Late Pleistocene stickleback environmental genomes reveal the chronology of freshwater adaptation
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Late Pleistocene stickleback environmental genomes reveal the chronology of freshwater adaptation. / Laine, Jan; Mak, Sarah S. T.; Martins, Nuno F. G.; Chen, Xihan; Gilbert, M. Thomas P.; Jones, Felicity C.; Pedersen, Mikkel Winther; Romundset, Anders; Foote, Andrew D.
I: Current Biology, Bind 34, Nr. 5, 2024, s. 1142-1147.e6.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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TY - JOUR
T1 - Late Pleistocene stickleback environmental genomes reveal the chronology of freshwater adaptation
AU - Laine, Jan
AU - Mak, Sarah S. T.
AU - Martins, Nuno F. G.
AU - Chen, Xihan
AU - Gilbert, M. Thomas P.
AU - Jones, Felicity C.
AU - Pedersen, Mikkel Winther
AU - Romundset, Anders
AU - Foote, Andrew D.
N1 - Funding Information: We thank three anonymous reviewers whose feedback greatly improved this manuscript. This work was funded by a European Research Council (ERC) consolidator grant ( ERC-COG-101045346 “EXPLOAD”) and a Norwegian Research Council (NFR) ERC application support grant ( 324353 ) awarded to A.D.F. Publisher Copyright: © 2024 The Author(s)
PY - 2024
Y1 - 2024
N2 - Directly observing the chronology and tempo of adaptation in response to ecological change is rarely possible in natural ecosystems. Sedimentary ancient DNA (sedaDNA) has been shown to be a tractable source of genome-scale data of long-dead organisms1,2,3 and to thereby potentially provide an understanding of the evolutionary histories of past populations.4,5 To date, time series of ecosystem biodiversity have been reconstructed from sedaDNA, typically using DNA metabarcoding or shotgun sequence data generated from less than 1 g of sediment.6,7 Here, we maximize sequence coverage by extracting DNA from ∼50× more sediment per sample than the majority of previous studies1,2,3 to achieve genotype resolution. From a time series of Late Pleistocene sediments spanning from a marine to freshwater ecosystem, we compare adaptive genotypes reconstructed from the environmental genomes of three-spined stickleback at key time points of this transition. We find a staggered temporal dynamic in which freshwater alleles at known loci of large effect in marine-freshwater divergence of three-spined stickleback (e.g., EDA)8 were already established during the brackish phase of the formation of the isolation basin. However, marine alleles were still detected across the majority of marine-freshwater divergence-associated loci, even after the complete isolation of the lake from marine ingression. Our retrospective approach to studying adaptation from environmental genomes of three-spined sticklebacks at the end of the last glacial period complements contemporary experimental approaches9,10,11 and highlights the untapped potential for retrospective “evolve and resequence” natural experiments using sedaDNA.
AB - Directly observing the chronology and tempo of adaptation in response to ecological change is rarely possible in natural ecosystems. Sedimentary ancient DNA (sedaDNA) has been shown to be a tractable source of genome-scale data of long-dead organisms1,2,3 and to thereby potentially provide an understanding of the evolutionary histories of past populations.4,5 To date, time series of ecosystem biodiversity have been reconstructed from sedaDNA, typically using DNA metabarcoding or shotgun sequence data generated from less than 1 g of sediment.6,7 Here, we maximize sequence coverage by extracting DNA from ∼50× more sediment per sample than the majority of previous studies1,2,3 to achieve genotype resolution. From a time series of Late Pleistocene sediments spanning from a marine to freshwater ecosystem, we compare adaptive genotypes reconstructed from the environmental genomes of three-spined stickleback at key time points of this transition. We find a staggered temporal dynamic in which freshwater alleles at known loci of large effect in marine-freshwater divergence of three-spined stickleback (e.g., EDA)8 were already established during the brackish phase of the formation of the isolation basin. However, marine alleles were still detected across the majority of marine-freshwater divergence-associated loci, even after the complete isolation of the lake from marine ingression. Our retrospective approach to studying adaptation from environmental genomes of three-spined sticklebacks at the end of the last glacial period complements contemporary experimental approaches9,10,11 and highlights the untapped potential for retrospective “evolve and resequence” natural experiments using sedaDNA.
KW - adaptation
KW - ancient DNA
KW - environmental genomes
KW - evolve and resequence
KW - Gasterosteus aculeatus
KW - sediment core
KW - three-spined sticklebacks
KW - time series
U2 - 10.1016/j.cub.2024.01.056
DO - 10.1016/j.cub.2024.01.056
M3 - Journal article
C2 - 38350445
AN - SCOPUS:85186991757
VL - 34
SP - 1142-1147.e6
JO - Current Biology
JF - Current Biology
SN - 0960-9822
IS - 5
ER -
ID: 391313362