminated gypsum layers within shale are reliable indicators of depositional regression, secondary gypsum should not be interpreted as evidence of sea-level fall without additional supporting data. In summary, the combination of brown shale with laminated gypsum, the presence of sporadic and fragmented but articulated mollusc shells, low species diversity, and the overall sedimentary context suggests a restricted, low-energy lagoonal environment. 3.4. Taphofacies D: Two concretionary horizons, measuring approximately 0.2 m and 0.25 m in thickness, are identified in the studied section (Fig. 2 ). The lower concretion layer overlies a yellow shale. It underlies Taphofacies A, while the upper horizon is embedded within the Assilina Limestone, corresponding to Taphofacies F. Both layers are dominated by Assilina tests, which are preferentially concentrated along the rims of the concretions (Fig. 8 a–d), showing high abundance. However, the fossil abundance decreases toward the ferruginous cores. A total of 1018 foraminifera were recorded from these horizons, comprising 1010 Assilina and 8 Nummulites specimens. Overall, 36.25% of the total foraminifera exhibit fragmentation (Stages 1–3). Fragmentation likely began through hydraulic transport and was later augmented or preserved by microbial micritization (Stage 1), which weakened the test walls (Garuglieri et al., 2024 ; Messadi et al., 2019 ), often seen in inner ramp settings. These weakened walls may have further fractured under compaction during early burial, although micritic infilling also contributed to partial test preservation. Of the fragmented Assilina , 93.75% exhibit micritization. Even among unfragmented tests, 61.68% of forams show micritization, and 38.32% display a combination of micritization and sparitization (Stage 1), underscoring the significant diagenetic role of micritization in this taphofacies (Fig. 8 c–d). The foraminiferal assemblage is of low diversity (0.32 species per cm 2 ) but high abundance (at the rim of the concretions), comprising primarily Assilina laxispira and rare Nummulites spp. The presence of Assilina , which typically inhabits warm, shallow inner to middle ramp environments (Dinçer, 2016 ; Khan et al., 2024 ), alongside micritization features (Messadi et al., 2019 ), supports deposition in a shallow marine setting. However, the ferruginous cores of the concretions, interpreted to result from early diagenetic iron precipitation in marginal marine conditions, indicate post-depositional modification. Such concretions likely formed through microbial mediation under suboxic conditions, where iron was mobilized in pore waters and subsequently precipitated due to localized redox changes (Raiswell, 1971 ; Mozley & Davis, 2005 ). The micritic envelopes around the Assilina tests may have acted as diffusion barriers, promoting differential iron precipitation and explaining the fossil concentration at concretion margins. This geochemical zonation reflects diagenetic overprinting of originally shallow marine sediments by iron-rich pore fluids during early concretion growth. 3.5. Taphofacies E: Taphofacies E is characterized by a 1 m-thick, splintery, impure lime-rich brown shale horizon underlying a massive Assilina -bearing limestone (Taphofacies F; Fig. 9 a). The fossil assemblage includes Assilina , Nummulites , bivalves, corals, and ostracods, with an overall increase in diversity compared to underlying units. The basal part of the horizon exhibits unidirectional fossil imbrication. In contrast, the top of the sequence shows prominent bidirectional imbrication, indicating an increase in the hydraulic energy towards the top. This change is also evident in the higher percentage of fragmented fossils and the dominance of Stage 2 fragmentation in the upper part of the horizon. Fossil abundance is moderate, with evidence of Stage 1 micritization and early sparry cementation. A total of 717 fossils were studied from thin sections and hand specimens, of which Assilina dominates (546 specimens, 76.15%), followed by bivalves (87, 12.13%), Nummulites (49, 6.83%), ostracods (24, 3.35%), corals (9, 1.25%), and two unidentified specimens (0.29%). Fragmentation is prevalent (63.18%), with bivalves and corals exhibiting complete fragmentation (100%), Assilina showing 63.2%, Nummulites 24.5%, and ostracods remaining intact. Fragmentation stages 1 and 2 are observed in foraminifera and molluscs (Fig. 3 ). Notably, 58.9% of the fragmented foraminifera exhibit Stage 1 micritization. In contrast, mollusca shells show minimal endolithic activity (Stage 0), likely due to differing shell microstructures and taphonomic pathways. Some Assilina tests display sparry recrystallization concentrated within the pillar structures between chambers (Fig. 9 b–c), a feature specific to Assilina subspinosa (Gazi et al., 2015) while A. laxispira does not show this character. Pillars are vertical internal supports composed of fine-grained high-Mg calcite, originally more porous than the surrounding test walls (Sengupta and Mukhopadhyay, 2008 ; Loeblich and Tappan, 2015 ). Their porosity and elevated surface area enhance susceptibility to diagenetic alteration, resulting in early sparitization recognized by their clear, coarse crystalline structure. The presence of spar within originally porous high-Mg calcite pillars, while the surrounding wall micrite remains unaltered or only micritized, supports a diagenetic overprint, likely associated with marine or shallow burial cementation phases (Flügel and Munnecke, 2010 ). The increased faunal diversity (0.96 species per cm 2 ) in this horizon compared to the previous taphofacies, along with the dominance of flattened forms and presence of current-aligned bioclasts, indicates deposition in a well-oxygenated, shallow marine environment transitioning from restricted lagoonal conditions below. Such a setting corresponds with inner to middle ramp depositional environments as interpreted for Assilina (Khan et al., 2024 ; Dincer, 2016; BouDagher-Fadel, 2008). The bidirectional imbrication, matching cross-lamination in host sediments, further confirms current action as a major agent in fossil orientation and partial fragmentation. These taphonomic and sedimentological features collectively support an interpretation of deposition on the inner ramp, under increasing energy conditions in open marine setting with intermittent hydrodynamic reworking. 3.6. Taphofacies F: Taphofacies F comprises three massive, Assilina -dominated limestone horizons measuring approximately 1 m, 2 m, and 1 m in thickness, respectively. These horizons range texturally from wackestone to grainstone (Fig. 2 ) and display pinch-and-swell structures (Fig. 10 a–b). Associated faunal components include Nummulites , molluscs, and corals (Fig. 10 – 11 ). The fossil diversity is 0.8 species per cm 2 , and the abundance of fossils is variable (moderate to high), as established through both loose specimen collection and thin-section analysis, and it varies from moderate to high. The lowermost horizon is separated from the two upper ones by a brown shale interlayer containing gypsum, corresponding to Taphofacies C, interpreted as a lagoonal shallowing phase. All horizons are well-exposed and accessible in the type section of the Naredi Formation. A total of 2,348 fossils were documented from this taphofacies. Of these, 2,272 (96.76%) are Assilina , 67 (2.85%) are Nummulites , two are molluscs, and two specimens remained indeterminate under microscopic observation. Additionally, three coral hand specimens were recovered (Fig. 10 c), though corals were not observed in thin sections. Fossil fragmentation is observed in 34.67% of all specimens, with 35.61% of Assilina (809 out of 2,272) showing varying stages 1–3. Nummulites are consistently intact, while coral preservation is poor. Among the fragmented Assilina tests, 75.4% (610 specimens) show micritization and sparitization corresponding to stages 1 and 2. Abundance increases vertically within each horizon, transitioning from low at the base to high towards the top, correlating with the facies change from wackestone to grainstone. Fragmentation intensity also varies vertically: stages 2 and 3 are predominant near the base, while stages 1 & 2 dominate the upper intervals (Fig. 3 ). Laterally, the two upper limestone horizons exhibit a decrease in foraminiferal abundance and a facies shift from grainstone to wackestone towards the northwest along strike. Species-level identification reveals the presence of Assilina exponens (Sowerby, 1840 ) and Assilina subspinosa (Gazi et al., 2015) (Fig. 10 b & 10 d) Test orientation data show two distinct patterns. In the upper portions of the horizons, fossil alignment follows a bidirectional imbrication (Fig. 11 a), indicative of unidirectional current regimes, which are responsible for the test fragmentation. In contrast, the lower parts exhibit disordered, swirl-like arrangements (Fig. 11 b), reflecting localized soft sediment deformation, which suggests initial breakage due to hydraulic currents and subsequently due to soft-sediment deformation. SEM analysis reveals pyrite crystallization within some molluscan shells, suggesting microbial mediation supported by earlier works such as Folk ( 2005 ) and MacLean et al. ( 2008 ). The dominance of Assilina , coupled with increased biodiversity relative to the underlying lagoonal facies, suggests a transition from a restricted marginal marine environment to an open marine ramp setting. The variation in fragmentation, abundance, and sediment texture supports fluctuating hydrodynamic energy conditions, consistent with an environment shifting between middle and inner ramp settings. 4. Discussion The taphonomic features preserved across the Naredi Formation reflect a progressive transition from a restricted lagoonal setting to more open, higher-energy inner to mid-ramp depositional environments. This is evidenced by systematic changes in fossil assemblages, test preservation, sedimentary fabrics, and associated diagenetic modifications. Taphofacies A–C are dominated by molluscan taxa (e.g., Turritella , Corbula ), while Taphofacies D–F witness a marked dominance of larger rotaliid foraminifera such as Assilina and Nummulites , along with corals, ostracods, and bivalves. This upward diversification points to a transgressive trend marked by deepening water and increasing openness of the depositional environment. The interpretation of this transgression independently anchors glauconite occurrence to sedimentary condensation and slow sedimentation (Odin & Matter, 1981) while separately using the fossil assemblage composition and diversity trends as indicators of environmental shift. However, the presence of gypsum layers within Taphofacies C marks a significant departure from this deepening trend, recording short-lived regressive pulses or localized evaporitic conditions with elevated salinity, likely within a restricted lagoonal setting under semi-arid climatic influence. Such phases reflect relative sea-level fluctuations or climatic oscillations superimposed on long-term marine inundation. Fragmentation intensity varies across the succession, serving as a key taphonomic indicator. Importantly, fragmentation does not correlate linearly with increasing or decreasing water depth. For example, in Taphofacies B, which records evidence of current action, shows incredible preservation of Nummulites but fragmented Mollusca fossils. This suggests that fragmentation is governed not solely by water depth or energy conditions, but also by intrinsic properties of the bioclasts such as test shape, shell thickness, and internal architecture. The hydrodynamically stable Nummulites were less prone to mechanical damage, unlike the thin-shelled and bivalves. Shells of bivalves tend to separate shortly after death when the adductor muscles decay and the valves open, making them more prone to damage. So, while fragmentation is often used as a proxy for energy regimes (e.g., wave or current action), it is essential to interpret it in conjunction with other indicators such as test robustness, biotic activities, and overprinting by diagenetic processes. Overall, inner to middle ramp settings show better fossil preservation, with more intact and micritized tests, compared to the lagoonal facies dominated by disarticulated and poorly preserved specimens. Concretions in Taphofacies A and D display contrasting formation mechanisms, reflecting distinct early diagenetic conditions. In Taphofacies A, carbonate concretions formed through concentric precipitation around small organic or skeletal nuclei, preserving fossils within the concretions. These patterns suggest early porewater-driven carbonate cementation, where favorable microenvironments promoted rapid mineral precipitation, which encapsulated fossils rapidly (Marshall & Pirrie, 2013 ). The thick-walled, high-spired Turritella shells were more resistant to post-burial damage than the thinner-shelled Corbula (Kidwell, 1991 ; Fürsich & Oschmann, 1993 ; Savazzi, 1991 ). The co-occurrence of both articulated and fragmented bivalves suggests time-averaging or short-term reworking prior to concretion growth (Kidwell & Flessa, 1995 ). In contrast, concretions in Taphofacies D, embedded within Assilina -dominated packstones, are ferruginous and likely formed under suboxic conditions via microbial mediation, where iron was mobilized in pore waters and precipitated due to redox gradients (Raiswell, 1971 ; Mozley & Davis, 2005 ). The concentration of micritized Assilina tests at concretion margins suggests that micritic envelopes acted as diffusion barriers, facilitating localized iron enrichment. Concretions in Taphofacies A (lagoonal) formed through early carbonate cementation around molluscan shells in low-energy settings, while those in Taphofacies D (inner ramp) are ferruginous and microbially mediated, reflecting diagenesis around micritized Assilina . Micritization of foraminiferal tests, especially in Taphofacies D-F, is interpreted as a result of microbial endolithic activity, often mediated by microborers in well-lit, shallow marine settings (Burchette & Wright, 1992 ; Messadi et al., 2019 ; Garuglieri et al., 2024 ). While micritization is not exclusive to inner ramp settings, as it can occur wherever microbial colonization is active in the photic zone, it is most common in stable, low-sedimentation areas with prolonged seafloor exposure (Flügel, 2010 ). The inferred suboxic to hypersaline conditions evidenced by glauconite formation and gypsum deposition in Taphofacies A-C may have inhibited the activity of endolithic microorganisms that require stable, oxygenated substrates for bioerosion (Flügel, 2010 ; Macintyre et al., 2000 ). Additionally, the spatial distribution of fossil concentrations and swirl-like arrangements of Assilina and molluscs in Taphofacies F suggests soft sediment deformation, likely driven by liquefaction or fluidization due to seismic or hydrodynamic disturbance (Owen, 1996 ), since there is no evidence of bioturbation. The results of this study substantiate previous interpretations of the Naredi Formation as a lagoonal to middle ramp depositional system (Keller et al., 2013 ; Khozyem et al., 2013 ; Srivastava & Singh, 2017 ), while offering a more detailed reconstruction through the application of taphonomic criteria. Earlier studies in the Kutch Basin primarily focused on sedimentary facies, microfacies, and biofacies (e.g., Khanolkar & Saraswati, 2019 ), with limited integration of taphonomic processes. The findings of this study show strong parallels with previous global research in both methodology and interpretation. Like Beavington-Penney ( 2004 ), Nebelsick et al. ( 2011 ), and Ćosović et al. ( 2012 ), the Naredi Formation exhibits systematic relationships between taphonomic features such as fragmentation, abrasion, and micritization and depositional energy gradients, supporting their model of facies-linked taphonomic variability. The occurrence of micritization restricted to the middle ramp settings in this study mirrors the energy-controlled micritization patterns observed in their work. Similarly, the selective preservation of foraminiferal tests and their micritic overprinting across facies aligns with the biological and post-burial alteration processes highlighted by Lipps ( 1988 ) and Loubere & Gary ( 1990 ). Consistent with the approaches of Babazadeh & Alavi ( 2013 ) and Tomassetti & Benedetti ( 2020 ), this study integrates taphonomic observations with microfacies analysis to interpret cyclic sedimentation and platform evolution during the Eocene, reflecting a comparable level of resolution in reconstructing shallow marine carbonate systems. Furthermore, the identification of Assilina -rich assemblages showing bidirectional imbrication and specific test orientations in the Naredi Formation supports the interpretations by Jorry et al. ( 2006 ), Hadi et al. (2016), and Zohdi et al. ( 2013 ), who associated similar features with storm reworking, wave energy influence, and transport directionality on carbonate ramps. Overall, the present study confirms and extends these global findings, enhancing the comparative understanding of Eocene ramp systems. These findings not only position the Naredi Formation within global Paleogene carbonate ramp models but also offer a novel methodological contribution to Indian Eocene paleoenvironmental studies. 5. Conclusion This study provides the first comprehensive taphonomic analysis of the Naredi Formation, revealing a complex interplay of depositional environments, early diagenetic processes, and fossil assemblage dynamics. Through detailed evaluation of fragmentation, micritization, bioturbation, and bioclast arrangements, six distinct taphofacies have been identified that record a transition from a restricted lagoon to a more open marine ramp setting. The identification of five regressive phases and novel taphonomic features such as imbrication and soft sediment deformation significantly refines the paleoenvironmental interpretation of the Eocene in the Kutch Basin and establishes a new baseline for regional and global comparisons of Paleogene carbonate systems. 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Memoir on the Geology of Kutch, to accompany the map compiled by AB Wynne and F. Fedden during the season, 68, 1868-1869. Zohdi, A., Mousavi-Harami, R., Ali Moallemi, S., Mahboubi, A., & Immenhauser, A. (2013). Evolution, paleoecology and sequence architecture of an Eocene carbonate ramp, southeast Zagros Basin, Iran. GeoArabia, 18(4), 40-80. DOI: https://doi.org/10.2113/geoarabia180449 Additional Declarations The authors declare no competing interests. Cite Share Download PDF Status: Published Journal Publication published 24 Sep, 2025 Read the published version in Facies → Version 1 posted You are reading this latest preprint version Research Square lets you share your work early, gain feedback from the community, and start making changes to your manuscript prior to peer review in a journal. As a division of Research Square Company, we’re committed to making research communication faster, fairer, and more useful. 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Also discoverable on Platform About Our Team In Review Editorial Policies Advisory Board Help Center Resources Author Services Accessibility API Access RSS feed Manage Cookie Preferences © Research Square 2026 | ISSN 2693-5015 (online) Privacy Policy Terms of Service Do Not Sell My Personal Information {"props":{"pageProps":{"initialData":{"identity":"rs-7500403","acceptedTermsAndConditions":true,"allowDirectSubmit":true,"archivedVersions":[],"articleType":"Research Article","associatedPublications":[],"authors":[{"id":508043114,"identity":"7740355c-1f20-45ba-9096-884fd7f9369d","order_by":0,"name":"Sreemoyee Chakraborty","email":"data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAZAAAAAyAQMAAABI0h/eAAAABlBMVEX///8AAABVwtN+AAAACXBIWXMAAA7EAAAOxAGVKw4bAAAA6klEQVRIiWNgGAWjYFAD9vaDD4AUDx/xWnjOJBuAKDbitUgkmEmAaIJa5GcfPvjoRsVhOX6JhLTKrzl2MmwMzA8f3cCjxeBcWrJxzpnDxpI9D4/dlt2WDHQYm7FxDj4tPDxm0rlthxM3HE9Iuy25jRmohYdNGp8W+R7+77+BWur3H0gwK5bcVk9YC8MZHjZmoJYEA44EM8aP2w4T1mJwhs1YOudMuuGMM2eSpRm3HQeaQMAv8j3MDz/nVFjL87e3H/z4c1u1PT9788PHeB0GAc1gkpkHTBJWDgJ1YJLxB3GqR8EoGAWjYIQBAOLuRqCMicyhAAAAAElFTkSuQmCC","orcid":"https://orcid.org/0000-0001-5180-156X","institution":"Indian Statistical Institute","correspondingAuthor":true,"prefix":"","firstName":"Sreemoyee","middleName":"","lastName":"Chakraborty","suffix":""},{"id":508043115,"identity":"5c5a9f77-e984-4cc5-a67a-9c30f9586762","order_by":1,"name":"Dhurjati Prasad Sengupta","email":"","orcid":"https://orcid.org/0000-0003-2758-1565","institution":"Indian Statistical Institute","correspondingAuthor":false,"prefix":"","firstName":"Dhurjati","middleName":"Prasad","lastName":"Sengupta","suffix":""},{"id":508043116,"identity":"dae352b0-672b-40d4-b377-ee0e5196fea3","order_by":2,"name":"Kalyan Halder","email":"","orcid":"https://orcid.org/0000-0003-1920-5535","institution":"Presidency University","correspondingAuthor":false,"prefix":"","firstName":"Kalyan","middleName":"","lastName":"Halder","suffix":""}],"badges":[],"createdAt":"2025-08-31 12:02:08","currentVersionCode":1,"declarations":{"humanSubjects":false,"vertebrateSubjects":false,"conflictsOfInterestStatement":false,"humanSubjectEthicalGuidelines":false,"humanSubjectConsent":false,"humanSubjectClinicalTrial":false,"humanSubjectCaseReport":false,"vertebrateSubjectEthicalGuidelines":false},"doi":"10.21203/rs.3.rs-7500403/v1","doiUrl":"https://doi.org/10.21203/rs.3.rs-7500403/v1","draftVersion":[],"editorialEvents":[{"content":"https://doi.org/10.1007/s10347-025-00713-5","type":"published","date":"2025-09-25T00:00:00+00:00"}],"editorialNote":"","failedWorkflow":false,"files":[{"id":90856861,"identity":"4a7d71b9-1ae9-478e-bc90-bb4879e15e17","added_by":"auto","created_at":"2025-09-09 05:13:51","extension":"jpeg","order_by":1,"title":"Figure 1","display":"","copyAsset":false,"role":"figure","size":171659,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003eGeological Map of the Cenozoic of Kutch Basin, Gujarat, India modified after Biswas (1992), showing the basin's location in the country (inset map). The black dots mark the studied locations from where the Naredi Formation was studied to create the lithology.\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image1.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/21cf5a2622839ee28ad69dc9.jpeg"},{"id":90856209,"identity":"eac8c253-1a17-4ffd-bc39-a13b67d25390","added_by":"auto","created_at":"2025-09-09 05:05:51","extension":"jpeg","order_by":2,"title":"Figure 2","display":"","copyAsset":false,"role":"figure","size":365834,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003eLitholog of the 25 m thick Lower Eocene (Ypressian) Naredi Formation, Kutch Basin, India showing the different taphofacies and corresponding regressive events. The black and red dots represent the levels from where hand specimens and thin sections were studied respectively\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image2.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/329f366b6a1f6c71c4965a39.jpeg"},{"id":90856210,"identity":"ba5b8183-0b12-401a-b032-4ae4b33732a0","added_by":"auto","created_at":"2025-09-09 05:05:51","extension":"jpeg","order_by":3,"title":"Figure 3","display":"","copyAsset":false,"role":"figure","size":87234,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003eDifferent stages of fragmentation in Mollusca and Foraminifera in the Eocene Formations of Kutch Basin, India\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image3.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/d7e2a2606592cc336990077a.jpeg"},{"id":90856214,"identity":"72a3a168-951b-4d95-8778-96185d14ca33","added_by":"auto","created_at":"2025-09-09 05:05:51","extension":"jpeg","order_by":4,"title":"Figure 4","display":"","copyAsset":false,"role":"figure","size":303414,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003ea- b) Articulated and disarticulated but fragmented bivalves near the periphery of concretions, c) articulated and intact bivalve in the center of the concretion, d) fragmented bivalves and intact turritellid (gastropod) in the concretion\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image4.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/e5ced9716c82747e47d4bac3.jpeg"},{"id":90856215,"identity":"c401a26b-67bc-4261-840d-92fc334c15b0","added_by":"auto","created_at":"2025-09-09 05:05:51","extension":"jpeg","order_by":5,"title":"Figure 5","display":"","copyAsset":false,"role":"figure","size":534101,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003ea) Paleocurrent imbrication of fossils, corresponding to cross laminations in the fossiliferous glauconitic green shale, b) \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eNummulites\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003ewith spar-filled chambers, bivalves, and Glauconite, c) Glauconite in the green shale\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image5.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/a8f5522deca1c46fb95b56c0.jpeg"},{"id":90856212,"identity":"da0545ea-183c-43bb-9f75-e6e09d63b7b8","added_by":"auto","created_at":"2025-09-09 05:05:51","extension":"jpeg","order_by":6,"title":"Figure 6","display":"","copyAsset":false,"role":"figure","size":103341,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003ea-b) \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eNummulites burdigalensis burdigalensis \u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003e(Sahni et al., 2006; Saraswati et al., 2012; Mitra 2023), c-d) \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eNummulites globulus nanus\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003e (Schaub, 1981; Saraswati et al., 2012; Keller et al., 2014)\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image6.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/5303338926386533ff273b0a.jpeg"},{"id":90856232,"identity":"f33f8c63-7ad2-46f7-a05e-9db8431e2e43","added_by":"auto","created_at":"2025-09-09 05:05:51","extension":"jpeg","order_by":7,"title":"Figure 7","display":"","copyAsset":false,"role":"figure","size":593682,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003ea) Brown shale with interlayered gypsum and sporadic mollusc shells, b) fragmented and disarticulated Corbulidae recovered from the brown shale\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image7.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/6f40d1e1db745c5b8dce79fd.jpeg"},{"id":91148401,"identity":"670e088f-3a1c-409e-ac4a-1ac4b187e5fd","added_by":"auto","created_at":"2025-09-12 06:44:07","extension":"jpeg","order_by":8,"title":"Figure 8","display":"","copyAsset":false,"role":"figure","size":444005,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003ea) Field photograph of the concretion layer in the Naredi Formation, b) concretion with a ferric core and foraminifera concentrated near the rim, c) \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eAssilina\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003e chambers filled with micrite, d) \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eAssilina\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003echambers filled with both spar and micrite\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image8.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/ecdad67f08908d8ff43da66f.jpeg"},{"id":90856867,"identity":"9c93ed6d-5118-4a9f-bea5-2a1b493405e0","added_by":"auto","created_at":"2025-09-09 05:13:51","extension":"jpeg","order_by":9,"title":"Figure 9","display":"","copyAsset":false,"role":"figure","size":326567,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003ea) Representing Taphofacies E \u003c/strong\u003e- \u003cem\u003e\u003cstrong\u003eAssilina-\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003ebearing brown shale of about 1 m thickness just below a massive \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eAssilina-\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003ebearing limestone, b-c) Recrystallized pillars between the chambers in the \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eAssilina\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003e tests\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image9.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/32035a5084a5a7cb3a590e07.jpeg"},{"id":90856217,"identity":"978f869f-d5a7-453a-a192-fa6d98555864","added_by":"auto","created_at":"2025-09-09 05:05:51","extension":"jpeg","order_by":10,"title":"Figure 10","display":"","copyAsset":false,"role":"figure","size":253838,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003ea) Field photograph of the \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eAssilina\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003e-dominated massive limestone, b) \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eAssilina exponens\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003e in the limestone, c) hand specimen of corals from Taphofacies F, d) \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eAssilina subspinosa\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003e with recrystallized pillars\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image10.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/99f083a06239b1eaa9cb58dc.jpeg"},{"id":90856218,"identity":"956d28f1-5dfc-44db-b560-16412d4def25","added_by":"auto","created_at":"2025-09-09 05:05:51","extension":"jpeg","order_by":11,"title":"Figure 11","display":"","copyAsset":false,"role":"figure","size":471435,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cstrong\u003ea) Paleocurrent imbrication of fossils, corresponding to cross laminations of the host strata shown by \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eAssilina\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003e tests within the limestone, b) \u003c/strong\u003e\u003cem\u003e\u003cstrong\u003eAssilina\u003c/strong\u003e\u003c/em\u003e\u003cstrong\u003e tests following uneven swirl-like folded patterns within the limestone, indicating soft sedimentary deformation\u003c/strong\u003e\u003c/p\u003e","description":"","filename":"image11.jpeg","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/1e5c90e0ef123dfa4cc47c53.jpeg"},{"id":92444013,"identity":"3918b069-a776-4f27-b48e-e596b97c98d7","added_by":"auto","created_at":"2025-09-29 19:41:54","extension":"pdf","order_by":0,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":5316679,"visible":true,"origin":"","legend":"","description":"","filename":"manuscript.pdf","url":"https://assets-eu.researchsquare.com/files/rs-7500403/v1/242a80da-0af2-4170-8452-44c0e1fb7eda.pdf"}],"financialInterests":"The authors declare no competing interests.","formattedTitle":"\u003cp\u003eTaphofacies from the lower Eocene Naredi Formation of Kutch Basin, western India, and their significance\u003c/p\u003e","fulltext":[{"header":"1. Introduction","content":"\u003cp\u003eTaphofacies analysis is crucial in interpreting ancient environments because it captures the full spectrum of post-mortem processes affecting fossils, offering insights that go beyond traditional sedimentological and taxonomic approaches. A taphofacies is defined as a body of sedimentary rock distinguished from surrounding units by its unique suite of taphonomic properties (Boessenecker et al., \u003cspan citationid=\"CR16\" class=\"CitationRef\"\u003e2014\u003c/span\u003e), reflecting both pre-burial processes\u0026mdash;such as bioerosion, disarticulation, transport, fragmentation, and post-burial changes like compaction, mineral replacement, fossil dissolution, and reworking. These combined processes imprint distinct signatures on fossil assemblages, enabling the identification of specific fossil-bearing horizons that correspond to past depositional environments. Despite its potential, this method remains underutilized in key paleogeographic regions such as the Indian subcontinent.\u003c/p\u003e\u003cp\u003eSo, this study tests the hypothesis whether systematic variations in the taphonomic characteristics of larger benthic foraminifera and associated mega-invertebrates within the Naredi Formation correspond to distinct depositional settings, allowing the differentiation of taphofacies that can serve as independent indicators of paleoenvironmental conditions.\u003c/p\u003e\u003cp\u003eThis leads to answering the question: Can taphofacies analysis of the Naredi Formation in the Kutch Basin provide a reliable and independent framework for reconstructing paleoenvironmental settings beyond traditional lithological and taxonomic methods?\u003c/p\u003e\u003cp\u003eThe Kutch Basin in western India, a pericratonic rift basin (Fig.\u0026nbsp;\u003cspan refid=\"Fig1\" class=\"InternalRef\"\u003e1\u003c/span\u003e), bounded by three faults with a well-preserved Cenozoic sequence, including the fossil-rich lower Eocene Naredi Formation, presents an ideal case for applying taphofacies analysis. The goal is to establish a taphofacies framework that serves as an independent proxy for reconstructing paleoenvironmental conditions, ultimately enhancing and refining existing interpretations based on lithology and fossil taxonomy.\u003c/p\u003e\u003cp\u003e\u003c/p\u003e\u003cp\u003eGlobal studies show the importance of taphonomy in paleoenvironmental interpretation. Beavington-Penney (\u003cspan citationid=\"CR8\" class=\"CitationRef\"\u003e2004\u003c/span\u003e), Nebelsick et al. (\u003cspan citationid=\"CR54\" class=\"CitationRef\"\u003e2011\u003c/span\u003e), and Ćosović et al. (\u003cspan citationid=\"CR21\" class=\"CitationRef\"\u003e2012\u003c/span\u003e) linked taphonomic features to transport, facies variation, and carbonate platform architecture. Lipps (\u003cspan citationid=\"CR43\" class=\"CitationRef\"\u003e1988\u003c/span\u003e) and Loubere and Gary (\u003cspan citationid=\"CR45\" class=\"CitationRef\"\u003e1990\u003c/span\u003e) highlighted biological and post-burial alterations in foraminifera through taphonomy. Babazadeh and Alavi (\u003cspan citationid=\"CR4\" class=\"CitationRef\"\u003e2013\u003c/span\u003e) and Tomassetti and Benedetti (\u003cspan citationid=\"CR75\" class=\"CitationRef\"\u003e2020\u003c/span\u003e) used microfacies and reworked assemblages to reconstruct Eocene carbonate systems. Despite India\u0026rsquo;s key Paleogene role, such frameworks are lacking. This study of the Naredi Formation helps fill that gap.\u003c/p\u003e\u003cp\u003eThe Eocene succession of Kutch is well-studied for stratigraphy, sedimentology, and paleontology. Wynne (1872) was the first to study the Cenozoic rocks of Kutch Basin. Biswas (\u003cspan citationid=\"CR9\" class=\"CitationRef\"\u003e1965\u003c/span\u003e) did a detailed mapping along with the stratigraphy of the basin. Further studies were conducted in the subsequent years to establish a formal stratigraphy and time correlation by Biswas and Raju (\u003cspan citationid=\"CR14\" class=\"CitationRef\"\u003e1971\u003c/span\u003e, \u003cspan citationid=\"CR15\" class=\"CitationRef\"\u003e1973\u003c/span\u003e) and Biswas (\u003cspan citationid=\"CR14\" class=\"CitationRef\"\u003e1971\u003c/span\u003e, \u003cspan citationid=\"CR15\" class=\"CitationRef\"\u003e1973\u003c/span\u003e, \u003cspan citationid=\"CR12\" class=\"CitationRef\"\u003e1977\u003c/span\u003e, \u003cspan citationid=\"CR13\" class=\"CitationRef\"\u003e1992\u003c/span\u003e). The Eocene fauna, including foraminifera, vertebrates, and invertebrates, is quite well studied (for example, Kumar and Sahni, \u003cspan citationid=\"CR42\" class=\"CitationRef\"\u003e1986\u003c/span\u003e; Bajpai and Thewissen, \u003cspan citationid=\"CR7\" class=\"CitationRef\"\u003e2000\u003c/span\u003e; Sengupta et al., \u003cspan citationid=\"CR68\" class=\"CitationRef\"\u003e2011\u003c/span\u003e; Keller et al., \u003cspan citationid=\"CR35\" class=\"CitationRef\"\u003e2013\u003c/span\u003e; Halder and Sinha, \u003cspan citationid=\"CR33\" class=\"CitationRef\"\u003e2014\u003c/span\u003e; Khanolkar and Saraswati, \u003cspan citationid=\"CR38\" class=\"CitationRef\"\u003e2019\u003c/span\u003e; Banerjee et al., \u003cspan citationid=\"CR6\" class=\"CitationRef\"\u003e2019\u003c/span\u003e; Halder and Das, \u003cspan citationid=\"CR32\" class=\"CitationRef\"\u003e2019\u003c/span\u003e; Chakraborty and Sengupta, \u003cspan citationid=\"CR19\" class=\"CitationRef\"\u003e2023\u003c/span\u003e). Previous workers have also done substantial work on sedimentology, stratigraphy, and sequence stratigraphy (for example, Sarkar et al. \u003cspan citationid=\"CR64\" class=\"CitationRef\"\u003e2012\u003c/span\u003e; Saraswati et al. \u003cspan citationid=\"CR62\" class=\"CitationRef\"\u003e2016\u003c/span\u003e, \u003cspan citationid=\"CR63\" class=\"CitationRef\"\u003e2018\u003c/span\u003e; Catuneanu and Dave \u003cspan citationid=\"CR18\" class=\"CitationRef\"\u003e2017\u003c/span\u003e; Srivastava and Singh, \u003cspan citationid=\"CR70\" class=\"CitationRef\"\u003e2017\u003c/span\u003e; Srivastava et al., \u003cspan citationid=\"CR71\" class=\"CitationRef\"\u003e2019\u003c/span\u003e; Banerjee et al., \u003cspan citationid=\"CR5\" class=\"CitationRef\"\u003e2018\u003c/span\u003e; Srivastava and Singh, \u003cspan citationid=\"CR72\" class=\"CitationRef\"\u003e2019\u003c/span\u003e; Srivastava et al., \u003cspan citationid=\"CR73\" class=\"CitationRef\"\u003e2022\u003c/span\u003e). However, hardly any work has been done on the biota's taphonomy present in the Kutch Basin's Cenozoic deposits.\u003c/p\u003e\u003cp\u003eThe Eocene rocks of the Kutch Basin predominantly represent marginal marine to open marine settings and are well exposed near Baranda, Nareda, Harudi, and Lakhpat. The Naredi Formation, especially well developed near Nareda village (23\u0026deg;34'32.6\"N, 068\u0026deg;38'36.2\"E), consists of near-horizontal beds exposed as vertical sections along shallow river valleys. North of Harudi village, a river section marks the contact between the Naredi and overlying Harudi Formations. The lower part of the Naredi Formation comprises green, grey, and brown shales with intercalated gypsum layers, while the upper part includes foraminiferal limestones and ferruginous claystone (Biswas, \u003cspan citationid=\"CR13\" class=\"CitationRef\"\u003e1992\u003c/span\u003e; Srivastava and Singh, \u003cspan citationid=\"CR70\" class=\"CitationRef\"\u003e2017\u003c/span\u003e). Following Biswas (\u003cspan citationid=\"CR13\" class=\"CitationRef\"\u003e1992\u003c/span\u003e), the formation has been divided into three members: a Gypseous Shale Member (grey, brown, green shales and concretions with interlayered gypsum), an \u003cem\u003eAssilina\u003c/em\u003e Limestone Member (dirty white limestone and marl), and a Ferruginous Claystone Member (brown and grey claystones, and a red laterite bed capping the sequence). However, a revised and more detailed litholog (Fig.\u0026nbsp;\u003cspan refid=\"Fig2\" class=\"InternalRef\"\u003e2\u003c/span\u003e) was constructed based on new field observations and fossil content to support the taphofacies analysis. As the uppermost horizons are barren, the present study focuses exclusively on the fossiliferous interval from the base to the topmost \u003cem\u003eAssilina\u003c/em\u003e-bearing horizon.\u003c/p\u003e"},{"header":"2. Materials and Methods","content":"\u003cp\u003eThe Naredi Formation has been studied at two locations in and around the type section (23\u0026deg; 34\u0026apos; 32.6\u0026quot; N, 068\u0026deg; 38\u0026apos; 36.2\u0026quot; E) to revise the lithology and study the taphofacies. Three other locations near the type section of the Harudi Formation (23\u0026deg; 31\u0026rsquo;27.0\u0026rdquo; N, 068\u0026deg; 41\u0026rsquo;11.0\u0026rdquo; E) were also studied to complete the lithology of the topmost part of the formation (above the \u003cem\u003eAssilina\u003c/em\u003e limestone) as shown by black dots in Fig. \u003cspan class=\"InternalRef\"\u003e1\u003c/span\u003e. Rock samples were collected at 1-meter intervals because the exposure in these sections was continuous, with a generally homogeneous lithology. The majority of the formation comprises shale, with a gradual transition to limestone and ferruginous claystone towards the top. Most of the beds in the studied sections range from 1 to 4 meters in thickness, making a 1-meter interval an effective resolution for capturing vertical variations without oversampling. This sampling resolution also allowed for consistent recording of key sedimentary features, such as thin gypsum interlayers within the shale, as well as subtle changes in rock colour and fossil occurrence. In cases where individual beds were thinner than 1 meter, samples were taken from both the base and top of the unit to ensure internal variation was documented. Limestones have been named according to the Dunham classification of rocks (Dunham, \u003cspan class=\"CitationRef\"\u003e1962\u003c/span\u003e).\u003c/p\u003e\n\u003cp\u003eThe rock samples were sent to Lab Crystals, Lucknow, Uttar Pradesh, India, for the preparation of slides. A total of 29 thin sections were prepared from separate rock samples collected across different fossiliferous horizons of the Naredi Formation (Fig. \u003cspan class=\"InternalRef\"\u003e2\u003c/span\u003e). These thin sections collectively represent approximately 5 meters of fossiliferous intervals distributed across key horizons within the 25 m thick succession (marked in Fig. \u003cspan class=\"InternalRef\"\u003e2\u003c/span\u003e). Of the 29 thin sections, 5 measured 26 \u0026times; 47 mm and the rest 50 \u0026times; 75 mm, as the splintery green shale prevented preparation of larger thin sections. In cases where a single fossiliferous horizon was laterally extensive, samples were taken about 10 meters apart to capture lateral variation, with each thin section representing a unique point and not repeated from the same rock sample.\u003c/p\u003e\n\u003cp\u003eThin sections were examined under a Leica DVM6 M digital microscope to study the internal and external taphonomic features of foraminifera, which require microscopic analysis due to their small size. In contrast, horizons containing only macrofossils were studied using hand specimens, also from rock samples at an interval of 10 meters apart to capture the lateral variation, as their larger size allowed for detailed observation without thin-sectioning. Fossil extraction for hand specimen studies was carried out with great care to minimize damage to specimens. Only parts of the horizons where fossils could be retrieved without the use of chemical treatments were selected for extraction. Mechanical methods were limited to gentle techniques, using distilled water, a small hammer, and a fine chisel when necessary to dislodge fossils from the matrix. This approach ensured the preservation of delicate taphonomic features critical to the analysis. And if samples got damaged during extraction, even after extreme caution, they have been studied accordingly. Taphonomic attributes such as fragmentation, test shape, and wall alteration were assessed in both thin sections (microscopic scale) and hand specimens (macroscopic scale). Figure \u003cspan class=\"InternalRef\"\u003e2\u003c/span\u003e shows the sampling levels and represents the composite litholog of the Naredi Formation. SEM (Scanning Electron Microscope) studies were conducted on the thin sections of rocks and fossil specimens at the Geology Department, Presidency University, Kolkata, West Bengal, India.\u003c/p\u003e\n\u003cp\u003eTaxonomy, diversity (the increase or decrease in the number of different groups of fossils occurring within a bed per unit area), and sedimentological characters have been considered for an accurate interpretation of the environment of deposition. The taphonomic changes occurring in the fossiliferous layers and the changing environment were also recorded. Different taphonomic features have been observed within the fossiliferous rock units of the Naredi Formation of Kutch Basin, India. The major characters used to describe each taphofacies include:\u003c/p\u003e\n\u003cp\u003eFragmentation \u0026ndash; The level of fragmentation in foraminifera and Mollusca has been divided into Stages 0\u0026ndash;3. Stage 0 corresponds to an intact fossil, and the level of fragmentation increases from Stage 1 to Stage 3. Figure \u003cspan class=\"InternalRef\"\u003e3\u003c/span\u003e gives a pictorial description of the different stages. This feature is also calculated as a percentage, showing how many of the total number of fossils are fragmented in each taphofacies and comprises a pre-burial feature.\u003c/p\u003e\n\u003cp\u003eArticulation \u0026ndash; This pre-burial character is only applicable for bivalves and has been calculated as the percentage of the total bivalves found in an articulated state. An articulated bivalve has both valves joined together.\u003c/p\u003e\n\u003cp\u003eAbundance \u0026ndash; This feature is studied by calculating the total number of fossils in a designated area. Fossil abundance was calculated per unit area (cm\u0026sup2;) using both exposed surfaces of rock slabs and thin sections, allowing detection of both larger and smaller fossils. While volumetric estimates would have been ideal, the hard matrix and fossil composition made fossil separation and chemical treatments ineffective. Thus, area-based counts provide a more consistent and reliable measure. There are three grades \u0026ndash; Low (\u0026lt;\u0026thinsp;0.1 fossils per sq. cm), Medium (0.1\u0026ndash;4 fossils per sq. cm), and High (\u0026gt;\u0026thinsp;4 fossils per sq cm). The unitary method was used to standardize fossil counts to a common unit area, enabling accurate abundance comparison across uneven sampling areas. Throughout the Naredi Formation, there is a wide variation in the abundance of fossils. In some of the taphofacies, variation is observed even within a single fossiliferous horizon.\u003c/p\u003e\n\u003cp\u003eMineral alteration \u0026ndash; This character includes sparitization and micritization of fossils. Micritization occurs syndepositionally and in the early stages of burial and is biogenic. It alters the fossils by weakening the test walls in fossils such as foraminifera, often contributing to fragmentation. Micritization has been divided into 3 stages: Stage 0 \u0026ndash; No micritization, Stage 1 \u0026ndash; Partial wall micritization with infilled chambers, Stage 2 - Heavy micritization with internal structures obscured. Sparitization occurs post-depositionally in early to late stages of diagenesis due to compaction, fluid movement, and chemical alteration. It has also been divided into 3 stages: Stage 0 \u0026ndash; No sparitization, Stage 1 \u0026ndash; Slight recrystallization, wall textures preserved and chambers infilled, Stage 2 \u0026ndash; Majority of the test recrystallized, internal structure obliterated.\u003c/p\u003e\n\u003cp\u003eSpecial characters \u0026ndash; Features such as soft sediment deformation (a post-depositional but pre-lithification process) and concretion formation (a post-burial process) were also recorded. These processes can distort fossil orientation, enhance fragmentation, or create localized zones of diagenetic overprint.\u003c/p\u003e\n\u003cp\u003eImbrication of fossils \u0026ndash; This character indicates the orientation of the fossils within a litho unit (1 \u0026amp; 2 \u0026ndash; pre-burial feature, 3 - post-depositional but pre-lithification feature). The observed fossil orientations in this study include: (1) a unidirectional, layer-parallel alignment of specimens; (2) a bidirectional, layer-parallel orientation corresponding to cross-laminated structures; and (3) a concentric or swirl-like pattern indicative of localized hydrodynamic vortices or soft sediment deformation.\u003c/p\u003e\n\u003cp\u003eDiversity and Assemblage \u0026ndash; Diversity is known to increase from a lagoonal to an open marine setting. A qualitative study on diversity gives a better insight into the environment of deposition of the taphofacies. In this study, the diversity measurement has been taken as the number of species per cm\u0026sup2;. If only the genus could be identified for a fossil group, it was considered \u003cem\u003eGenus sp.\u003c/em\u003e to avoid bias. And this data has been generated by studying area grids in hand specimens (10 x 10 cm\u003csup\u003e2\u003c/sup\u003e for Taphofacies A and C, whereas a 2.5 x 2.5 cm\u003csup\u003e2\u003c/sup\u003e for Taphofacies B, D-F due to the difference in size and distribution of fossils). Diversity has then been standardized and represented as species per cm\u0026sup2;. Studying the fossil assemblage is a key element in understanding the paleoenvironment because certain organisms can only survive in specific environmental conditions. For example, \u003cem\u003eAssilina\u003c/em\u003e occurs only in warm shallow marine environments (Din\u0026ccedil;er, \u003cspan class=\"CitationRef\"\u003e2016\u003c/span\u003e); it cannot be found in lagoonal or brackish water conditions.\u003c/p\u003e\n\u003cp\u003e\u003cstrong\u003eTable 1.\u0026nbsp;\u003c/strong\u003e\u003cstrong\u003eMajor characteristics of six identified taphofacies within the Naredi Formation, Kutch Basin, India\u0026nbsp;\u003c/strong\u003e\u003c/p\u003e\n\u003cp\u003e\u003cimg 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\" width=\"1025\" height=\"697\"\u003e\u003c/p\u003e\n\u003cdiv align=\"left\" class=\"colspec\"\u003e\u003cbr\u003e\u003c/div\u003e\n\u003cp\u003e\u003c/p\u003e\n\u003cp\u003eSize and shape of the fossils \u0026ndash; Fossil shape and size were assessed using both hand specimens and petrographic thin sections. Given the consistent orientation of the fossils, thin sections were prepared to capture vertical cross-sections for measurement. To validate the accuracy of these measurements and account for potential sectional bias, complementary measurements were also obtained from loose specimens that could be dislodged from the fossiliferous litho units.\u003c/p\u003e"},{"header":"3. Taphofacies of the Naredi Formation","content":"\u003cp\u003eThe Naredi Formation has been subdivided into six distinct taphofacies (A\u0026ndash;F) based on a combination of taphonomic attributes such as fragmentation, micritization, biofabric, fossil articulation, spatial arrangement, and associated sedimentological features. These taphofacies represent specific microenvironments within the broader transition from a lagoonal to a middle ramp setting. The defining characteristics of each taphofacies are summarized in Table\u0026nbsp;1, and detailed descriptions are provided below.\u003c/p\u003e\u003cdiv id=\"Sec4\" class=\"Section2\"\u003e\u003ch2\u003e3.1. Taphofacies A:\u003c/h2\u003e\u003cp\u003eThe lower part of the Naredi Formation contains two fossiliferous concretionary horizons, approximately 0.4 m and 0.2 m thick (Fig.\u0026nbsp;\u003cspan refid=\"Fig2\" class=\"InternalRef\"\u003e2\u003c/span\u003e), composed of fossil-bearing grey and brown limestone concretions embedded within shale, with gypsum interlayers. These concretions exhibit concentric colour changes, typically light brown at the margins, transitioning to darker brown or grey toward the centre. A total of 37 individual molluscan specimens were studied from nine concretions, showing low diversity (0.01 species per cm\u003csup\u003e2\u003c/sup\u003e) and low abundance, dominated by \u003cem\u003eCorbula\u003c/em\u003e (bivalves) and rarely \u003cem\u003eTurritella\u003c/em\u003e (gastropods).\u003c/p\u003e\u003cp\u003eTaphonomic data indicate that 78.4% of the fossils are fragmented (stages 1 \u0026amp; 2, Fig.\u0026nbsp;\u003cspan refid=\"Fig3\" class=\"InternalRef\"\u003e3\u003c/span\u003e), and 47% of bivalves remain articulated. In this taphofacies, some bivalves show fragmentation even in their articulated form, which may reflect post-mortem compaction within partially cemented concretions, rather than transport-induced breakage. Fragmented shells, both articulated and disarticulated, are more common near the concretion margins (Fig.\u0026nbsp;\u003cspan refid=\"Fig4\" class=\"InternalRef\"\u003e4\u003c/span\u003ea\u0026ndash;b), while intact, articulated bivalves are typically found at the centers (Fig.\u0026nbsp;\u003cspan refid=\"Fig4\" class=\"InternalRef\"\u003e4\u003c/span\u003ec). \u003cem\u003eTurritella\u003c/em\u003e are usually intact and located near the periphery (Fig.\u0026nbsp;\u003cspan refid=\"Fig4\" class=\"InternalRef\"\u003e4\u003c/span\u003ed). A bimodal size distribution is observed, with both large (avg. 42.9 mm) and small (avg. 9.3 mm) specimens occurring at both core and margin positions. Turritellids are often found in shallow marine habitats but also in very shallow (i.e., marginal marine) and deep marine environments (Scholz et al., 2024). However, the presence of low-diversity, low-abundance assemblages dominated by \u003cem\u003eCorbula\u003c/em\u003e, a taxon tolerant of brackish, low-oxygen conditions (Anderson \u0026amp; Roopnarine, \u003cspan citationid=\"CR3\" class=\"CitationRef\"\u003e2003\u003c/span\u003e; Naugolnykh, \u003cspan citationid=\"CR53\" class=\"CitationRef\"\u003e2017\u003c/span\u003e), supports deposition in a marginal marine to restricted lagoonal setting. Table\u0026nbsp;1 outlines the taphofacies characteristics.\u003c/p\u003e\u003cp\u003e\u003c/p\u003e\u003c/div\u003e\u003cdiv id=\"Sec5\" class=\"Section2\"\u003e\u003ch2\u003e3.2. Taphofacies B:\u003c/h2\u003e\u003cp\u003eIn the lower part of the Naredi Formation, two glauconitic green shale horizons (~\u0026thinsp;0.2 m thick each) occur, interlayered with gypsum and clay showing cross-laminations (Fig.\u0026nbsp;\u003cspan refid=\"Fig2\" class=\"InternalRef\"\u003e2\u003c/span\u003e, Fig.\u0026nbsp;\u003cspan refid=\"Fig5\" class=\"InternalRef\"\u003e5\u003c/span\u003e). These beds contain high glauconite pellet content, visible in both thin sections and SEM and exhibit variable pellet maturity (Srivastava \u0026amp; Singh, \u003cspan citationid=\"CR70\" class=\"CitationRef\"\u003e2017\u003c/span\u003e). Fossils comprise of \u003cem\u003eNummulites\u003c/em\u003e and disarticulated molluscan shells, with occasional coral fragments, and show moderate abundance with Stage 1 sparitization, and moderate diversity (0.64 species per cm\u003csup\u003e2\u003c/sup\u003e). A total of 273 fossils were recorded for taphonomic studies from these horizons, including 230 \u003cem\u003eNummulites\u003c/em\u003e (84.2%), 39 molluscs (14.3%), and 4 coral/unknown fragments (1.5%). 219 fossil specimens were documented in thin sections, while 54 specimens that could be extracted from rock samples were examined using high-magnification microscopy (Leica DVM6 M). \u003cem\u003eNummulites\u003c/em\u003e are well preserved, with 96.5% showing Stage 0 fragmentation, while molluscs are heavily fragmented and disarticulated (Stages 2\u0026ndash;3), with only 12.8% intact. The molluscs include probable corbulids, known for inhabiting low-energy marginal marine environments (Anderson \u0026amp; Roopnarine, \u003cspan citationid=\"CR3\" class=\"CitationRef\"\u003e2003\u003c/span\u003e). Overall fragmentation is 16.8%, and fossil size distribution is bimodal, with smaller \u003cem\u003eNummulites\u003c/em\u003e (avg. 0.8 mm) and larger mollusc fragments (avg. 1.3 mm). The lens shape of \u003cem\u003eNummulites\u003c/em\u003e (as observed in hand specimens, as well as in thin sections) provides hydrodynamic stability and resistance to fragmentation, while the larger, curved molluscan shells were more prone to mechanical breakage (Tasdemir, \u003cspan citationid=\"CR74\" class=\"CitationRef\"\u003e2009\u003c/span\u003e). This is consistent with studies showing that larger bioclasts have a higher likelihood of fragmentation under hydraulic stress (Kidwell \u0026amp; Flessa, \u003cspan citationid=\"CR41\" class=\"CitationRef\"\u003e1995\u003c/span\u003e). Fossils exhibit bidirectional paleocurrent imbrication matching the direction of cross-lamination, indicating bottom currents and limited post-mortem transport.\u003c/p\u003e\u003cp\u003e\u003c/p\u003e\u003cp\u003e\u003c/p\u003e\u003cp\u003eThe green shale\u0026rsquo;s colour and the abundance of glauconite pellets indicate a phase of reduced siliciclastic sedimentation, a key condition for glauconitisation (Odin \u0026amp; Matter, \u003cspan citationid=\"CR56\" class=\"CitationRef\"\u003e2003\u003c/span\u003e; Amorosi, \u003cspan citationid=\"CR2\" class=\"CitationRef\"\u003e1997\u003c/span\u003e). Such conditions typically arise during marine transgressions, when sediment input slows relative to accommodation space, allowing prolonged residence time necessary for glauconite formation. The interbedded gypsum layers further support low sedimentation and episodic restriction, suggesting deposition in a marginal marine to inner shelf setting under periodically evaporitic conditions (Srivastava \u0026amp; Singh, \u003cspan citationid=\"CR70\" class=\"CitationRef\"\u003e2017\u003c/span\u003e). The fossil assemblage in this horizon reinforces the transgressive interpretation. The dominance of well-preserved, low-fragmentation \u003cem\u003eNummulites\u003c/em\u003e, particularly \u003cem\u003eN. burdigalensis burdigalensis\u003c/em\u003e and \u003cem\u003eN. globulus nanus\u003c/em\u003e, which are known from transgressive, mid-shelf to lagoonal settings (Racey, \u003cspan citationid=\"CR58\" class=\"CitationRef\"\u003e2001\u003c/span\u003e; Keller et al., 2014; Shahzad et al., 2024), supports deposition under open but shallow marine conditions. Molluscan taphonomy, characterized by higher fragmentation and low articulation, alongside features such as cross-laminations and imbricated bioclasts, indicates intermittent higher-energy events that may have accompanied early stages of transgression. Therefore, the glauconite-bearing horizon reflects a transgressive surface, likely representing a temporary sediment starvation phase within a shallow marine lagoonal system. The presence of interbedded gypsum points to episodic restriction and hypersalinity (Srivastava and Singh \u003cspan citationid=\"CR70\" class=\"CitationRef\"\u003e2017\u003c/span\u003e), suggesting fluctuating connectivity with the open marine system during early transgression.\u003c/p\u003e\u003c/div\u003e\u003cdiv id=\"Sec6\" class=\"Section2\"\u003e\u003ch2\u003e3.3. Taphofacies C:\u003c/h2\u003e\u003cp\u003eThis taphofacies is defined by brown shale horizons containing sporadic, low-abundance mollusc shells and interlayered gypsum (Fig.\u0026nbsp;\u003cspan refid=\"Fig7\" class=\"InternalRef\"\u003e7\u003c/span\u003ea\u0026ndash;b). Four such horizons, measuring approximately 3.5 m, 2.0 m, 1.8 m, and 1.5 m in thickness (in ascending stratigraphic order), exhibit horizontal planar lamination and a splintery texture\u0026mdash;features indicative of restricted, low-energy depositional conditions. An additional 0.8 m thick horizon near the base of the formation comprises grey-brown shale with patchy, poorly developed gypsum and similarly sporadic mollusc shells.\u003c/p\u003e\u003cp\u003eA total of 45 mollusca fossils were recorded in the field, averaging 2.3 cm in length. Only seven were recovered intact; the rest disintegrated during extraction due to their fragile preservation. Prior to collection, outlines of all specimens were measured in situ, revealing that 95.5% (43 out of 45) were already fragmented. The surviving shells display Stage 1 fragmentation (Fig.\u0026nbsp;\u003cspan refid=\"Fig3\" class=\"InternalRef\"\u003e3\u003c/span\u003e), with consistent breakage along exposed edges, suggesting weathering as the primary agent rather than post-mortem transport. Despite this, the shells remained articulated, reinforcing deposition under calm, low-energy conditions. Taxonomic identification was limited due to fragmentation, low abundance, and low diversity (0.01 species per cm\u003csup\u003e2\u003c/sup\u003e), though some specimens could be assigned to Corbulidae.\u003c/p\u003e\u003cp\u003eThe presence of thick continuous laminated gypsum interlayers within four of the five brown shale horizons (Fig.\u0026nbsp;\u003cspan refid=\"Fig7\" class=\"InternalRef\"\u003e7\u003c/span\u003ea) strongly supports episodic regression and evaporitic conditions typical of a restricted lagoonal environment. These gypsum layers reflect increased salinity under evaporative stress; conditions commonly associated with sea-level fall and reduced circulation. The repeated alternation of shale and gypsum suggests cyclic changes in salinity and water depth, driven by frequent sea-level fluctuations. This interpretation partially aligns with previous findings by Srivastava and Singh (\u003cspan citationid=\"CR70\" class=\"CitationRef\"\u003e2017\u003c/span\u003e), who reported a single gypsum-bearing shale horizon in the Naredi Formation and interpreted it as evidence of lagoonal regression. In contrast, the current study identifies five such horizons, of which four contain bioclasts and are assigned to Taphofacies C. This expanded dataset indicates that the Naredi Formation recorded at least five distinct regressive episodes.\u003c/p\u003e\u003cp\u003eHowever, the fifth gypsum-bearing shale horizon does not contain bioclasts and is thus excluded from Taphofacies C. Furthermore, the grey-brown shale horizon near the base of the formation, with its sparse and patchy gypsum, presents a more complex case. The nature of gypsum in this interval \u0026ndash; thin, poorly laminated, and irregularly distributed, raises the possibility of a diagenetic origin rather than primary evaporitic deposition. Such gypsum may have formed through brine seepage along weathered fractures or by dissolution and reprecipitation from underlying grit beds, as suggested by Gontharet et al. (\u003cspan citationid=\"CR30\" class=\"CitationRef\"\u003e2007\u003c/span\u003e). This possibility introduces an important caveat: while well-laminated gypsum layers within shale are reliable indicators of depositional regression, secondary gypsum should not be interpreted as evidence of sea-level fall without additional supporting data.\u003c/p\u003e\u003cp\u003eIn summary, the combination of brown shale with laminated gypsum, the presence of sporadic and fragmented but articulated mollusc shells, low species diversity, and the overall sedimentary context suggests a restricted, low-energy lagoonal environment.\u003c/p\u003e\u003cp\u003e\u003c/p\u003e\u003c/div\u003e\u003cdiv id=\"Sec7\" class=\"Section2\"\u003e\u003ch2\u003e3.4. Taphofacies D:\u003c/h2\u003e\u003cp\u003eTwo concretionary horizons, measuring approximately 0.2 m and 0.25 m in thickness, are identified in the studied section (Fig.\u0026nbsp;\u003cspan refid=\"Fig2\" class=\"InternalRef\"\u003e2\u003c/span\u003e). The lower concretion layer overlies a yellow shale. It underlies Taphofacies A, while the upper horizon is embedded within the \u003cem\u003eAssilina\u003c/em\u003e Limestone, corresponding to Taphofacies F. Both layers are dominated by \u003cem\u003eAssilina\u003c/em\u003e tests, which are preferentially concentrated along the rims of the concretions (Fig.\u0026nbsp;\u003cspan refid=\"Fig8\" class=\"InternalRef\"\u003e8\u003c/span\u003ea\u0026ndash;d), showing high abundance. However, the fossil abundance decreases toward the ferruginous cores.\u003c/p\u003e\u003cp\u003eA total of 1018 foraminifera were recorded from these horizons, comprising 1010 \u003cem\u003eAssilina\u003c/em\u003e and 8 \u003cem\u003eNummulites\u003c/em\u003e specimens. Overall, 36.25% of the total foraminifera exhibit fragmentation (Stages 1\u0026ndash;3). Fragmentation likely began through hydraulic transport and was later augmented or preserved by microbial micritization (Stage 1), which weakened the test walls (Garuglieri et al., \u003cspan citationid=\"CR28\" class=\"CitationRef\"\u003e2024\u003c/span\u003e; Messadi et al., \u003cspan citationid=\"CR49\" class=\"CitationRef\"\u003e2019\u003c/span\u003e), often seen in inner ramp settings. These weakened walls may have further fractured under compaction during early burial, although micritic infilling also contributed to partial test preservation. Of the fragmented \u003cem\u003eAssilina\u003c/em\u003e, 93.75% exhibit micritization. Even among unfragmented tests, 61.68% of forams show micritization, and 38.32% display a combination of micritization and sparitization (Stage 1), underscoring the significant diagenetic role of micritization in this taphofacies (Fig.\u0026nbsp;\u003cspan refid=\"Fig8\" class=\"InternalRef\"\u003e8\u003c/span\u003ec\u0026ndash;d).\u003c/p\u003e\u003cp\u003eThe foraminiferal assemblage is of low diversity (0.32 species per cm\u003csup\u003e2\u003c/sup\u003e) but high abundance (at the rim of the concretions), comprising primarily \u003cem\u003eAssilina laxispira\u003c/em\u003e and rare \u003cem\u003eNummulites\u003c/em\u003e spp. The presence of \u003cem\u003eAssilina\u003c/em\u003e, which typically inhabits warm, shallow inner to middle ramp environments (Din\u0026ccedil;er, \u003cspan citationid=\"CR22\" class=\"CitationRef\"\u003e2016\u003c/span\u003e; Khan et al., \u003cspan citationid=\"CR37\" class=\"CitationRef\"\u003e2024\u003c/span\u003e), alongside micritization features (Messadi et al., \u003cspan citationid=\"CR49\" class=\"CitationRef\"\u003e2019\u003c/span\u003e), supports deposition in a shallow marine setting. However, the ferruginous cores of the concretions, interpreted to result from early diagenetic iron precipitation in marginal marine conditions, indicate post-depositional modification. Such concretions likely formed through microbial mediation under suboxic conditions, where iron was mobilized in pore waters and subsequently precipitated due to localized redox changes (Raiswell, \u003cspan citationid=\"CR59\" class=\"CitationRef\"\u003e1971\u003c/span\u003e; Mozley \u0026amp; Davis, \u003cspan citationid=\"CR52\" class=\"CitationRef\"\u003e2005\u003c/span\u003e). The micritic envelopes around the \u003cem\u003eAssilina\u003c/em\u003e tests may have acted as diffusion barriers, promoting differential iron precipitation and explaining the fossil concentration at concretion margins. This geochemical zonation reflects diagenetic overprinting of originally shallow marine sediments by iron-rich pore fluids during early concretion growth.\u003c/p\u003e\u003cp\u003e\u003c/p\u003e\u003c/div\u003e\u003cdiv id=\"Sec8\" class=\"Section2\"\u003e\u003ch2\u003e3.5. Taphofacies E:\u003c/h2\u003e\u003cp\u003eTaphofacies E is characterized by a 1 m-thick, splintery, impure lime-rich brown shale horizon underlying a massive \u003cem\u003eAssilina\u003c/em\u003e-bearing limestone (Taphofacies F; Fig.\u0026nbsp;\u003cspan refid=\"Fig9\" class=\"InternalRef\"\u003e9\u003c/span\u003ea). The fossil assemblage includes \u003cem\u003eAssilina\u003c/em\u003e, \u003cem\u003eNummulites\u003c/em\u003e, bivalves, corals, and ostracods, with an overall increase in diversity compared to underlying units. The basal part of the horizon exhibits unidirectional fossil imbrication. In contrast, the top of the sequence shows prominent bidirectional imbrication, indicating an increase in the hydraulic energy towards the top. This change is also evident in the higher percentage of fragmented fossils and the dominance of Stage 2 fragmentation in the upper part of the horizon. Fossil abundance is moderate, with evidence of Stage 1 micritization and early sparry cementation.\u003c/p\u003e\u003cp\u003eA total of 717 fossils were studied from thin sections and hand specimens, of which \u003cem\u003eAssilina\u003c/em\u003e dominates (546 specimens, 76.15%), followed by bivalves (87, 12.13%), \u003cem\u003eNummulites\u003c/em\u003e (49, 6.83%), ostracods (24, 3.35%), corals (9, 1.25%), and two unidentified specimens (0.29%). Fragmentation is prevalent (63.18%), with bivalves and corals exhibiting complete fragmentation (100%), \u003cem\u003eAssilina\u003c/em\u003e showing 63.2%, \u003cem\u003eNummulites\u003c/em\u003e 24.5%, and ostracods remaining intact. Fragmentation stages 1 and 2 are observed in foraminifera and molluscs (Fig.\u0026nbsp;\u003cspan refid=\"Fig3\" class=\"InternalRef\"\u003e3\u003c/span\u003e). Notably, 58.9% of the fragmented foraminifera exhibit Stage 1 micritization. In contrast, mollusca shells show minimal endolithic activity (Stage 0), likely due to differing shell microstructures and taphonomic pathways.\u003c/p\u003e\u003cp\u003eSome \u003cem\u003eAssilina\u003c/em\u003e tests display sparry recrystallization concentrated within the pillar structures between chambers (Fig.\u0026nbsp;\u003cspan refid=\"Fig9\" class=\"InternalRef\"\u003e9\u003c/span\u003eb\u0026ndash;c), a feature specific to \u003cem\u003eAssilina subspinosa\u003c/em\u003e (Gazi et al., 2015) while \u003cem\u003eA. laxispira\u003c/em\u003e does not show this character. Pillars are vertical internal supports composed of fine-grained high-Mg calcite, originally more porous than the surrounding test walls (Sengupta and Mukhopadhyay, \u003cspan citationid=\"CR67\" class=\"CitationRef\"\u003e2008\u003c/span\u003e; Loeblich and Tappan, \u003cspan citationid=\"CR44\" class=\"CitationRef\"\u003e2015\u003c/span\u003e). Their porosity and elevated surface area enhance susceptibility to diagenetic alteration, resulting in early sparitization recognized by their clear, coarse crystalline structure. The presence of spar within originally porous high-Mg calcite pillars, while the surrounding wall micrite remains unaltered or only micritized, supports a diagenetic overprint, likely associated with marine or shallow burial cementation phases (Fl\u0026uuml;gel and Munnecke, \u003cspan citationid=\"CR25\" class=\"CitationRef\"\u003e2010\u003c/span\u003e).\u003c/p\u003e\u003cp\u003eThe increased faunal diversity (0.96 species per cm\u003csup\u003e2\u003c/sup\u003e) in this horizon compared to the previous taphofacies, along with the dominance of flattened forms and presence of current-aligned bioclasts, indicates deposition in a well-oxygenated, shallow marine environment transitioning from restricted lagoonal conditions below. Such a setting corresponds with inner to middle ramp depositional environments as interpreted for \u003cem\u003eAssilina\u003c/em\u003e (Khan et al., \u003cspan citationid=\"CR37\" class=\"CitationRef\"\u003e2024\u003c/span\u003e; Dincer, 2016; BouDagher-Fadel, 2008). The bidirectional imbrication, matching cross-lamination in host sediments, further confirms current action as a major agent in fossil orientation and partial fragmentation. These taphonomic and sedimentological features collectively support an interpretation of deposition on the inner ramp, under increasing energy conditions in open marine setting with intermittent hydrodynamic reworking.\u003c/p\u003e\u003cp\u003e\u003c/p\u003e\u003c/div\u003e\u003cdiv id=\"Sec9\" class=\"Section2\"\u003e\u003ch2\u003e3.6. Taphofacies F:\u003c/h2\u003e\u003cp\u003eTaphofacies F comprises three massive, \u003cem\u003eAssilina\u003c/em\u003e-dominated limestone horizons measuring approximately 1 m, 2 m, and 1 m in thickness, respectively. These horizons range texturally from wackestone to grainstone (Fig.\u0026nbsp;\u003cspan refid=\"Fig2\" class=\"InternalRef\"\u003e2\u003c/span\u003e) and display pinch-and-swell structures (Fig.\u0026nbsp;\u003cspan refid=\"Fig10\" class=\"InternalRef\"\u003e10\u003c/span\u003ea\u0026ndash;b). Associated faunal components include \u003cem\u003eNummulites\u003c/em\u003e, molluscs, and corals (Fig.\u0026nbsp;\u003cspan refid=\"Fig10\" class=\"InternalRef\"\u003e10\u003c/span\u003e\u0026ndash;\u003cspan refid=\"Fig11\" class=\"InternalRef\"\u003e11\u003c/span\u003e). The fossil diversity is 0.8 species per cm\u003csup\u003e2\u003c/sup\u003e, and the abundance of fossils is variable (moderate to high), as established through both loose specimen collection and thin-section analysis, and it varies from moderate to high. The lowermost horizon is separated from the two upper ones by a brown shale interlayer containing gypsum, corresponding to Taphofacies C, interpreted as a lagoonal shallowing phase. All horizons are well-exposed and accessible in the type section of the Naredi Formation.\u003c/p\u003e\u003cp\u003eA total of 2,348 fossils were documented from this taphofacies. Of these, 2,272 (96.76%) are \u003cem\u003eAssilina\u003c/em\u003e, 67 (2.85%) are \u003cem\u003eNummulites\u003c/em\u003e, two are molluscs, and two specimens remained indeterminate under microscopic observation. Additionally, three coral hand specimens were recovered (Fig.\u0026nbsp;\u003cspan refid=\"Fig10\" class=\"InternalRef\"\u003e10\u003c/span\u003ec), though corals were not observed in thin sections. Fossil fragmentation is observed in 34.67% of all specimens, with 35.61% of \u003cem\u003eAssilina\u003c/em\u003e (809 out of 2,272) showing varying stages 1\u0026ndash;3. \u003cem\u003eNummulites\u003c/em\u003e are consistently intact, while coral preservation is poor. Among the fragmented \u003cem\u003eAssilina\u003c/em\u003e tests, 75.4% (610 specimens) show micritization and sparitization corresponding to stages 1 and 2.\u003c/p\u003e\u003cp\u003eAbundance increases vertically within each horizon, transitioning from low at the base to high towards the top, correlating with the facies change from wackestone to grainstone. Fragmentation intensity also varies vertically: stages 2 and 3 are predominant near the base, while stages 1 \u0026amp; 2 dominate the upper intervals (Fig.\u0026nbsp;\u003cspan refid=\"Fig3\" class=\"InternalRef\"\u003e3\u003c/span\u003e). Laterally, the two upper limestone horizons exhibit a decrease in foraminiferal abundance and a facies shift from grainstone to wackestone towards the northwest along strike. Species-level identification reveals the presence of \u003cem\u003eAssilina exponens\u003c/em\u003e (Sowerby, \u003cspan citationid=\"CR69\" class=\"CitationRef\"\u003e1840\u003c/span\u003e) and \u003cem\u003eAssilina subspinosa\u003c/em\u003e (Gazi et al., 2015) (Fig.\u0026nbsp;\u003cspan refid=\"Fig10\" class=\"InternalRef\"\u003e10\u003c/span\u003eb \u0026amp; \u003cspan refid=\"Fig10\" class=\"InternalRef\"\u003e10\u003c/span\u003ed)\u003c/p\u003e\u003cp\u003e\u003c/p\u003e\u003cp\u003eTest orientation data show two distinct patterns. In the upper portions of the horizons, fossil alignment follows a bidirectional imbrication (Fig.\u0026nbsp;\u003cspan refid=\"Fig11\" class=\"InternalRef\"\u003e11\u003c/span\u003ea), indicative of unidirectional current regimes, which are responsible for the test fragmentation. In contrast, the lower parts exhibit disordered, swirl-like arrangements (Fig.\u0026nbsp;\u003cspan refid=\"Fig11\" class=\"InternalRef\"\u003e11\u003c/span\u003eb), reflecting localized soft sediment deformation, which suggests initial breakage due to hydraulic currents and subsequently due to soft-sediment deformation. SEM analysis reveals pyrite crystallization within some molluscan shells, suggesting microbial mediation supported by earlier works such as Folk (\u003cspan citationid=\"CR26\" class=\"CitationRef\"\u003e2005\u003c/span\u003e) and MacLean et al. (\u003cspan citationid=\"CR47\" class=\"CitationRef\"\u003e2008\u003c/span\u003e).\u003c/p\u003e\u003cp\u003e\u003c/p\u003e\u003cp\u003eThe dominance of \u003cem\u003eAssilina\u003c/em\u003e, coupled with increased biodiversity relative to the underlying lagoonal facies, suggests a transition from a restricted marginal marine environment to an open marine ramp setting. The variation in fragmentation, abundance, and sediment texture supports fluctuating hydrodynamic energy conditions, consistent with an environment shifting between middle and inner ramp settings.\u003c/p\u003e\u003c/div\u003e"},{"header":"4. Discussion","content":"\u003cp\u003eThe taphonomic features preserved across the Naredi Formation reflect a progressive transition from a restricted lagoonal setting to more open, higher-energy inner to mid-ramp depositional environments. This is evidenced by systematic changes in fossil assemblages, test preservation, sedimentary fabrics, and associated diagenetic modifications. Taphofacies A\u0026ndash;C are dominated by molluscan taxa (e.g., \u003cem\u003eTurritella\u003c/em\u003e, \u003cem\u003eCorbula\u003c/em\u003e), while Taphofacies D\u0026ndash;F witness a marked dominance of larger rotaliid foraminifera such as \u003cem\u003eAssilina\u003c/em\u003e and \u003cem\u003eNummulites\u003c/em\u003e, along with corals, ostracods, and bivalves. This upward diversification points to a transgressive trend marked by deepening water and increasing openness of the depositional environment. The interpretation of this transgression independently anchors glauconite occurrence to sedimentary condensation and slow sedimentation (Odin \u0026amp; Matter, 1981) while separately using the fossil assemblage composition and diversity trends as indicators of environmental shift. However, the presence of gypsum layers within Taphofacies C marks a significant departure from this deepening trend, recording short-lived regressive pulses or localized evaporitic conditions with elevated salinity, likely within a restricted lagoonal setting under semi-arid climatic influence. Such phases reflect relative sea-level fluctuations or climatic oscillations superimposed on long-term marine inundation.\u003c/p\u003e\u003cp\u003eFragmentation intensity varies across the succession, serving as a key taphonomic indicator. Importantly, fragmentation does not correlate linearly with increasing or decreasing water depth. For example, in Taphofacies B, which records evidence of current action, shows incredible preservation of \u003cem\u003eNummulites\u003c/em\u003e but fragmented Mollusca fossils. This suggests that fragmentation is governed not solely by water depth or energy conditions, but also by intrinsic properties of the bioclasts such as test shape, shell thickness, and internal architecture. The hydrodynamically stable \u003cem\u003eNummulites\u003c/em\u003e were less prone to mechanical damage, unlike the thin-shelled and bivalves. Shells of bivalves tend to separate shortly after death when the adductor muscles decay and the valves open, making them more prone to damage. So, while fragmentation is often used as a proxy for energy regimes (e.g., wave or current action), it is essential to interpret it in conjunction with other indicators such as test robustness, biotic activities, and overprinting by diagenetic processes. Overall, inner to middle ramp settings show better fossil preservation, with more intact and micritized tests, compared to the lagoonal facies dominated by disarticulated and poorly preserved specimens.\u003c/p\u003e\u003cp\u003eConcretions in Taphofacies A and D display contrasting formation mechanisms, reflecting distinct early diagenetic conditions. In Taphofacies A, carbonate concretions formed through concentric precipitation around small organic or skeletal nuclei, preserving fossils within the concretions. These patterns suggest early porewater-driven carbonate cementation, where favorable microenvironments promoted rapid mineral precipitation, which encapsulated fossils rapidly (Marshall \u0026amp; Pirrie, \u003cspan citationid=\"CR48\" class=\"CitationRef\"\u003e2013\u003c/span\u003e). The thick-walled, high-spired \u003cem\u003eTurritella\u003c/em\u003e shells were more resistant to post-burial damage than the thinner-shelled \u003cem\u003eCorbula\u003c/em\u003e (Kidwell, \u003cspan citationid=\"CR40\" class=\"CitationRef\"\u003e1991\u003c/span\u003e; F\u0026uuml;rsich \u0026amp; Oschmann, \u003cspan citationid=\"CR27\" class=\"CitationRef\"\u003e1993\u003c/span\u003e; Savazzi, \u003cspan citationid=\"CR65\" class=\"CitationRef\"\u003e1991\u003c/span\u003e). The co-occurrence of both articulated and fragmented bivalves suggests time-averaging or short-term reworking prior to concretion growth (Kidwell \u0026amp; Flessa, \u003cspan citationid=\"CR41\" class=\"CitationRef\"\u003e1995\u003c/span\u003e). In contrast, concretions in Taphofacies D, embedded within \u003cem\u003eAssilina\u003c/em\u003e-dominated packstones, are ferruginous and likely formed under suboxic conditions via microbial mediation, where iron was mobilized in pore waters and precipitated due to redox gradients (Raiswell, \u003cspan citationid=\"CR59\" class=\"CitationRef\"\u003e1971\u003c/span\u003e; Mozley \u0026amp; Davis, \u003cspan citationid=\"CR52\" class=\"CitationRef\"\u003e2005\u003c/span\u003e). The concentration of micritized \u003cem\u003eAssilina\u003c/em\u003e tests at concretion margins suggests that micritic envelopes acted as diffusion barriers, facilitating localized iron enrichment. Concretions in Taphofacies A (lagoonal) formed through early carbonate cementation around molluscan shells in low-energy settings, while those in Taphofacies D (inner ramp) are ferruginous and microbially mediated, reflecting diagenesis around micritized \u003cem\u003eAssilina\u003c/em\u003e.\u003c/p\u003e\u003cp\u003eMicritization of foraminiferal tests, especially in Taphofacies D-F, is interpreted as a result of microbial endolithic activity, often mediated by microborers in well-lit, shallow marine settings (Burchette \u0026amp; Wright, \u003cspan citationid=\"CR17\" class=\"CitationRef\"\u003e1992\u003c/span\u003e; Messadi et al., \u003cspan citationid=\"CR49\" class=\"CitationRef\"\u003e2019\u003c/span\u003e; Garuglieri et al., \u003cspan citationid=\"CR28\" class=\"CitationRef\"\u003e2024\u003c/span\u003e). While micritization is not exclusive to inner ramp settings, as it can occur wherever microbial colonization is active in the photic zone, it is most common in stable, low-sedimentation areas with prolonged seafloor exposure (Fl\u0026uuml;gel, \u003cspan citationid=\"CR25\" class=\"CitationRef\"\u003e2010\u003c/span\u003e). The inferred suboxic to hypersaline conditions evidenced by glauconite formation and gypsum deposition in Taphofacies A-C may have inhibited the activity of endolithic microorganisms that require stable, oxygenated substrates for bioerosion (Fl\u0026uuml;gel, \u003cspan citationid=\"CR25\" class=\"CitationRef\"\u003e2010\u003c/span\u003e; Macintyre et al., \u003cspan citationid=\"CR46\" class=\"CitationRef\"\u003e2000\u003c/span\u003e). Additionally, the spatial distribution of fossil concentrations and swirl-like arrangements of \u003cem\u003eAssilina\u003c/em\u003e and molluscs in Taphofacies F suggests soft sediment deformation, likely driven by liquefaction or fluidization due to seismic or hydrodynamic disturbance (Owen, \u003cspan citationid=\"CR57\" class=\"CitationRef\"\u003e1996\u003c/span\u003e), since there is no evidence of bioturbation.\u003c/p\u003e\u003cp\u003eThe results of this study substantiate previous interpretations of the Naredi Formation as a lagoonal to middle ramp depositional system (Keller et al., \u003cspan citationid=\"CR35\" class=\"CitationRef\"\u003e2013\u003c/span\u003e; Khozyem et al., \u003cspan citationid=\"CR39\" class=\"CitationRef\"\u003e2013\u003c/span\u003e; Srivastava \u0026amp; Singh, \u003cspan citationid=\"CR70\" class=\"CitationRef\"\u003e2017\u003c/span\u003e), while offering a more detailed reconstruction through the application of taphonomic criteria. Earlier studies in the Kutch Basin primarily focused on sedimentary facies, microfacies, and biofacies (e.g., Khanolkar \u0026amp; Saraswati, \u003cspan citationid=\"CR38\" class=\"CitationRef\"\u003e2019\u003c/span\u003e), with limited integration of taphonomic processes. The findings of this study show strong parallels with previous global research in both methodology and interpretation. Like Beavington-Penney (\u003cspan citationid=\"CR8\" class=\"CitationRef\"\u003e2004\u003c/span\u003e), Nebelsick et al. (\u003cspan citationid=\"CR54\" class=\"CitationRef\"\u003e2011\u003c/span\u003e), and Ćosović et al. (\u003cspan citationid=\"CR21\" class=\"CitationRef\"\u003e2012\u003c/span\u003e), the Naredi Formation exhibits systematic relationships between taphonomic features such as fragmentation, abrasion, and micritization and depositional energy gradients, supporting their model of facies-linked taphonomic variability. The occurrence of micritization restricted to the middle ramp settings in this study mirrors the energy-controlled micritization patterns observed in their work. Similarly, the selective preservation of foraminiferal tests and their micritic overprinting across facies aligns with the biological and post-burial alteration processes highlighted by Lipps (\u003cspan citationid=\"CR43\" class=\"CitationRef\"\u003e1988\u003c/span\u003e) and Loubere \u0026amp; Gary (\u003cspan citationid=\"CR45\" class=\"CitationRef\"\u003e1990\u003c/span\u003e). Consistent with the approaches of Babazadeh \u0026amp; Alavi (\u003cspan citationid=\"CR4\" class=\"CitationRef\"\u003e2013\u003c/span\u003e) and Tomassetti \u0026amp; Benedetti (\u003cspan citationid=\"CR75\" class=\"CitationRef\"\u003e2020\u003c/span\u003e), this study integrates taphonomic observations with microfacies analysis to interpret cyclic sedimentation and platform evolution during the Eocene, reflecting a comparable level of resolution in reconstructing shallow marine carbonate systems. Furthermore, the identification of \u003cem\u003eAssilina\u003c/em\u003e-rich assemblages showing bidirectional imbrication and specific test orientations in the Naredi Formation supports the interpretations by Jorry et al. (\u003cspan citationid=\"CR34\" class=\"CitationRef\"\u003e2006\u003c/span\u003e), Hadi et al. (2016), and Zohdi et al. (\u003cspan citationid=\"CR80\" class=\"CitationRef\"\u003e2013\u003c/span\u003e), who associated similar features with storm reworking, wave energy influence, and transport directionality on carbonate ramps. Overall, the present study confirms and extends these global findings, enhancing the comparative understanding of Eocene ramp systems. These findings not only position the Naredi Formation within global Paleogene carbonate ramp models but also offer a novel methodological contribution to Indian Eocene paleoenvironmental studies.\u003c/p\u003e"},{"header":"5. Conclusion","content":"\u003cp\u003eThis study provides the first comprehensive taphonomic analysis of the Naredi Formation, revealing a complex interplay of depositional environments, early diagenetic processes, and fossil assemblage dynamics. Through detailed evaluation of fragmentation, micritization, bioturbation, and bioclast arrangements, six distinct taphofacies have been identified that record a transition from a restricted lagoon to a more open marine ramp setting. The identification of five regressive phases and novel taphonomic features such as imbrication and soft sediment deformation significantly refines the paleoenvironmental interpretation of the Eocene in the Kutch Basin and establishes a new baseline for regional and global comparisons of Paleogene carbonate systems.\u003c/p\u003e"},{"header":"Abbreviations","content":"\u003cp\u003eLBF \u0026ndash; Larger Benthic Foraminifera\u003c/p\u003e\n\u003cp\u003eSEM \u0026ndash; Scanning Electron Microscope\u003c/p\u003e"},{"header":"Declarations","content":"\u003ch2\u003eFunding\u003c/h2\u003e\u003cp\u003eThis research has been funded by the Indian Statistical Institute, Kolkata, India\u003c/p\u003e"},{"header":"References","content":"\u003col\u003e\n \u003cli\u003eAhmad, S., Jalal, W., Ali, F., Hanif, M., Ullah, Z., Khan, S, Ali, A., Jan, I. U., and Rehman, K. (2015). Using larger benthic foraminifera for the paleogeographic reconstruction of Neo-Tethys during Paleogene. 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V., Lonsdorf, T., Christman, Z., Heierbacher, M., Kibelstis, B. J., Putnam, I., Boles, Z. M., Walsh, S., \u0026amp; Lacovara, K. J. (2021). Microstratigraphic analysis of fossil distribution in the lower Hornerstown and upper Navesink formations at the Edelman Fossil Park, NJ. Frontiers in Earth Science, 9, 756655. DOI: https://doi.org/10.3389/feart.2021.756655\u003c/li\u003e\n \u003cli\u003eWoRMS - World Register of Marine Species.\u0026nbsp;www.marinespecies.org.\u003c/li\u003e\n \u003cli\u003eWynne, A. B. (1867). Memoir on the Geology of Kutch, to accompany the map compiled by AB Wynne and F. Fedden during the season, 68, 1868-1869.\u003c/li\u003e\n \u003cli\u003eZohdi, A., Mousavi-Harami, R., Ali Moallemi, S., Mahboubi, A., \u0026amp; Immenhauser, A. (2013). Evolution, paleoecology and sequence architecture of an Eocene carbonate ramp, southeast Zagros Basin, Iran. GeoArabia, 18(4), 40-80. DOI: https://doi.org/10.2113/geoarabia180449\u003c/li\u003e\n\u003c/ol\u003e"}],"fulltextSource":"","fullText":"","funders":[],"hasAdminPriorityOnWorkflow":true,"hasManuscriptDocX":true,"hasOptedInToPreprint":true,"hasPassedJournalQc":"","hasAnyPriority":true,"hideJournal":false,"highlight":"","institution":"Indian Statistical Institute","isAcceptedByJournal":true,"isAuthorSuppliedPdf":false,"isDeskRejected":"","isHiddenFromSearch":false,"isInQc":false,"isInWorkflow":false,"isPdf":false,"isPdfUpToDate":true,"isWithdrawnOrRetracted":false,"journal":{"display":true,"email":"[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true},"keywords":"Taphofacies, taphonomy, larger benthic foraminifera, Naredi Formation, Eocene, Kutch Basin","lastPublishedDoi":"10.21203/rs.3.rs-7500403/v1","lastPublishedDoiUrl":"https://doi.org/10.21203/rs.3.rs-7500403/v1","license":{"name":"CC BY 4.0","url":"https://creativecommons.org/licenses/by/4.0/"},"manuscriptAbstract":"\u003cp\u003eThe Cenozoic marine sedimentation in the Kutch Basin, western India, initiated with the Naredi Formation, a dominantly argillaceous unit interbedded with a foraminiferal limestone. While the formation has been studied from sedimentological, paleontological, and geochemical perspectives, taphonomy remains largely unexplored. This study presents a novel classification of sedimentary rocks based on the taphonomic characteristics of embedded fossils, with the focus on Larger Benthic Foraminifera and Mollusca. Six Taphofacies are identified using the following criteria: fragmentation, imbrication, diagenetic alteration, type of preservation and packing, distribution of sizes, bioturbation, and articulation. The taphofacies, along with a detailed study of the existing horizons, indicate a more intricate depositional picture of the Naredi Formation than previously recognized. Notably, five transient regressive phases are identified, four of which coincide with Taphofacies C, marked by evaporite presence and lagoonal restriction, challenging earlier interpretations of a single transgressive\u0026ndash;regressive cycle. Taphonomic evidence also captures intra-horizon variability, including current-induced fragmentation in middle ramp deposits, microbial micritization of LBF tests, and soft-sediment deformation features. Overall, the integration of taphonomic, sedimentological, and paleontological data refines the lagoonal-to-open marine depositional model and highlights the utility of taphofacies analysis as a tool for reconstructing palaeoenvironmental and diagenetic histories.\u003c/p\u003e","manuscriptTitle":"Taphofacies from the lower Eocene Naredi Formation of Kutch Basin, western India, and their significance","msid":"","msnumber":"","nonDraftVersions":[{"code":1,"date":"2025-09-09 05:05:46","doi":"10.21203/rs.3.rs-7500403/v1","editorialEvents":[{"type":"communityComments","content":0}],"status":"published","journal":{"display":true,"email":"[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true}}],"origin":"","ownerIdentity":"f6a4113e-d8ef-43d4-9119-3f855b610000","owner":[],"postedDate":"September 9th, 2025","published":true,"recentEditorialEvents":[],"rejectedJournal":[],"revision":"","amendment":"","status":"published-in-journal","subjectAreas":[{"id":53957015,"name":"Geology"},{"id":53957016,"name":"Climate Analysis and Modeling"}],"tags":[],"updatedAt":"2025-09-29T19:41:44+00:00","versionOfRecord":{"articleIdentity":"rs-7500403","link":"https://doi.org/10.1007/s10347-025-00713-5","journal":{"identity":"facies","isVorOnly":false,"title":"Facies"},"publishedOn":"2025-09-25 00:00:00","publishedOnDateReadable":"September 25th, 2025"},"versionCreatedAt":"2025-09-09 05:05:46","video":"","vorDoi":"10.1007/s10347-025-00713-5","vorDoiUrl":"https://doi.org/10.1007/s10347-025-00713-5","workflowStages":[]},"version":"v1","identity":"rs-7500403","journalConfig":"researchsquare"},"__N_SSP":true},"page":"/article/[identity]/[[...version]]","query":{"redirect":"/article/rs-7500403","identity":"rs-7500403","version":["v1"]},"buildId":"8U1c8b4HqxoKbykW_rLl7","isFallback":false,"isExperimentalCompile":false,"dynamicIds":[84888],"gssp":true,"scriptLoader":[]}