Abstract
In order to describe large-scale spatial structure of Asian sockeye salmon the variability of 45 SNP loci
was analyzed in 22 samples from the North-West coast of the Pacific Ocean. Three large regional population
complexes were identified: southwestern Kamchatka, Kamchatka River basin, and the North-East (comprising
stocks from Koryak Highlands). Populations within the identified complexes are connected by gene migration and
have a common origin, close geographic proximity, comparable climatic, landscape and environmental conditions in
the freshwater and early marine periods of life. Populations confined to watersheds of the North coast of the Sea of
Okhotsk (Palana and Okhota rivers), along with island populations, displayed noteworthy distinctions from the
isolated population complexes. We hypothesize that the marked divergence observed in island populations is
primarily caused by genetic drift occurring during long periods of isolation. The pronounced divergence of Palana
River population may be the result of both genetic drift and natural selection, driven by the challenging
smoltification and juvenile transition to the ocean, along with local adaptations during spawning and early life
periods in the Palansky Lake. At the same time in the Okhota River population, demographic factors such as genetic
drift and bottlenecks played a key role.
Keywords
Oncorhynchus nerka, sockeye salmon, SNP, population structure, regional complexes, post-glacial
colonization, demographic processes, island populations
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Introduction
Sockeye salmon Oncorhynchus nerka (Walbaum) is a commercially important species that has been an
object of both fishery and artificial breeding across its extensive distribution range, which encompasses the entire
northern part of the Pacific Rim (Burgner, 1991). It is most numerous in the North America, where 80-85% of its
stock are reproduced, while Asian populations contribute to about 15-20% (Forrester & C.R., 1987; Bugaev, 2011).
Sockeye salmon has the most complex population structure among all species within the genus Oncorhynchus.
Large populations of Pacific salmon display metapopulation characteristics (Schtickzelle & Quinn, 2007). This
implies that they comprise a system of relatively isolated populations interconnected through minimal individual
migrations and capable to extinction and subsequent recolonization at the expense of other components of the
system. Such dynamics contribute to the overall stability of the system over successive generations. In general,
populations of sockeye salmon from different rivers are subdivided into distinct local subpopulations and seasonal
races, which spawn during the summer (early form) and autumn (late form) (Burgner, 1991; Quinn, 2005). Apart
from temporal and geographic intraspecific units, sockeye salmon exhibit a life-history dichotomy in their
freshwater rearing environments (life-history ecotypes) (Quinn, 2005; Wood et al., 2008): lake-type populations rear
in lakes for one to three years (more often two years) before travelling to the ocean to feed whereas sea/river
populations rear in river habitats normally for one year, or even less (Pavey et al., 2010). Foraging, water current,
and predation differ significantly between the lake-type and riverine populations affecting stable morphological and
genetic differences arising as a consequence of local adaptations and isolation by adaptation (Lin et al., 2008). For
instance the river ecotype has a deeper, shorter caudal peduncle associated with swimming against a current and a
deeper body, whereas lake
‐ type sockeye salmon have a more streamlined body shape (Pavey et al., 2010).
Furthermore, sockeye salmon has high-level organization of population systems, such as large regional population
complexes (Varnavskaya, 2006) or eco-geographic units (EGUs) (Zhivotovsky, 2016). Although both concepts are
largely similar, the first one has a slightly broader scope, and we will adopt it for future use. Such complexes have
their own biological, ecological, demographic and genetic characteristics and diverse local adaptations to a variety
of environmental conditions, which allows the entire system to survive with significant environmental changes and
anthropogenic pressure due to the restoration of endangered components at the expense of other populations of the
same complex (Hilborn et al., 2003). These complexes are formed due to the shared descent, robust connectivity
through migratory patterns, congruent adaptations arising from similar ecological and physical-geographical habitat
attributes, and stabilization driven by ecological diversification (Olsen et al., 2008). The sustainability of population
systems (both metapopulations and regional complexes) of sockeye salmon is maintained by their inherent
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biocomplexity. Within the context of Pacific salmon, biocomplexity is an interconnected network of local
populations that as a whole maintain a relatively constant overall stock productivity, achieved through diverse
components and a range of life strategies (Hilborn et al., 2003).
Since 2017, in a number of watersheds of Kamchatka, significant changes in the dynamics of the spawning
run, biological indicators, and intrapopulation diversity of sockeye salmon have been observed. These changes have
arisen as a consequence of density-dependent, trophic, and both local and global climatic and hydrological factors.
However, the primary driver has been an imbalanced
pressure on the population system components stemming
from unsustainable management practices and non-selective fishery (Lepskaya et al., 2017; “Information …,” 2019;
Koval et al., 2020). The main reason is the insufficiency or ignorance of information regarding the population
structure, ecological dynamics, and temporal differentiation of salmon populations during the in the planning and
organization of fishing. The organization of sustainable fishery, coupled with the protection, artificial propagation,
and management of salmon populations, requires an extensive scientific base. This base should encompass
fundamental aspects such as the delineation of exploited stock boundaries,
assessment of biocomplexity, genetic
diversity, adaptive capabilities, and constraints. It should also encompass considerations of conservation prospects,
especially in scenarios involving intensive artificial reproduction and opportunities for recolonization in the event of
overexploitation. It is also important to assess the background for successful recolonization, evaluate the potential of
donor populations, and gauge the reproductive success of migrating individuals. A comprehensive, large-scale
investigation into the population structure of Asian sockeye salmon, involving the identification of regional
population complexes, their differentiation, and an exploration of their origin and historical development, will
provide valuable insights into the demographic, ecological, and evolutionary processes occurring within these
systems. Such a study has the potential to address, if not fully answer, many of the questions that have been raised in
this context.
Over 95% of Asian sockeye salmon stocks are concentrated within the Kamchatka Peninsula, with primary
reproduction centers in the Kamchatka (East coast) and Kurilskoe Lake, Ozernaya (South-West coast) river basins.
In these watersheds, about 80–90% of the total catch of the species in the Russian Far East is annually caught
(Bugaev, 2011). Among secondary sockeye salmon stocks, several distinct populations have a relatively high
abundance: on the west coast it's the populations of the Bolshaya and Palana rivers, in the east of Kamchatka –
Apuka R. and Pakhacha R. populations (Shubkin & Bugaev, 2023). Chukotka is the second most important region
of sockeye salmon reproduction in Asia after the Kamchatka peninsula. In the watersheds of Eastern Chukotka, the
largest population of sockeye salmon inhabit the Meinypylgin lake-river system (Golub, 2003). On the North
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Okhotsk coast, sockeye salmon is not numerous. The largest stock of the Okhotsk region is reproduced in the basin
of the Okhota river (Nikulin, 1975). However, it is not large and has no significant commercial value (Chereshnev,
2008). Relatively small populations of sockeye salmon inhabit watersheds of the Commander Islands, Hokkaido
Island and the Kuril Islands − Shumshu, Paramushir, Urup and Iturup (Shedko, 2002; Zhulkov et al., 2012). Despite
their limited commercial significance and relatively small numbers, island populations of sockeye salmon are of
exceptional scientific interest and may provide important insights into the origins and evolutionary history of
sockeye salmon in Asia. Moreover, these island populations are a convenient model for studying microevolutionary
processes and potential pathways of adaptive evolution within the species. Island populations frequently exhibit
unique ecological, morphological, and genetic characteristics, a phenomenon known as the 'island syndrome', which
is formed as a result of historical and demographic processes and under the influence of climatic, orographic,
ethological and biocenological factors in conditions of isolation (Baeckens & Van Damme, 2020).
The distinctive characteristics that make the island's biodiversity so special also make it particularly
susceptible and vulnerable. The level of diversity in island populations is usually low, and besides, their numbers are
not large, all this makes them more prone to extinction. Furthermore, due to restricted resources, reduced abilities to
disperse, and residence in relatively stable and predictable marine climates, island populations, often located at
range edges, are more vulnerable to limiting factors. They evolve survival strategies developing local adaptations,
interdependence, co-evolution, and mutual influence within limited list of species and factors, rather than broad
defense mechanisms against a wide array of predators, competitors, infections, and variable physical environmental
conditions. Consequently, a disproportionately high number of species extinctions have been recorded on islands
compared to continental systems. Island populations are exceptionally vulnerable to anthropogenic impacts and
demand focused efforts and specific conservation measures. Therefore, it is of the utmost importance to identify and
assess complexes of island populations to determine their conservation potential.
Asian sockeye salmon island populations remain inadequately explored due to their limited numbers,
logistical challenges due to the remote and inaccessible locations, and the complexities associated with organizing
fisheries in uninhabited areas. However, between 2006 and 2014, we were able to collect samples from several
sockeye salmon nursery lakes on the Kuril and Commander Islands. The study of the polymorphism of the mtDNA
control region showed that the sockeye salmon from the lakes of Iturup Island was characterized by moderate
haplotype and nucleotide diversity, while the genetic diversity of the sockeye salmon from the Northern Kuriles and
Bering Island was significantly lower compared to the continental populations (Khrustaleva, 2016; Khrustaleva et
al., 2020). Furthermore, unique haplotypes were found within the South Kuril sockeye salmon populations, which
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are transitional forms between two Asian mtDNA haplogroups. We believe that these populations of sockeye
salmon may have originated from the southern refugium that existed during the last Pleistocene regressions in the
Hokkaido region and may have avoided secondary contact during the last wave of colonization of the Asian coast in
the early Holocene.
Given the limited number of marker-based genetic studies on Asian sockeye salmon, our primary objective
is to conduct a comprehensive investigation into the population structure of this species on a regional scale,
encompassing its entire distribution range along the West Coast of the Pacific Ocean. We will place particular
emphasis on studying island populations, which face heightened vulnerability due to global climate change in the
North Pacific and escalating anthropogenic pressures. Additionally, we aim to identify regional population
complexes that can act as protective buffers for these island populations, helping to mitigate the negative impact of
environmental changes or unsustainable commercial human activities. Finally, our research will explore the
ecological, genetic, and historical factors that contribute to the distinctions observed among the complexes and
populations of Asian sockeye salmon.
Materials and methods
Study area and sample collection
The samples were collected in 2003 through 2008 in the rivers of the East and West coasts of Kamchatka
peninsula, Chukotka peninsula, mainland coast of the Sea of Okhotsk, Kuril and Commander Islands (Table 1,
Figure 1). Sockeye salmon adults were caught using river seine nets in the river beds and lake creeks at a distance of
5-30 km from the river mouth during the mass run of sockeye salmon, as well as directly in the spawning lakes
(Supplementary Table S1). Most Kamchatka samples were obtained from fishing companies directly after catch in
local fisheries. In the Bolshaya River, smelt juvenile fishes were caught using minnow seine in the upper reach of
Plotnikov River and in the lower course of Bystraya River (Supplementary Table S1, Figure 1). The pectoral fin and
liver tissue samples were fixed in 96% ethanol.
SNP genotyping and data borrowing
Genomic DNA was extracted with Qiagen DNeasy 96 tissue kits (Qiagen, Valencia, California). TaqMan-
PCR using Fluidigm 96.96 Dynamic Arrays (Fluidigm, San Francisco, California) allowed for the genotyping of 95
individuals per 96- well plate (with one inlet used as a no-template control using tris-EDTA buffer) was carried out
following the protocol of Seeb et al. (Seeb et al., 2009). All individuals (n = 1226) were genotyped for 45 SNP loci
(Habicht et al., 2010) including three mitochondrial and 42 nuclear loci localized in structural and regulatory genes,
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dispersed repeats, and EST (Supplementary Table S2). In total 22 sockeye salmon samples from 14 localities of the
Asian coast of the Pacific Ocean were analyzed. For a more extensive analysis of the regional subdivision of
Kamchatka sockeye salmon, open data on the same set of loci (http://www.tandfonline.com/doi/suppl/10.1577/T09-
149.1?scroll=top) of Dr. C. Habicht and coauthors (Habicht et al. 2010) were used (Supplementary Table S3, Figure
S1). Hereinafter, the One_ prefix in loci names is omitted for brevity.
Fig. 1. Schematic map of the study area with sampling points (triangles). The point's annotations are given
in Table. 1. Regional complexes of Asian sockeye salmon are marked with different colors.
Statistical analysis
Allelic frequencies, observed and expected heterozygosities ( Ho, He) for each locus (excluding mtDNA
SNPs), and estimates of the allelic richness ( Ar) by rarefaction using the smallest sample size were obtained in
hierfstat (Goudet, 2005). Deviations from Hardy-Weinberg expectation (HWE) were evaluated across all loci for
each population by exact test (using the Markov chain (MC)) implemented in GENEPOP v4.0 (Raymond &
Rousset, 1995). Default parameters were used for the MC algorithm (dememorization = 1,000; batches = 20;
iterations per batch = 5,000). The Weir and Cockerham (1984) FST and F IT statistics for each locus and global FST
statistics as well as exact G-tests for genic and genotypic differentiation were calculated using GENEPOP v4.0.
Tests for linkage disequilibrium between all loci pairs were performed using simulated exact tests in GENEPOP
v4.0. Benjamini-Hochberg FDR correction was applied for all multiple tests. The necessary condition for pooling of
putatively linked loci was established as in (Habicht et al., 2010): if tests for linkage disequilibrium are significant in
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more than half of the samples, then either the less informative locus from the pair is dropped or the two loci is
combined into a composite genotype. All three mtDNA SNPs were combined into a composite haplotypes for
baseline evaluation ( Cytb_CO). In order to select a set of neutral loci, a panel of 45 SNP markers was iteratively
screened to identify outlier loci at different spatial scales, either analysing all population samples together or
evaluating various combinations of samples from different locations (Supplementary Figure S2). Outlier detection
was performed using coalescent simulations under the hierarchical island model to obtain p-values of the locus-
specific F-statistic conditioned on observed levels of heterozygosities implemented in in Arlequin 3.5 (Excoffier &
Lischer, 2010). The isolation by distance hypothesis was tested using the Mantel-tests for putatively neutral loci in
the ade4 R package (Dray & Dufour, 2007). The evidence of population "bottlenecks" was identified using the
Bottleneck 1.2.02 (Cristescu et al., 2010). This analysis is based on the loss of rare alleles predicted in recently
bottlenecked populations, resulting in heterozygosity excess. As this method assumes that markers are selectively
neutral, we only used non-outlier loci. We used the infinite alleles model (IAM) as the most appropriate
evolutionary model for SNP loci. To test for significant heterozygosity excess compared to the level predicted under
mutation-drift equilibrium, we used three tests: a sign test, a standardized differences test, and a one-tailed Wilcoxon
signed rank test. A bottleneck was considered verified if all three tests were significant.
The Cavalli-Sforza chord distances evaluation and reconstruction of trees by the Neighbors Joining (NJ)
Method
were carried out in Rphylip package (Felsenstein, 1989). Based on the distance matrices and the obtained
bootstrap estimates (1000 iterations), a phylogenetic networks were built using the Neighbor-Net (NN) algorithm in
the phangorn R package (Schliep, 2011). Principal coordinate analysis (PCoA) based on Euclidian distances
between individual genotypes was carried out in hierfstat (Goudet, 2005). Principal component analysis (PCA) was
performed using the R libraries factoextra (Kassambara & Mundt, 2020) and FactoMineR (Lê et al., 2008). The
discriminant analysis of principal components (DAPC) was performed using adegenet 1.3-1 R package (Jombart &
Ahmed, 2011). The population structure was assessed de novo, pre-determining the number of clusters in the entire
dataset using iterative analysis of k-means. The optimal number of clusters (K), or genetic groups, is often defined
as the K with the lowest Bayesian criterion (BIC) values among the identified clusters. However, we opted to use
the scree test (choosing a point on the curve of BIC dependence on the number K after which the average rate of
change of the function is significantly reduced). The DAPC procedure then used the optimal number of groups and
the first 32 identified principal components. On the next step, the probabilities of each genotype belonging to a
given cluster were graphically visualized.
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Table 1. Samples characteristics, regions and locations, population IDs, date of catch, and summary statistics for 40 SNP loci: mean ex pected ( He) and observed ( Ho)
heterozygosities, allelic richness ( Ar), the inbreeding coefficients ( FIS), the results of the exact tests on Hardy–Weinberg equilibrium ( HWE p-value), and the results of sign test
(psign), standardized differences test (pstdv) and two-tail Wilcoxon sign-rank tests (pW) for heterozygote excess, * − p < 0.05, ** − p < 0.01, *** − p < 0.001.
# Region Location Pop ID Date of catch n H e(SD) H o(SD) Ar (SD) F IS HWE p-
value psign p stdv p W
1 Chukotka, Navarinsky
region Vaamochka Lake Ch July 2004 50 0,26(0,2) 0,24(0,01) 1,8(0,55) 0,07 0.999 0.006** 0.002** 0.006**
2
Kamchatka peninsula,
Olyutorsky region
Apuka River, early run KAerl June 2008 18 0,26(0,19) 0,24(0,01) 1,82(0,53) 0,09 0.983 0.001** 0.01* 0.019*
3 Apuka River, late run KAlt June 2008 28 0,25(0,18) 0,22(0,02) 1,87(0,49) 0,09 0.997 0.127 0.139 0.29
4 Pakhacha River KPh June 2005 59 0,27(0,19) 0,24(0,01) 1,86(0,46) 0,13 0.265 0.049* 0.095 0.38
5
Kamchatka peninsula,
East coast
Kamchatka River, late run KK-04 June-July 2004 82 0,25(0,19) 0,21(0,01) 1,78(0,43) 0,15 0*** 0.002** 0*** 0.007**
6 Kamchatka River, early run KK-05 June 2005 15 0,27(0,22) 0,23(0,02) 1,74(0,58) 0,17 0.251 0*** 0*** 0***
7 Azabachje Lake, Bushuyka River KKa July 2004 81 0,25(0,19) 0,24(0,01) 1,76(0,42) 0,03 0.974 0*** 0*** 0.003**
8 Commander Islands Bering Island, Sarannoye Lake BS August 2007 58 0,18(0,2) 0,17(0,01) 1,63(0,58) 0,01 0.832 0.265 0.179 0.369
9 Continental coast of the
Sea of Okhotsk Okhota River Okh July 2004 80 0,24(0,21) 0,21(0,01) 1,68(0,47) 0,13 0.049* 0.043* 0.003** 0.027*
10 Kamchatka peninsula,
North-West Palana River KP July 2003 94 0,25(0,19) 0,22(0,01) 1,73(0,45) 0,09 0.982 0.001** 0.001** 0.003**
11
Kamchatka peninsula,
West coast
Bolshaya Vorovskaya River KV July 2007 45 0,24(0,2) 0,23(0,01) 1,8(0,51) 0,03 1 0.085 0.02* 0.05
12 Bolshaya River KB-03 July 2003 91 0,25(0,19) 0,22(0,01) 1,82(0,5) 0,14 0.104 0.086 0.007** 0.046*
13 Bolshaya River KB-04 August 2004 90 0,26(0,2) 0,24(0,01) 1,83(0,49) 0,1 0.004** 0.083 0.009** 0.046*
14 Bolshaya River drainage, Bistraya
River KBb July-August 2004 33 0,25(0,21) 0,24(0,01) 1,79(0,53) 0,02 0.909 0.146 0.018* 0.105
15 Bolshaya River drainage,
Plotnikova River KBp August 2004 39 0,26(0,21) 0,22(0,01) 1,79(0,53) 0,15 0.551 0.026* 0.006** 0.027*
16 Opala River KOp-07 July 2007 50 0,23(0,19) 0,21(0,01) 1,77(0,45) 0,12 0.884 0.038* 0.034* 0.096
17 Opala River KOp-08 July-August 2008 31 0,25(0,2) 0,24(0,01) 1,83(0,5) 0,04 1 0.107 0.033* 0.137
18 Ozernaya River KO August 2003 95 0,25(0,2) 0,24(0,01) 1,82(0,48) 0,05 0.667 0.05 0.014* 0.098
19
North Kuril Islands
Shumshu Island, Bettobu Lake NKS August 2008 50 0,22(0,21) 0,21(0,01) 1,71(0,55) 0,06 0.732 0.247 0.044* 0.245
20 Paramushir Island, Glukhoye Lake
(Shumnaya Ryver) NKP July 2008 48 0,17(0,17) 0,16(0,01) 1,67(0,53) 0,08 0.617 0.145 0.091 0.167
21 South Kuril Islands Urup Island, Tokotan Lake SKU July-August 2008 35 0,18(0,21) 0,18(0,01) 1,58(0,58) 0 0.053 0.177 0.1 0.117
22 Iturup Island, Krasivoye Lake SKI October 2006 50 0,17(0,21) 0,17(0,01) 1,55(0,61) 0,01 0.924 0.099 0.026* 0.068
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Further clustering analyses were completed with STRUCTURE (Pritchard et al., 2000) where three
independent runs for each number of cluster − K (2–22) were conducted using the admixture model at 50,000
iterations with a burn-in of 10,000. The most probable number of population clusters was determined by the
estimation of Δ K in STRUCTURE HARVESTER (Earl & vonHoldt, 2012). In the last step, we used GENELAND
v.0.3 (Guillot et al., 2008), which incorporates geographic information (coordinates) in order to estimate the number
of panmictic groups and locating their spatial boundaries. The model used was the correlated frequency model, and
a posterior probability map at the optimal cluster number, K = 8, was built, using 100000 Markov chain Monte
Carlo (MCMC) iterations, with a thinning interval of 10000. Data visualization was performed in R using ggplot2
library.
Results
Characteristics of loci and Diversity within Asian Sockeye Salmon Populations
Of the 45 loci analyzed, 43 were polymorphic in at least one sample, with the exception of p53-576 and RAG1-
103. The tests for linkage disequilibrium (LD) for the MHC2_190v2 and MHC2_251v2 loci were significant in
seven out of 22 samples, which did not satisfy the linkage criterion by Habicht at al. (Habicht et al., 2010).
Concurrently, these two substitutions are located within the Onne-DAB gene of the Major Histocompatibility
Complex (MHC) at a distance of 62 base pairs from each other. This physical proximity strongly indicates linkage,
prompting their analysis both independently and as a single linkage block or a locus, denoted as MHC2, with distinct
allelic/genotypic variants referred to as haplotypes/genotypes. LD-tests also revealed a correlation between the
genotypes of two pairs of loci GPDH − GPDH2 and GPH-414 − MHC2_251 in the sample from the Kamchatka
River (2004) and the zP3b − MARCKS-2 pair in the sample of the Bolshaya River (2003) (Fig. 2A). Nonetheless, it
is evident that there is insufficient basis to their blocking. Thus, after exclusion of monomorphic and blocking of
linked loci, the number of analyzed SNPs decreased to 40.
Estimates of intrapopulation genetic diversity in 22 samples of sockeye salmon are given in Table. 1,
Supplementary Table. S3, and Figure S2. After FDR correction, a significant deviations from Hardy–Weinberg
equilibrium was noted in samples from the mouth of the Bolshaya River (KB-03 and KB-04) at the ZNF-61 locus
(KB-03: p = 0.0004, F
IS = 0.39; KB-04: p = 0.0002, FIS = 0.40) and in the sample from the Okhota River (Okh) for
the GPH-414 locus (p = 0.0001, FIS = 0.42). In addition, significant deviations from HWE expectations were
revealed for the loci of the MHC2 complex: when they were considered separately, a significant deficit of
heterozygotes for both loci was noted in the sample from the mouth of the Kamchatka River (KK-04)
(MHC2_190v2: p = 0.0004, FIS = 0.65; MHC2_251v2 : p = 0, FIS = 0.95) and for the MHC2_251v2 locus in the
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sample from the Plotnikova River (KBp) ( p = 0.0003, FIS = 0.61). In total, for all loci, tests for HWE were
insignificant only in three samples after FDR-correction (Table 1).
Population Differentiation: Understanding Genetic Variation and Structure
The heterogeneity of allelic and genotypic frequencies in all dataset was revealed by the results of G-test on
genic and genotypic differentiation of populations. No significant inter-sample differences were found only for some
loci − ctgf-301, U502-167, MARCKS-241, Tf_ex3-182, and RH2op-395. By the results of paired tests the alleles and
genotypes frequencies of SNP loci did not differ significantly (after FDR correction) in samples from the rivers of
the Koryak Highlands (KA and KPh), from the lower reaches of the Kamchatka River, and from watersheds of the
South-East coast of the Kamchatka Peninsula (Fig. 2B).
The intersample genetic diversity, estimated by the FST value, averaged 0.135 (p = 0). For individual loci it
varied from 0.0009 ( MARCKS-241) to 0.405 ( serpin). According to the matrix of paired FST, a pronounced
differentiation of sockeye salmon from the South Kuril Islands and Paramushir Island, as well as the proximity of
the populations of Southwestern Kamchatka, including the Shumshu Island, and the relatively high similarity of the
populations of the Koryak Highlands (Ch, KA and KPh) are clearly traced (Fig. 2B).
Fig. 2. (A) The results of the LD-tests are presented as the heat map, below the diagonal − the significance
levels ( p-values) when testing the hypothesis about the genotypic equilibrium, above the diagonal − significant
deviations from the equilibrium after FDR correction. Mitochondrial loci were excluded from this analysis; ( B)
Pairwise F
ST matrix for Asian Pacific Coast sockeye salmon samples (below the diagonal). Above the diagonal −
shaded cells indicate non-significant differences in paired exact-tests on genic differentiation after FDR correction.
Sample annotations are given in Table. 1.
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11
Clustering with PCoA, PCA, DAPC, and phylogenetic relationships of populations
As a reconnaissance study of the population structure of sockeye salmon in Asia, a PCoA analysis of
individual genotypes of sockeye salmon from various localities of the Asian part of the range was carried out
(Supplementary Figure S3). On the corresponding graph, it is difficult to delineate most of populations clusters, but
individuals caught in the lake-river systems of the Southern and Northern Kuril Islands (samples SKI, SKU and
NKP) and the North coast of the Sea of Okhotsk (samples KP and Okh) are well separated from the main point pool.
To distinguish regional groups of populations, the samples were ordinated on the space of main principal
components using the PCA (Fig. 3A). In sum, four main components were identified, explaining in total more than
half of the variability (53.4%) of the genetic traits (allelic frequencies of 40 polymorphic SNP loci). The first
component explains primarily the variability of the two loci – serpin and HGFA, as well as two mass haplotypes of
the mtDNA locus; the second − STC-410, ACBP-79, GPH-414 (Supplementary Figure S4).
In the space of the first two principal components, the samples of sockeye salmon from western and eastern
Kamchatka formed a dense cluster. Near the cluster there were located samples from the watersheds of the mainland
coast of the Sea of Okhotsk (Okh) and Bering Island (BS). (Fig. 3A). Populations of the coasts of the North-East
Kamchatka and Chukotka were isolated from this cluster along the second component. In addition, the Palana River
sample was distant from the other populations of the West Kamchatka peninsula along the both components,
whereas the third component differentiated the Palana sample to the greatest extent. The island populations of the
North and South Kuril Islands were the most divergent from the others. (Fig. 3A). However, attempts to separate
clusters corresponding to regional groupings of sockeye salmon were not successful. Furthermore, the proportion of
genetic trait variability explained by the first pairs of components was relatively small, not exceeding 35%. This
suggests that a significant percentage of genetic variability may be attributed to other factors requiring more
scrupulous analysis. To achieve a higher level of detail, we conducted a PCA analysis that incorporated our own
dataset, supplemented by data from (Habicht et al., 2010). By including thirteen samples from Kamchatka
populations (Supplementary Table S3, Figure S1) we were able to differentiate large regional complexes of South-
West Kamchatka (the South-West SW), Koryak Highlands including North-Eastern Kamchatka and Chukotka (the
North-East, NE), as well as the Kamchatka river basin (KR) (Fig. 3B).
To classify individual genotypes and delineate the genetic subdivisions of sockeye salmon along the Asian
Pacific coast, we conducted DAPC analysis employing a de novo clustering approach, enabled the identification of
distinct groups (K=8) within the entire dataset (Supplementary Figure S5, Fig. 3C). Certain groups were represented
by of individual populations: from Paramushir Island, Bering Island, as well as Palana and Okhota rivers, as
depicted in Figure 3D. The mainland populations were divided into three large regional clusters corresponding to
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those identified earlier: SW (including the Shumshu Island), NE, and KR. Two samples from the South Kuril
Islands were combined into a separate cluster (Fig. 3D).
To elucidate population relationships and the proximal chronological sequence of their divergence, we
attempted to construct a split phylogenetic network. The original tree and the resulting network had a star-shaped
topology and were divided into 2 clusters formed by Kamchatka peninsula populations on one side, and NE
complex, the North Okhotsk sea coast (KP & Okh), and all island populations on the other (Fig. 4A). The network's
topology revealed four distinct clusters, corresponding to the population groupings the same as in P
С A and DAPC
tests. Notably, samples from the North Okhotsk sea coast and all island populations exhibited substantial
divergence. The low bootstrap support observed in the source tree underscores the inherent instability of the net
topology.
To enhance the accuracy of our phylogenetic reconstruction, we attempted to eliminate loci that may be
subject to selection, potentially distorting the tree's topology, and reconstruct the tree based on neutral substitutions.
To achieve this, we applied a method for outlier loci detecting as proposed by Excoffier et al. for the hierarchical
island model of populations (Excoffier et al., 2009). Specifically, MHC2_190v2, MHC2_251v2, GPH-414, serpin,
HGFA (p < 0.01) and GHII-2165, HpaI-99, U401-224, STC-410, ALDOB-135, GPDH (p < 0.05) were identified as
candidates for the directional selection, and U504-141 & LEI-87 (p < 0.01) – as candidate loci for the balancing
selection (Supplementary Figure S6). All the mentioned loci, as well as three mtSNPs, were subsequently excluded
from the analysis. However, it's noteworthy that the overall topology of the network remained largely unchanged,
but the stability of some nodes in the already identified clades has increased, and the uncertainty in some basal
nodes has increased significantly (Fig. 4B).
Uncovering Population Structure by Bayesian Clustering of Samples
Based on the analysis conducted in STRUCTURE 2.3.4 and the determination of the optimal number of
groups using STRUCTURE HARVESTER, the highest
Δ K value was associated with eight clusters, the second
highest peak corresponded to four clusters (Supplementary Figure S7). After the first round of clustering (K=2),
island populations became isolated (except for the population of Shumshu Island), further clustering led to the
consistent separation of the Okhota R. sample (K=3), Paramushir Island sample (K=4), Palana R. and Azabachye
Lake samples (K=5) from a more or less homogeneous group of populations of Kamchatka and Chukotka (Fig. 4C).
Further steps led to the separation of large clusters of South-West Kamchatka (including Shumshu Island) (SW) and
North-Eastern cluster (NE). The distribution of samples across eight clusters corresponds to the subdivision of
sockeye salmon in this region into nine distinct groups: SW, NE, and KR complexes, and individual populations of
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the Palana R., Okhota R., and three separate groupings of island populations of Bering Island, Paramushir Island and
the South Kuril Islands (SK). The sockeye salmon population from Azabachye Lake was notably distinct from the
other Kamchatka River samples, but did not exhibit differentiation when the MHC group loci were excluded from
the analysis.
Fig. 3. (A) PCA results showing population clustering based on the first two, and the first and the third
principle components (PCs), own data; ( B) The same, using our data and data from (Habicht et al., 2010). Sample
annotations are given in Supplementary Table S3. (C) Clustering of the samples based on DAPC, clusters identified
by the k-means method, the axes represent the first two linear discriminants; ( D) An admixture analysis with k = 7
using DAPC, the histogram showing the probabilities of assigning individuals to the clusters. To indicate the
regional affiliation of the samples, color bar is used, according to the color scheme in Fig. 1.
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Spatial clustering analysis in GENELAND successfully identified eight distinct groups among Asian
sockeye salmon populations, with a substantial overlap with the previously identified clusters in STRUCTURE (Fig.
5). The primary difference observed was the unification of two samples from watersheds within the Northern Kuril
Islands into a single cluster.
Fig. 4. (A) Phylogenetic network build using the Neighbor-Net method and chord distances for samples of
sockeye salmon from different watersheds of the Asian Pacific coast. Numbers in nodes are bootstrap indices (only
values ≥ 25 are given); ( B) The same for 27 putative neutral SNP loci; ( С ) An admixture analysis with
STRUCTURE. The bar plots show the proportion of the genome assigned to each of the inferred clusters where each
column represents an individual. Eight rounds of clustering were required to partition population structure down to
region location. Color bars and areas are according to the color scheme in Fig. 1.
Isolation by distance tests
To assess the load of gene flow in shaping territorial population complexes of sockeye salmon, we tested
the hypothesis of isolation by distance separately for the Western and Eastern coasts of Kamchatka using more
complete data from (Habicht et al., 2010).The Mantel test was employed to evaluate the correlation between
matrices of genetic and geographic distances, both along Kamchatka coasts and within specific regions. The analysis
revealed a significant correlation between geographic and genetic distances for both coasts of the peninsula,
considering 27 neutral SNP loci (for East Kamchatka − p = 0.0005***, for West Kamchatka − p = 0.0341*).
However, within the identified complexes, the tests were not significant (for populations of WK complex − p =
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0.7679, for NE − p = 0.3471, for KR − p = 0.0834). These findings indicate a high level of population connectivity
within complexes due to gene migration, with greater isolation observed between distant localities.
Fig. 5. The results of the spatial Bayesian analysis implemented in GENELAND for Asian sockeye
salmon: (A) A synthetic map of population membership in inferred clusters (spatial clusters marked by different
colors) with posterior density distribution of the number of clusters (in the inset); (В -F) Panels showing space of the
study area with the posterior probabilities belonging to some of inferred clusters for each pixel (dark red color
reflects a higher posterior probability of membership to a cluster). Black dots represent the geographical position of
sampled locations.
Discussion
Identifying Major Regional Complexes within Kamchatka peninsula
The analysis of sockeye salmon genetic differentiation within the studied range enables us to delineate
regional population complexes associated with the most important reproduction areas of this species. The primary
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sockeye salmon populations in the Asian region reproduce within Kamchatka, where three distinct regional groups
were identified: SW, NE, and KR complexes. Populations inhabiting watersheds along the North coast of the Sea of
Okhotsk, specifically the Palana River and Okhota River, as well as island populations (excluding Shumshu Island
population), were characterized by significant genetic differentiation from the so-called "core populations" of this
species inhabiting Kamchatka rivers.
The establishment of sockeye salmon regional complexes is primarily associated with adaptations to their
habitats in the same geographic area, the prevalence of life strategies adequate to local reproductive conditions, high
connectivity through migrations, and is fundamentally determined by their common descent. Simultaneously, the
main factors contributing to a specific range of adaptations within the complexes are related to the features of the
spawning and freshwater growing watersheds, such as the topography, prevailing climatic conditions, its
hydrobiological characteristics, aspects of anadromous migration and smoltification, as well as the coastal
geomorphology that sets conditions for the early sea phase of juvenile life. The distinctions observed between the
populations of West and East Kamchatka can be attributed to a complex set of adaptations specific to the climate
and the landscape on the respective western and eastern coastlines of the peninsula, as well as prevailing types of
spawning biotopes in the region. For instance, the length of the rivers on the west coast significantly exceeds that of
the rivers of North-East Kamchatka. The lower and middle sections of the channels of most West Kamchatka rivers
pass through low-lying swampy tundra and have a weak current (Pogodaev, 2013). In the majority of these
watersheds, there are no deep lakes essential for the reproduction of this species, except for the Ozernaya and Palana
rivers. Along the West Kamchatka, the coastline remains relatively flat, lacking significant bays or estuaries.
Consequently, juvenile salmon from these rivers typically enter the open sea directly or briefly utilize estuary lakes
or the estuarine zones of rivers for feeding. In contrast, the northeastern coast of Kamchatka indented by numerous
bays and inlets. Juvenile salmon from this region first migrate to partially enclosed coastal waters, bays, and inlets
before running to the open sea. This transitional phase may significantly influence their early marine survival
(Pogodaev, 2013). Rivers on the northeast coast tend to be shorter and faster flowing. Most of them have lakes
within their drainage basins (Supplementary Table S3). Within the populations inhabiting these regions, two distinct
ecological-temporal forms are prevalent: an early form, primarily spawning in lakes, and a late form, predominantly
reproducing in river bed. The distribution between these two forms within the populations is approximately equal
(Shubkin & Bugaev, 2023). On the West Coast, the number of the early form is relatively low; the majority of the
stocks are represented by the late, predominantly sea/river form. Given the higher migratory activity and lower
homing of the sea/river ecitype, it is likely that moderate gene flow occurs between adjacent river basins,
contributing to genetic uniformity within regional complexes (Beacham et al., 2006a). Consequently, the boundaries
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of such complexes can be determined by landscape zones and reproductive barriers. The gene migration restrictions
can be caused by both the spatial distance or geographical barriers (such as seas, straits, mountain ridges, etc.), and
ecological (specialization to the spawning ecotopes prevailing in a given area and subsequent isolation by
adaptation) or temporary (separation by time of approaches to reproductive watersheds, anadromous migration and
spawning sites) mechanisms of isolation.
The observed low level of population differentiation within the large Kamchatka complexes, SW and NE,
can most likely be attributed to their common ancestral origin and the relatively short time that has passed since
their divergence. It is commonly held that most populations of Asian sockeye salmon are relatively young, and their
age does not exceed 10-12 thousand years (Chereshnev, 1998; Brykov et al., 2005), because its modern range
largely coincides with the inferred area of the last Wisconsin glaciation in the North Pacific (maximum ~26.5−19
thousand years ago, deglaciation ~16,900−12,680 thousand years ago) (Braitseva & Evteeva, 1968; Velichko &
Faustova, 1989). During the last glacial maximum, a substantial portion of the Western Kamchatka Lowland and the
entire area of the Koryak Highlands were glaciated (Braitseva & Evteeva, 1968; Grosswald, 2009). This glaciation
would have acted as a barrier preventing anadromous fish from accessing these watersheds. Previously, based on the
Results
of an analysis of variability in the mtDNA control region, we determined that the entire Asian part of the
sockeye salmon range represents a zone of secondary contact resulted from the rapid expansion of this species
during the Holocene transgression, leading to the colonization of the majority of watersheds on the Kamchatka
Peninsula by two distinct genetic lineages of sockeye salmon with differing origins (i.e., fish from different refugia
that probably existed in the Beringia region (the territory of modern Alaska) and in the Kamchatka River basin)
(Khrustaleva et al., 2020). These findings were confirmed by the results of admixture analysis in DAPC and in
STRUCTURE, according to which all populations of these complexes had a “hybrid” origin, i.e. formed as a result
of genetic admixture of at least two ancestral populations. It is evident that the contribution of North American
populations to the gene pool of the northeastern complex is more substantial than that of the southwestern complex.
This is further supported by the frequency distribution of combined mtSNP haplotypes in sockeye salmon, with a
notable predominance of the GCC/CGG haplotype in the rivers of Northeastern Kamchatka and Chukotka
(Khrustaleva, 2016). The same haplotype was dominant in American sockeye salmon populations from Norton
Sound, Bristol Bay, Yukon and Kuskokwim rivers (Habicht et al., 2010).
Metapopulation of the Kamchatka River Basin
Several authors in numerous studies have frequently proposed the existence of a major refugium within the
Asian segment of its range, presumably located within the Kamchatka River paleobasin (Brykov et al., 2005;
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Beacham et al., 2006b; Khrustaleva et al., 2020). Presently, a large population of sockeye salmon is reproducing
here, second only to the Kuril Lake population. The results of admixture analysis revealed the distinctiveness of the
Azabachye Lake sample (formed a separate homogenous cluster), while sockeye salmon of the Kamchatka river
basin had a hybrid origin (Fig. 3D, 4C) and contained an admixture of genotypes identical to those identified in
Azabachye Lake. Genetic divergence of Azabachye and tributary sockeye salmon in the Kamchatka river basin has
been repeatedly demonstrated in studies examining the polymorphism of microsatellite loci and mtDNA sequences
(Brykov et al., 2005; Beacham et al., 2006b; Pilganchuk & Shpigalskaya, 2013; Pilganchuk et al., 2019; Khrustaleva
et al., 2020). Additionally, Brykov (Brykov et al., 2005) postulated that this divergence can be attributed to the
different origins of sockeye salmon in the upper and lower reaches of the river basin. Nevertheless, we posit that the
differentiation of Azabachye sockeye salmon is likely associated with relatively recent demographic events. In the
Azabachye Lake basin we examined the early sockeye salmon population, reproducing on the stream spawning
grounds of a small river Bushuyka flowing into the lake. In the relatively small isolated population genetic drift
usually occurs or it may have undergone fluctuations in its effective size in the recent past resulted in shifts in allelic
frequencies. Positive bottleneck tests have been obtained for almost all samples from the Kamchatka River
watershed including Azabachye sample (Table 1, Supplementary Table S3). In summary, we can deduce that the
genetic characteristics unique to the metapopulation of Kamchatka river basin were caused by prolonged isolation of
its part during the Upper Pleistocene glaciations within a large lake that existed in the middle reaches of the river
(Bugaev & Kirichenko, 2008), subsequent rapid expansion into local and neighboring watersheds during the
Holocene transgression, and, probably, secondary contact with adventive populations that colonized predominantly
the lower part of the river basin after the glacier retreat (Brykov et al., 2005; Khrustaleva et al., 2020).
Possible Factors Underlying the Divergence of North Sea of Okhotsk Populations
The high divergence observed in the Palana River population can result from the influence of directional
selection. The selection is likely driven by the Palana River geographical location (subperiphery of the range) and
the sockeye salmon biology peculiarities associated with its habitat conditions. The Palana River flows into the Sea
of Okhotsk in the northern part of the peninsula at approximately 59°N. This region is characterized by a severe
subarctic climate featuring long cold winters and short rainy summers. Palansky Lake, for example, remains ice-
covered until late June, with ice cover fully restored by the end of October (Bugaev et al., 2002). The northern
geographical location of the Palana River, far from the ocean growing areas, causes extensive migration of juvenile
sockeye salmon along the coast of Western Kamchatka to reach the Pacific Ocean for feeding. This migratory
pattern inevitably impacts their biological characteristics and population dynamics (Bugaev et al., 2002).
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Furthermore, a distinctive feature of this population is that the spawning and freshwater feeding of juvenile sockeye
salmon before migration to the sea are predominantly concentrated within the Palansky Lake. Here, in the vast
majority of cases, sockeye salmon spend approximately 2 years (Bugaev et al., 2002), so all Palana sockeye salmon
can be classified as a lake ecotype.
The Palana River estuary is hypertidal and characterized by significant spatiotemporal variability of all
abiotic factors (primarily the level, speed and direction of water flow, salinity, temperature, turbidity) primarily
driven by hyper-high tides, exceeding 10 meters. The tidal intrusion of salt water into the river's channel can extend
several kilometers upstream, leading to a strong reverse current. Juveniles migrating downstream have to expend
more energy, in turn, high turbidity of water in the estuarine zone and active mixing of the water mass complicates
the visual and olfactory orientation of migrants and the search for food. Consequently, the conditions for
smoltification of sockeye salmon in this population can be classified as extreme. The survival of juveniles during the
estuarine can only be supported by their high swimming activity, endurance, and readiness for the transition to
saltwater (completeness of pre-catadromous transformation, achievement of a certain body size, corresponding
physiological changes). In such a demanding environment, the mortality rate of underyearlings (0+) and yearlings
(1+) is notably high.
Identifying the specific genes and mechanisms involved in these adaptive processes remains a complex
challenge. The primary contribution to the third component that distinguishes this population from others is likely
the genetic variations found in the GPDH (glycerol-3-phosphate dehydrogenase) and RAG1 genes (Supplementary
Fig. S3). The GPDH2 SNP is localized in the CDS of the GPDH gene, encoding glycerol-3-phosphate
dehydrogenase [NAD(+)], an enzyme involved in the Krebs cycle and cellular energy metabolism. A high level of
its expression was detected in sockeye salmon smelt in British Columbia (Houde et al., 2019). The RAG3-93
substitution is situated in the 3' UTR of the recombination activating protein ( RAG1) gene and may potentially be
linked to adaptive loci within its coding region. The catalytic components of the RAG complex are involved in the
activation of V-D-J recombination of immunoglobulin, which is a unique recombination mechanism that occurs
only in developing lymphocytes at an early stage of B- and T-cell maturation and is responsible for the diversity of
antibodies/immunoglobulins and T-cell receptors. The third SNP whose contribution to PC3 was quite significant
was VIM-569. The Vim gene encodes vimentin, a protein found in intermediate filaments within connective tissues
and other mesoderm-derived tissues. During vertebrate embryonic development, vimentin is expressed in cells with
high migratory activity; postnatal expression of this gene is observed in fibroblasts, endothelial cells, lymphocytes
and some specialized cells of the thymus and brain (Battaglia et al., 2018). Its main function is to maintain cellular
and tissue integrity. Beyond this fundamental function, intermediate filaments play a crucial role in the intracellular
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distribution of organelles and proteins, subsequently influencing the functions of them (Minin & Moldaver, 2008).
Several studies have demonstrated that the functioning of mitochondria within cells is influenced, in part, by the
distribution of vimentin filaments (Herrmann & Aebi, 2000). Furthermore, two loci that stand out as potential
candidates for directional selection in the Palana population are ALDOB-135 and GPH-414 (p < 0.005). These loci
are located within the ALDOB and GPH genes, which encode Acyl-coenzyme A-binding protein and glycoprotein
hormone alpha-subunit, respectively. The former is involved in lipid metabolism and the intracellular transport of
acetyl-CoA, a central metabolite in the Krebbs cycle. The second is a common subunit of all pituitary hormones
involved in the regulation of growth processes, puberty, the formation of breeding color and the resistance of fish to
high temperatures.
Another perspective on the substantial divergence observed in the Palana River sample suggests that the
reduced genetic diversity and a shift in gene frequencies could be attributed to a relatively recent reduction in
effective population size, which was also confirmed by appropriate bottleneck tests. The sockeye salmon population
in the Palana River experienced cyclical fluctuations similar to those observed in pink salmon (Bugaev, 2011).
Bottleneck tests also support the hypothesis of effective population size decline in the nearest past. Thus, it becomes
evident that the sockeye salmon population of Palana River has the special status among other sockeye salmon
stocks of Western Kamchatka.
In the Okhota River, it appears that a somewhat different scenario is being realized. The neutrality tests did
not reveal selection effects at any of the SNP loci in this sample. The notable reduction in genetic diversity within
this sample suggests a recent decline in the effective population size rather than the influence of selection. The
probability of a bottleneck in the Okhota River sockeye salmon population is confirmed by corresponding tests.
Moreover, documented historical records support a decrease in the effective population size within this river basin.
Thus, in the 1930s, more than 100 thousand sockeye salmon spawners passed through the Ueginsky lake system to
spawn, and their total number in the river reached 1.5 million fish (Marchenko, 2022). In the 1960s − 1970s the
number of sockeye salmon approaches has sharply decreased
due to the significant impact of the Japanese drift-net
fishery and the deterioration of conditions during the embryonic-larval period due to climatic cooling in the Sea of
Okhotsk basin (Bugaev, 2011). For example, in the Ueginsky lakes in 1966, 1967 and 1968 about 20, 10 and 0.3
thousand spawners went to spawn, respectively, and in 1969–1971 – no more than 5–6 thousand fish (Nikulin,
1975). Furthermore, since 2016 total catch amounts increased, peaking at 479 tons in 2021 (Marchenko, 2022), but
it is still subject to rather sharp fluctuations associated with the conditions of its natural reproduction.
Island Populations: Distinctive Characteristics and Ecological Significance
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The most substantial degree of genetic divergence, as determined through various tests and clustering
methods, was observed between island and mainland populations. Likewise, significant distinctions were observed
among island populations when compared to each other. The exception, apparently, is the sockeye salmon
population of Shumshu Island, probably associated with the SW complex. Furthermore, within all the island
populations examined, there was a pronounced reduction in genetic diversity, except for the sample from the
Bettobu lake-river system (Shumshu Island). Notably, allelic diversity and expected heterozygosity were
consistently lower in island populations than in mainland populations at all loci and neutral SNPs analyzed.
The pronounced genetic differences and decrease in genetic diversity of island populations can be
explained by three primary categories of factors. The first category is associated with the geological history of this
region and the patterns of the ichthyofauna of the Kuril and Commander ridges formation during periods of global
climatic oscillations: long-term isolation in refugia and recurrent colonization of watersheds of the Kuril and
Commander islands, founder effects or, which is also likely, extinction events due to greater amplitude of changes in
environmental factors during global climate fluctuations on exposed land areas. Second, demographic factors such
as small population sizes, effective number fluctuations, and a high degree of isolation will be considered. The
distance of the islands from the center of the species' range acts as a reproductive barrier, limiting gene flow not
only between island and mainland populations but also between neighboring islands. Additionally, these populations
are likely to have undergone a bottleneck event in the relatively recent past. Third, the observed genetic differences
could reflect the development of local adaptations to specific environmental conditions within these island
populations.
The similarity of samples from watersheds of the South Kuril Islands allows us to classify them as a single
population complex. Evidently, this complex was formed under the influence of Pleistocene climatic cycles. The
first Illinois glaciation covered all the islands of the Great Kuril Ridge. In the north, it was semi-glaciated, while the
southern regions displayed characteristics of mountain-valley glaciation. The second glaciation, known as the
Wisconsin, left minimal imprints on the central islands and primarily contributed to small moraines located at
altitudes of 1000-1200 meters starting from Urup Island. Similar small moraines from the second glaciation were
identified on Iturup Island, although they were absent further to the south. Consequently, the second glaciation
extended over nearly all the islands, but in the north it was mountain-valley, and to the south it was close to cirque.
During the Late Pleistocene regressions, it is presumed that Sakhalin, Hokkaido, Kunashir, the Lesser Kuril Ridge
islands, and possibly Iturup were united as a single landmass, and had terrestrial connections with Primorye.
(Gorshkov, 1967). It can be hypothesized that within the ice-free reservoirs of this extensive drained region of the
continental shelf, populations were retained. These populations are likely descendants of the first wave of
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colonization who migrated from more northern territories and survived the most recent Wisconsin glaciation. The
presence of Japanese kokanee populations isolated in the lakes of Hokkaido, located south of the primary species
range, essentially serves as evidence of these glacial relic populations. During the Upper Pleistocene to early
Holocene warming phase, temporarily exposed lands were flooded, populations dispersed and became isolated.
Some of these populations subsequently formed relatively large stocks within suitable watersheds in the southern
group of islands in the Kuril archipelago. It is probable that during the last Holocene transgression, these areas of the
range were practically not subject to the expansion of colonists from more northern territories, as evidenced by
mtDNA analysis data (Khrustaleva, 2016; Khrustaleva et al., 2020).
The islands in the northern region of the Kuril archipelago, specifically Paramushir and Shumshu, were
physically connected to the Kamchatka Peninsula during the Late Pleistocene climatic cooling phases. However,
while the origin of the Shumshu island population is confidently linked to the populations of the South-West
Kamchatka complex, primarily due to its location along the migration routes of Ozernaya River sockeye salmon
through the First and Second Kuril Strait (the distance between the mouth of the Bettobu River and the mouth of the
Ozernaya River not exceeding 85 km), the population on Paramushir island likely has a more intricate history
including the combined impact in its contemporary genetic diversity of the founder effect and genetic drift under
long isolation. A similar scenario for the formation of genetic distinctiveness can be assumed for the Bering Island
population. In this case, it's likely that the primary factors influencing its genetic characteristics were the founder
event and genetic drift. This assertion is supported by the analysis of mtSNP and the CytB gene sequences
polymorphism, which revealed that the mass haplotype in Saranoye Lake was the same as in the Kamchatka River
basin (Mineeva et al., 2015; Khrustaleva, 2016). This discovery suggests that the colonization of the Commander
Islands occurred during the Holocene transgression from this nearby refugium. And it's apparent that these islands
were not heavily colonized by North American sockeye salmon for some reason. It is possible that the Kamchatka
River basin was a fairly large center of expansion of this species on the Asian coast of the Pacific Ocean at the time.
Alternatively, American alleles might have been subsequently eliminated due to genetic drift. In conclusion, the
observed shifts in allelic frequencies and the decrease in genetic diversity in the Bering Island population may be the
Result
of its descent from a limited number of individuals representing one or more ancestral gene pools. To
comprehensively evaluate these hypotheses, more extensive studies are needed, including a broader sample selection
from Asian, North American, and Japanese stocks, along with the analysis of different genetic markers, including
sequences from various mtDNA segments.
The analysis conducted revealed a substantial loss of neutral genetic diversity in island forms of sockeye
salmon compared to continental ones. Factors influencing within-population diversity can include bottlenecks,
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23
genetic drift, and inbreeding, all of which are dependent on the effective population size. Bottleneck tests across all
island populations did not reveal a significant reduction in observed heterozygosity relative to expected, assuming
equilibrium between mutations and drift. So, we can infer that effective population sizes have not experienced
significant recent declines.
Microevolutionary processes within relatively small and isolated island populations are characterized by an
increased influence of genetic drift, resulting in a reduction in genetic diversity. A marked decrease in allelic
diversity and heterozygosity was observed across all loci as well as 27 neutral loci in all island populations, with the
less pronounced effects seen in the sample from Shumshu Island and the greatest loss of diversity in Iturup Island
population (Supplementary Figure 6). Notably, despite positive inbreeding coefficients ( F
IS) in most island
populations, they were close to zero (as shown in Table 1). This suggests that mating conditions within these
populations resemble panmix, with a relatively low occurrence of consanguineous crossing. Since directional
selection also may lead to a reduction in genetic diversity, which may increase population viability and improve
adaptation to the unique environment of a particular island, outlier SNPs have been identified when comparing
island and mainland populations. Only two loci ( serpin and HGFA) can be considered candidates for directional
selection effects, which cannot explain the observed decrease in genetic diversity. Hence, it is likely that not
inbreeding or natural selection, but genetic drift, which occurs under conditions of long-term isolation, played a
predominant role in shaping the genetic characteristics of island populations and led to reduced genetic diversity and
significant shifts in allelic frequencies, consequently influencing estimations of their genetic differentiation.
In conclusion, it is crucial to emphasize the significance of preserving biodiversity in unique island
ecosystems. Many islands in the Kuril chain, including those we have examined, exhibit what is referred to as a
"disharmony of the theriofauna," characterized by a notable overabundance of predatory mammals in the species
spectrum (Kostenko, 2002). On Iturup Island, for instance, the predator-to-prey ratio (comprising species such as
fox, mink, sable, and bear as predators, and rat, red-gray vole, house mouse, and white hare as prey) stands at 1:1. In
this context, predators are compelled to rely on supplementary trophic sources such as anadromous salmonids,
which is an essential component of their diet on the islands. These findings underscore the necessity of preserving
the intricate ecological balances that are essential for the overall health and stability of these unique ecosystems.
Active commercial expansion and unregulated sockeye salmon fishery on the islands in conditions of limited
ecological space can lead to the elimination of a number of species from island therio-complexes and increase
instability of the species structure of the communities. The vulnerable balance of these island ecosystems is
threatened by unsustainable exploitation and other negative anthropogenic impacts. Drawing from the findings we
obtained in this and previous works, the southernmost populations of anadromous sockeye salmon in Asia (the
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was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
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24
populations inhabiting the lakes of the southern group islands of the Kuril ridge, along with the kokanee populations
of Hokkaido) can be classified as glacial relicts. These populations possess unique genetic characteristics, exhibit
distinct population dynamics, and are especially vulnerable to the impacts of global climate change and
anthropogenic threats. Given their exceptional status, it is essential to pay special attention to them. Therefore, when
developing a strategy for their sustainable commercial exploitation, it is important to establish systematic genetic
and environmental monitoring programs. If there are indicators of a decline in their current condition, it is crucial to
stop all fishing activities and initiate discussions regarding the implementation of protective measures of sockeye
salmon within this region.
Acknowledgments Author gratefully acknowledges to Dr. J.E. Seeb (College of the Environment, University of
Washington, Seattle, WA, USA) for his comprehensive assistance, provision of methods, and laboratory analysis
management, as well as to all the employees of the Environmental Genomics Laboratory, Department of
Hydrobiology and Fisheries, University of Washington, M.V. Shitova, Ph.D. (The Vavilov Institute of General
Genetics of the Russian Academy of Sciences, VIGG RAS), and P.C. Afanasyev, Ph.D. (Russian Federal Research
Institute of Fisheries and Oceanography, VNIRO), for their help in laboratory processing, N.V. Klovach, Dr.science
(VNIRO), for sample collection management, and the employees of VNIRO, Kamchatka branch (KamchatNIRO),
Pacific branch (TINRO), Sakhalin branch (SakhNIRO), and Magadan branch (MagadanNIRO) of the VNIRO, who
took part in the samples collection.
Supplementary Information The online version contains supplementary material available at …
Funding The research was supported by the Russian Science Foundation (project No. 23-24-00307).
Data Availability The datasets generated and analyzed during the current study are available from the author on
reasonable request.
Conflicts of Interest The author declares no conflict of interest.
Ethical approval This study was carried out in compliance with the Federal Law No. 498-FZ ‘On Responsible
Handling of Animals and on Amending Certain Legislative Acts of the Russian Federation’ (17 December 2018).
No ethical approval was required for fish provided dead by local fisheries.
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