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Genetic evidence for a fall spawning group of Gulf sturgeon (Acipenser oxyrinchus desotoi) in the Apalachicola River, Florida | bioRxiv /* */ /* */ <!-- <!-- /*! * yepnope1.5.4 * (c) WTFPL, GPLv2 */ (function(a,b,c){function d(a){return"[object Function]"==o.call(a)}function e(a){return"string"==typeof a}function f(){}function g(a){return!a||"loaded"==a||"complete"==a||"uninitialized"==a}function h(){var a=p.shift();q=1,a?a.t?m(function(){("c"==a.t?B.injectCss:B.injectJs)(a.s,0,a.a,a.x,a.e,1)},0):(a(),h()):q=0}function i(a,c,d,e,f,i,j){function k(b){if(!o&&g(l.readyState)&&(u.r=o=1,!q&&h(),l.onload=l.onreadystatechange=null,b)){"img"!=a&&m(function(){t.removeChild(l)},50);for(var d in y[c])y[c].hasOwnProperty(d)&&y[c][d].onload()}}var j=j||B.errorTimeout,l=b.createElement(a),o=0,r=0,u={t:d,s:c,e:f,a:i,x:j};1===y[c]&&(r=1,y[c]=[]),"object"==a?l.data=c:(l.src=c,l.type=a),l.width=l.height="0",l.onerror=l.onload=l.onreadystatechange=function(){k.call(this,r)},p.splice(e,0,u),"img"!=a&&(r||2===y[c]?(t.insertBefore(l,s?null:n),m(k,j)):y[c].push(l))}function j(a,b,c,d,f){return q=0,b=b||"j",e(a)?i("c"==b?v:u,a,b,this.i++,c,d,f):(p.splice(this.i++,0,a),1==p.length&&h()),this}function k(){var a=B;return a.loader={load:j,i:0},a}var l=b.documentElement,m=a.setTimeout,n=b.getElementsByTagName("script")[0],o={}.toString,p=[],q=0,r="MozAppearance"in l.style,s=r&&!!b.createRange().compareNode,t=s?l:n.parentNode,l=a.opera&&"[object Opera]"==o.call(a.opera),l=!!b.attachEvent&&!l,u=r?"object":l?"script":"img",v=l?"script":u,w=Array.isArray||function(a){return"[object Array]"==o.call(a)},x=[],y={},z={timeout:function(a,b){return b.length&&(a.timeout=b[0]),a}},A,B;B=function(a){function b(a){var a=a.split("!"),b=x.length,c=a.pop(),d=a.length,c={url:c,origUrl:c,prefixes:a},e,f,g;for(f=0;f<d;f++)g=a[f].split("="),(e=z[g.shift()])&&(c=e(c,g));for(f=0;f<b;f++)c=x[f](c);return c}function g(a,e,f,g,h){var i=b(a),j=i.autoCallback;i.url.split(".").pop().split("?").shift(),i.bypass||(e&&(e=d(e)?e:e[a]||e[g]||e[a.split("/").pop().split("?")[0]]),i.instead?i.instead(a,e,f,g,h):(y[i.url]?i.noexec=!0:y[i.url]=1,f.load(i.url,i.forceCSS||!i.forceJS&&"css"==i.url.split(".").pop().split("?").shift()?"c":c,i.noexec,i.attrs,i.timeout),(d(e)||d(j))&&f.load(function(){k(),e&&e(i.origUrl,h,g),j&&j(i.origUrl,h,g),y[i.url]=2})))}function h(a,b){function c(a,c){if(a){if(e(a))c||(j=function(){var a=[].slice.call(arguments);k.apply(this,a),l()}),g(a,j,b,0,h);else if(Object(a)===a)for(n in m=function(){var b=0,c;for(c in a)a.hasOwnProperty(c)&&b++;return b}(),a)a.hasOwnProperty(n)&&(!c&&!--m&&(d(j)?j=function(){var a=[].slice.call(arguments);k.apply(this,a),l()}:j[n]=function(a){return function(){var b=[].slice.call(arguments);a&&a.apply(this,b),l()}}(k[n])),g(a[n],j,b,n,h))}else!c&&l()}var h=!!a.test,i=a.load||a.both,j=a.callback||f,k=j,l=a.complete||f,m,n;c(h?a.yep:a.nope,!!i),i&&c(i)}var i,j,l=this.yepnope.loader;if(e(a))g(a,0,l,0);else if(w(a))for(i=0;i (function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start':new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0];var j=d.createElement(s);var dl=l!='dataLayer'?'&l='+l:'';j.src='//www.googletagmanager.com/gtm.js?id='+i+dl;j.type='text/javascript';j.async=true;f.parentNode.insertBefore(j,f);})(window,document,'script','dataLayer','GTM-M677548'); Skip to main content Home About Submit ALERTS / RSS Search for this keyword Advanced Search New Results Genetic evidence for a fall spawning group of Gulf sturgeon ( Acipenser oxyrinchus desotoi ) in the Apalachicola River, Florida View ORCID Profile Jacob O. Zona , Brian R. Kreiser , Adam J. Kaeser , Adam G. Fox , Mark J. D’Ercole doi: https://doi.org/10.1101/2025.01.29.635482 Jacob O. Zona 1 School of Biological, Environmental, and Earth Sciences, University of Southern Mississippi , Hattiesburg, Mississippi, USA 2 Department of Natural Resource Management, South Dakota State University , Brookings, South Dakota, USA Find this author on Google Scholar Find this author on PubMed Search for this author on this site ORCID record for Jacob O. Zona For correspondence: jozona{at}svsu.edu Brian R. Kreiser 1 School of Biological, Environmental, and Earth Sciences, University of Southern Mississippi , Hattiesburg, Mississippi, USA Find this author on Google Scholar Find this author on PubMed Search for this author on this site Adam J. Kaeser 3 Panama City Fish and Wildlife Conservation Office, U.S. Fish and Wildlife Service , Panama City, Florida, USA Find this author on Google Scholar Find this author on PubMed Search for this author on this site Adam G. Fox 4 Warnell School of Forestry and Natural Resources, University of Georgia , Athens, Georgia, USA Find this author on Google Scholar Find this author on PubMed Search for this author on this site Mark J. D’Ercole 4 Warnell School of Forestry and Natural Resources, University of Georgia , Athens, Georgia, USA Find this author on Google Scholar Find this author on PubMed Search for this author on this site Abstract Full Text Info/History Metrics Preview PDF Abstract The Gulf sturgeon ( Acipenser oxyrinchus desotoi ) is a large, long-lived, anadromous fish inhabiting the northern Gulf of Mexico. This charismatic fish was hunted to near extinction in the early 1900’s and in 1991 was listed as threatened under the Endangered Species Act. Recovery continues to be challenged by threats such as habitat destruction, fisheries bycatch, and climate change. There are seven known natal rivers, historically thought to each contain a single, spring-spawning group. In recent years, multiple rivers (Suwannee, Choctawhatchee) have been shown to contain a second, fall-spawning group. This study utilizes genetic techniques to investigate the proposed existence of a fall-spawning group in the Apalachicola River, Florida. This river once supported one of the largest Gulf sturgeon populations, but post-exploitation faces a difficult path to recovery. The Jim Woodruff Lock and Dam blocks access to the majority of historic habitat in the system, with the only known remaining spawning grounds located immediately downriver. Tissue samples from juvenile Gulf sturgeon were collected between 2013 and 2022 and used to assess genetic population structure within the Apalachicola River. Analyses suggested two distinct genetic groups (F ST = 0.085). Based on dates of capture, length frequency distributions, and genetic assignment of spawning adults, these were identified as spring- and fall-spawning groups. Approximately 90% of juveniles collected were assigned to the spring, but only slight differences in genetic diversity were detected between groups. The temperature window for spawning was found to be three weeks shorter on average in the fall than the spring, highlighting the need for additional research into differing environmental or anthropogenic influences on these populations. The discovery of a fall-spawning group of Gulf sturgeon in the Apalachicola River improves our understanding of the representation, redundancy, and resiliency of the species and provides critical information for improved management of this river system. Introduction The Gulf sturgeon ( Acipenser oxyrinchus desotoi ) is a large, anadromous fish native to the northern Gulf of Mexico [ 1 ]. Subadults and adults overwinter in the nearshore waters of the gulf, while juveniles spend the winter in the lower salinity estuaries. Each spring all age groups make the migration back into freshwater systems where they spend the remainder of the year [ 2 – 4 ]. Similar to other sturgeons, they reach sexual maturity late in life, 8 – 12 years, and females are suspected to have spawning intervals of multiple years [ 5 ]. This suite of life history traits makes them particularly sensitive to anthropogenic disturbances, and the subspecies was listed as ‘Threatened’ under the Endangered Species Act in 1991 [ 6 ]. Historic overfishing as well as habitat alteration and indirect fisheries mortality have led to range contraction, local extirpations, and severe declines in abundance [ 5 , 7 – 9 ]. Reproducing populations of Gulf sturgeon can be found in seven river systems and each was thought to be represented by a single group that spawned during the spring [ 6 ]. In 2012, Randall and Sulak [ 10 ] suggested the Suwannee River supported a fall spawning group based on evidence from adult sturgeon movements and sexual characteristics, as well as the size structure of the juvenile population. The capture of several unexpectedly small juveniles in 2013 and again in 2019 was subsequently interpreted by Dula et al. [ 11 ] as potential evidence of fall spawning in the Apalachicola River. Spawning runs of Atlantic sturgeon ( Acipenser oxyrinchus oxyrinchus ), a closely related congener, have been documented in both spring and fall seasons in several southern-latitude, Atlantic Coast systems [ 12 – 15 ], and these stocks were found to be genetically distinct [ 16 – 18 ]. A more comprehensive understanding of the genetic structure and timing of spawning within each Gulf sturgeon population is critical for effective management of the species, especially in regulated river systems where access to spawning habitat, and hydrologic conditions during spawning might influence overall reproductive success [ 19 – 21 ]. The Apalachicola is the largest river in Florida by discharge [ 22 ], and its watershed, referred to as the Apalachicola-Chattahoochee-Flint river basin (or ACF), drains approximately 5 million hectares (ha) of the Gulf Coastal Plain and Appalachian Mountains [ 23 ]. The ACF system is fragmented by numerous dams, five of which are major projects operated by the U.S. government (i.e., Army Corps of Engineers). Jim Woodruff Lock and Dam, completed in 1957 at the confluence of the Flint and Chattahoochee rivers, created Lake Seminole reservoir and permanently blocked access to approximately 78% of historic Gulf sturgeon habitat in the ACF system [ 6 ]. Only 50-80 ha of potentially suitable spawning habitat exists in the Apalachicola below the dam [ 24 , 25 ]. Concern for the potential impact of hydrologic operations on Gulf sturgeon spawning motivated studies in the 2000s that involved egg collections in the field, and modeling of the effects of recruitment failure on the trajectory of the Apalachicola population [ 26 – 28 ]. These studies were conducted during the spring. Spawning was documented via egg collections at 3 sites, all within 11 kilometers of the dam [ 27 ]. Eggs were collected between April 4 and May 14, at temperatures between 20 and 25 Celsius [ 28 ]. A relationship between discharge, the depth at which sturgeon eggs were collected, and inundated hard bottom habitat, served as basis for Flowers et al. [ 28 ] to hypothesize that a reduction in total area of spawning habitat during low flow conditions, and/or short-term variations in discharge resulting from hydropeaking operations, might periodically result in reduced or failed recruitment that would affect recovery of the Apalachicola population. Through consultation, this work led to changes in the way the Army Corps of Engineers managed flows in the system during the spring to reduce the likelihood of stranding sturgeon eggs and larvae during falling water levels [ 29 ]. Temperatures favorable for sturgeon spawning also occur in the Apalachicola River in the fall (Oct-Nov) [ 24 ]. However, fall spawning remained undocumented at the time of these consultations, and consequently a fall recruitment period was not taken into consideration. The existence of a fall spawning group in the Apalachicola River would have important management implications for this population, where recruitment of juvenile sturgeon appears to be relatively low [ 30 ]. Environmental variables such as temperature and flow may differ seasonally in the Apalachicola River [ 31 ], potentially warranting a closer look at their relationships with recruitment success during different spawning seasons. Knowledge of fall spawning would also contribute insights to studies of juvenile age, growth, and recruitment, and help inform the overall conservation status of the species. Thus, the purpose of this study was to use genetic techniques to investigate the purported existence of a fall spawning group in the Apalachicola River and to assess its level of genetic distinctiveness from the spring group. Methods Gulf sturgeon were sampled in the Apalachicola River from May through July of 2013–2022 by field teams from the University of Georgia and the U.S. Fish and Wildlife Service. All sampling was conducted following protocols set by International Animal Care and Use Committee Permits (A2019 01-002-Y3-A3, A2021 09-010-Y3-A3) and annual collections permits issued by the Florida Fish and Wildlife Conservation Commission to the U.S. Fish and Wildlife Service (e.g. 2024 FNW-005, FNW23-05, FNW22-03, FNW21-09, FNW20-06, FNW19-08). Fish were captured using anchored monofilament gill nets (45.7 x 3 meters) comprised of three equal-length panels of 7.6-, 8.9-, and 10.2-centimeter mesh stretch measure. Identical nets were used in previous studies to effectively capture juvenile Gulf sturgeon in the Apalachicola River [ 11 , 30 ]. Nets were soaked for 60–120 minutes, depending on conditions. Each weekday during the sampling season, 6–12 nets were set. Sampling was concentrated in the Brothers River, a coastal plain tributary of the Apalachicola River where Gulf sturgeon commonly aggregate; sampling also occurred in various reaches of the mainstem Apalachicola River [ 30 ]. All captured sturgeon were scanned for tags and, if not previously tagged, implanted with a unique passive integrated transponder tag. Each fish was measured, and a small (approximately 1 cm 2 ) tissue sample was taken from its anal fin for genetic analysis. Fish were then released back into the river near their site of capture. Tissue samples were stored in 95% ethanol at room temperature and shipped to the University of Southern Mississippi for analysis. All laboratory procedures were conducted in accordance with International Animal Care and Use Committee Protocol #17101202. Total genomic DNA was extracted from tissue samples using the DNeasy Tissue Kit (Qiagen, Inc., Valencia, California). Thirteen microsatellite loci were amplified (Atlantic sturgeon - Aox B34, Aox D32, Aox D44, Aox D54, Aox D64, Aox D165, Aox D170, Aox D188, Aox D234, Aox D241, Aox D242, and Aox D297 [ 32 ] and lake sturgeon - LS 68 [ 33 ]) using 12.5 µL polymerase chain reactions (PCR). PCR components consisted of 1x Taq PCR buffer (New England Biolabs, Ipswich, Massachusetts), 2.5 mM MgCl 2 , 200 µM dNTPs, 0.25 units of Taq polymerase, 0.16 µM of M13 tailed forward primer [ 34 ], 0.16 µM of M13 tailed reverse primer, 0.08 µM of M13 labeled primer (Eurofins, Inc., Louisville, Kentucky), 10-200 ng/µL of template DNA, and nuclease-free water to the final volume. Polymerase chain reaction thermocycling conditions were as follows: initial denaturing step of 94 °C for 2 min followed by 35 cycles of 30 sec at 94 °C, 1 min at 53-58 °C, and 1 min at 72 °C, followed by a final elongation step of 10 min at 72 °C. See Dugo et al. [ 35 ] for locus-specific annealing temperatures. Genotypes were visualized using a LI-COR 4300 DNA sequencer (LI-COR Inc., Lincoln, Nebraska). Previous fin ray aging work with juvenile sturgeon in the Apalachicola River indicated that age-1 fish ranged from 390 to 520 millimeters (mm) fork length (FL) [ 36 ]. To decrease the odds of including individuals that may have strayed into the Apalachicola from adjacent systems, only fish ≤520 mm FL were included in analysis [ 2 , 9 ]. The program STRUCTURE v. 2.3.4 [ 37 ] was used to characterize population genetic structure of Gulf sturgeon within the Apalachicola River. STRUCTURE uses a Bayesian approach to assign individuals, based on their multi-locus genotypes, to some number of different genetic groups (K) that are in Hardy-Weinberg and linkage equilibrium. An admixture model was run under the assumption of correlated allele frequencies between groups with population of origin information as a prior [ 38 ]. Values of K between 1 and 6 were tested, each with 20 iterations of 150,000 Markov chain Monte Carlo repetitions with burn-ins of 100,000. The most likely value of K was then determined by examining the average likelihood scores for each value of K and the Δ K analysis as performed by StructureSelector [ 39 ]. CLUMPP 1.1.2 [ 40 ] was used to summarize the STRUCTURE results across all iterations for the most likely value of K, and Distruct 1.1 [ 41 ] was used to create a bar chart of admixture proportions. Length frequency distributions for each genetic group were graphed in R v. 4.4.0 to help visualize differences in spawning season and birth year [ 42 ]. As part of a different study, four adult Gulf sturgeon were captured in spawning condition in the Apalachicola River during October of 2022. These individuals were genotyped based on the methods above and were added to the dataset. An additional STRUCTURE analysis was run under the same parameters to determine if these adults assigned to a distinct genetic group, presumably representing a fall spawn. Pairwise F ST between genetic groups was determined using the “hierfstat” package in R to provide insight into the degree of genetic divergence [ 43 ]. Calculation of 95% confidence intervals was conducted using 1,000 bootstrap samples. Several measures of genetic diversity were calculated for each group. GenAlEx v. 6.5 [ 44 , 45 ] was used to determine average number of alleles per locus (N a ), observed heterozygosity (H o ), and expected heterozygosity (H e ). Allelic richness (A R ) was also calculated using “hierfstat.” Differences between groups were tested for statistical significance using two-tailed, paired sample t-tests using loci as paired samples. If assumptions necessary for parametric tests were not met, Wilcoxon signed-rank tests were used. Goodness-of-fit to the normal distribution was assessed using the Shapiro-Wilk test and equal variance was assessed using the Bartlett’s test. All statistical tests were conducted in R v. 4.4.0 [ 42 ]. To evaluate when fall spawning might be occurring in the Apalachicola River and compare spring vs. fall spawning windows, we examined temperature records from the USGS Chattahoochee gage 02358000 located approximately 1 km upstream of the primary spawning site [ 28 ]. Complete temperature records were available from 2017 to 2023. These records were used to determine the total number of days in each spawning season with temperatures suitable for spawning, between 17.0 and 25.0 °C [ 7 ]. Results A total of 526 juvenile Gulf sturgeon were sampled from the Apalachicola River system during spring and summer (April 23 through July 29) of the years 2013 to 2022. Forty-five fish were excluded from the study, leaving a sample size of 481 individuals for analysis (S1 Table). Of the excluded samples, four had missing data at more than three microsatellite loci, three belonged to individuals sampled twice in different years, and thirty-eight were from individuals larger than our 520 mm FL threshold. The STRUCTURE analysis suggested there were two distinct genetic groups within the Apalachicola River ( Fig 1 ), based on the results of the ΔK analysis (S1 Fig). The average probability of ancestry (mean q-score)- or probability of belonging to a genetic group-was high for both groups (0.98 and 0.93; Table 1 ). Several samples from each group possessed q-scores that indicated mixed ancestry, including seven fish with q-scores of less than 0.70 for their primary group of origin. Each of the remaining 474 juvenile Gulf sturgeon were assigned to one genetic group or the other. Download figure Open in new tab Fig 1. Results of STRUCTURE analysis at K = 2 for Apalachicola River Gulf sturgeon. Vertical bars represent individual fish where the proportion of each color represents degree of ancestry to corresponding genetic group, with gray for the spring spawning group and white for the fall spawning group. Samples are grouped by capture year and sorted within by fork length from largest (left) to smallest (right). All fish were ≤520 mm FL and collected from 2013 – 2022. View this table: View inline View popup Table 1. Genetic comparisons of the spring and fall spawning groups of Gulf sturgeon in the Apalachicola River. Fourteen Gulf sturgeon ≤300 mm FL were captured across multiple sampling years. Through STRUCTURE analysis, thirteen of these individuals were assigned to Group 2 and one was suggested to be of mixed ancestry. This size class was previously inferred to have originated from a fall spawning event [ 11 ]. Additionally, all four of the adults captured in spawning condition during the fall were assigned to Group 2 during the second STRUCTURE analysis (mean q-score = 0.97). Using these fish as a reference, we classified individuals from Group 2 as fall spawned and those from Group 1 as spring spawned. The two groups of juveniles exhibited distinctly different length frequency distributions; fish classified as spring spawned exhibited a unimodal distribution, whereas fall spawned fish demonstrated a bimodal distribution ( Fig 2 ). During the summer capture period, the average fish in the spring spawned group was 451 mm FL and 95% of individuals were at least 390 mm FL ( Fig 2 ). In that same period, approximately half of the fall spawned fish were 250–400 mm FL (Group 2A), and the other half were >450 mm FL (Group 2B). Based on size, dates of collection, and the timing of favorable temperatures for spawning in the Apalachicola system [ 24 ], fish belonging to Group 2A were classified as spawned during the fall prior to their collection (i.e., actual age range 7-10 months old), and fish belonging to Group 2B were classified as spawned two fall seasons prior to collection (i.e., age range 19-22 months old). The fish of Group 1 were classified as spawned during spring of the year prior to their collection (i.e., age range 12-14 months). Download figure Open in new tab Fig 2. Juvenile length frequency distributions for spring and fall spawning groups of Gulf sturgeon in the Apalachicola River. All fish were sampled from 2013 – 2022 and ≤520 millimeters in fork length. Assignment of each sturgeon in the spring and fall groups to a birth year revealed distinct differences in the likelihood of encountering spring vs. fall spawned individuals through our sampling efforts ( Table 2 ). Across all study years, 90% of fish (n=427) were classified as spring spawned. We observed a cohort of spring spawned fish in every year of the study. In contrast, only 47 fall spawned individuals (10%) were collected; these fish were observed in only four out of ten years ( Table 2 ). Most fall spawned fish identified in this study (89%) were determined to have originated from spawning events in 2012 (n=19) and 2018 (n=23) ( Table 2 ). Seven fish of mixed ancestry were not assigned to a birth year and season during this analysis. View this table: View inline View popup Table 2. Birth year and spawning season for juvenile Apalachicola River Gulf sturgeon. Calculation of pairwise F ST found substantial genetic differentiation between the spring and fall groups (F ST = 0.085, 95% CI = 0.050 – 0.119). The number of alleles per locus (N a ) and allelic richness (A R ) were higher on average in the spring, however, only N a was found to be statistically significant (N a : p = 0.007, V = 64; A R : p = 0.094, V = 70). Measures of heterozygosity were similar between groups (H o : p = 0.9, t = 0.14, df = 12; H e : p = 0.6, V = 38) ( Table 1 ). Between 2017 and 2023, temperatures favorable for spawning during the spring occurred 64 days on average (range 52-75) between the months of March and May. Favorable temperatures for fall spawning occurred 43 days on average (range 25-64) between the months of October and November. Discussion This paper provides the most substantial evidence to date for the existence of a fall spawning group of Gulf sturgeon in the Apalachicola River. Coupled with other studies, this evidence indicates that fall spawning exists within the three easternmost rivers supporting Gulf sturgeon: the Apalachicola, the Choctawhatchee [46, S. Rider unpublished data], and the Suwannee [10, Price et al. In Review]. Considering the prevalence of dual spawning among southern Atlantic sturgeon populations [ 15 , 18 ], it is possible that additional fall spawning groups of Gulf sturgeon in other rivers remain to be identified. The two spawning groups of Gulf sturgeon in the Apalachicola River were found to be genetically distinct, with an F ST comparable to the values reported when comparing populations from adjacent rivers [ 35 , 47 ]. Temporally separated spawning groups in the Choctawhatchee River exhibited a similar level of genetic differentiation [ 46 ]. These findings mirror those for the Atlantic sturgeon, where the amount of genetic differentiation between groups that spawned in different seasons was comparable to that found between groups that occupied different rivers [ 18 ]. Gulf sturgeon are known to have high river-of-origin fidelity [ 3 , 8 , 9 , 35 ], which has led to considerable reproductive isolation between river systems [ 48 , 49 ]. The amount of genetic differentiation we observed between spring and fall spawning groups in this study suggests Gulf sturgeon also demonstrate high spawning season fidelity. Fall spawned juveniles were detected less frequently and in much lower overall numbers than spring spawned juveniles in the Apalachicola River. These differences could reflect lower recruitment success for fish spawned in the fall, fewer fall spawning adults, or a combination of both. In rivers hosting relatively small Atlantic sturgeon populations, inconsistent annual recruitment success has been identified as a potential barrier to recovery [ 30 ]. Environmental factors that influence Gulf sturgeon recruitment success may fluctuate seasonally or via human influence [ 7 , 28 , 29 ]. For example, this study found that the temporal window for favorable spawning temperatures appears to be about 3 weeks shorter on average in the fall. Further research is needed to assess how these variables may impact the reproductive success of different spawning groups in the Apalachicola River. Because age-1 juveniles were prioritized for this study, some discrepancy in the number of spring vs. fall spawned fish in the sample set may be explained by lower net vulnerability, as mesh sizes may have been too large for effective capture of fish in Group 2A (i.e., fall fish 450 mm FL) would likely have exhibited net vulnerability similar to the spring spawned juveniles. When considering fish in this size range (450-520 mm FL), the proportion of fall spawned juveniles is even lower (10% vs 8%). In the Suwannee River, spring adults are found in larger numbers than fall adults, although the discrepancy is smaller, accounting for approximately 65% and 35%, respectively [Price et al In Review]. Despite the lower abundance of fall spawned juveniles in the sample set, only slight differences in genetic diversity were found between spring and fall groups. The higher number of alleles found per locus in the spring could be attributed to larger sample size and allelic richness was not significantly different between groups. Gene flow across spawning seasons may help to buffer the loss of genetic diversity in smaller groups. Even low levels of gene flow between small populations can mitigate harmful effects associated with low effective population size, such as decreased heterozygosity [ 50 ]. Further research is necessary for a more complete genetic comparison of the conservation status of the two groups. The presence of a fall spawning population of Gulf sturgeon should be considered in the context of research into juvenile dynamics in the Apalachicola River, conservation status assessments, and future management decisions including operation of the Jim Woodruff Lock and Dam. The results of this study point to the merits of pairing genetics analyses with traditional aging techniques to more accurately assign juvenile fish to an exact birth season and year of origin. This knowledge should benefit studies that aim to model and compare the growth of juvenile sturgeon cohorts, both within and across populations. The ability to parse spring from fall spawned individuals also provides an opportunity to investigate patterns of recruitment success among spawning groups over time. Although additional work is necessary to determine whether environmental factors influence or favor the success of one spawning group over another, the ability to accurately classify juveniles to a birth year and season will remain a cornerstone of these investigations. With regard to conservation status, the discovery of temporal isolation within the Apalachicola River elevates the representation, or breadth of genetic diversity, known to exist within this species [ 51 ]. This fall-spawning group may contain an important set of unique genes and traits that aid in adaptation to a changing environment in the future [ 52 ]. Beyond genetic diversity, the existence of the fall spawning group also contributes crucial conservation elements of redundancy and resiliency [ 51 ], as first noted by Dula et al. [ 11 ]. These authors hypothesized that fall-spawning adults may have escaped a major mortality event caused by Hurricane Michael by remaining upriver in reaches that did not suffer hypoxia. Our study confirms that this fall 2018 spawn contributed to the number of juveniles captured in subsequent years. Given the importance of redundancy, resiliency, and representation to the overall conservation status and recovery of Gulf sturgeon, future investigations should focus on identifying additional fall spawning groups, evaluating factors supporting their existence, and enacting conservation measures to protect these stocks across the full range of the species. Supporting Information S1 Table. Juvenile Apalachicola River Gulf sturgeon dataset used in this study. Table contains microsatellite genotypes, capture date, and fork length (mm) for each sample. S1 Fig. ΔK analysis suggesting K = 2 for Apalachicola River Gulf sturgeon. All samples were ≤520 mm FL and collected from 2013 – 2022. To identify the most likely number of genetic groups, ΔK analysis determines the change in log likelihood of the STRUCTURE data between each value of K. Acknowledgements Thank you to Robbilyn Verges for assistance with genetic data collection, Jake Schaefer (University of Southern Mississippi) for graduate mentorship, and numerous technicians (University of Georgia) for their contributions in the field. This work is made possible through the continued collaboration of many partners at the U.S. Fish and Wildlife Service, National Marine Fisheries Service, Florida Fish and Wildlife Conservation Commission, University of Georgia, University of Southern Mississippi, Louisiana State University, and University of Florida. References 1. ↵ U.S. Fish and Wildlife Service and National Marine Fisheries Service. Gulf sturgeon (Acipenser oxyrinchus desotoi) 5-Year Review: Summary and Evaluation . Panama City (FL): U.S. Fish and Wildlife Service ; 2022 . 63 p. 2. ↵ Sulak KJ , Clugston JP. 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