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ABSTRACT Many coastal marine species experienced Pleistocene gene flow between the North Pacific and Atlantic. Understanding historical connectivity between ocean basins should aid in predicting how regional faunas will respond to recent warming that has intensified trans‐Arctic dispersal. Wetland fauna of the Northwestern Atlantic may have survived in estuarine refugia throughout glacial cycles, or recolonised from the southern coast, North Pacific or Northeastern Atlantic. Here, we used multilocus genetic markers and historical climate data to investigate lineage distribution and connectivity among populations of the nominally cosmopolitan sea slugAlderia modesta, sampled from mudflats on both coasts of the North Pacific and North Atlantic. Mitochondrial DNA clades from European and North American populations were deeply divergent and reciprocally monophyletic; differences at seven polymorphic nuclear loci indicated prolonged absence of trans‐Atlantic gene flow. A Pacific ancestor likely first colonised the Atlantic during the marine biotic interchange of the middle Pliocene ~3.5 Ma. Both mtDNA phylogenetics and nuclear genotype assignments support repeated trans‐Arctic colonisation of the Northwestern Atlantic from the Pacific during inter‐glacial cycles; no gene flow was evident since the last glacial maximum, however. Time‐calibrated coalescent phylogenies, Bayesian skyline plots and haplotype networks all indicated recent population expansions in the Pacific and Europe, but not Northwestern Atlantic. In both the Pacific and Northwestern Atlantic, older lineages persisted in patchy refugia north of glacial margins, while a derived clade of Pacific haplotypes indicates northward post‐LGM expansion. The biogeographical history ofAlderiacontrasts with rocky‐shore taxa that were largely extirpated by glacial advance and recolonised from refugia following the last glacial maximum. Based on molecular differences and distinctions in radular and penial stylet morphology, we resurrect the nameAlderia harvardiensisGould 1870 forAlderiafrom the Northwestern Atlantic and North Pacific;A. modestarefers exclusively to European slugs.
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Ocean current patterns drive the worldwide colonization of eelgrass (Zostera marina)
Abstract Currents are unique drivers of oceanic phylogeography and thus determine the distribution of marine coastal species, along with past glaciations and sea-level changes. Here we reconstruct the worldwide colonization history of eelgrass (Zostera marinaL.), the most widely distributed marine flowering plant or seagrass from its origin in the Northwest Pacific, based on nuclear and chloroplast genomes. We identified two divergent Pacific clades with evidence for admixture along the East Pacific coast. Two west-to-east (trans-Pacific) colonization events support the key role of the North Pacific Current. Time-calibrated nuclear and chloroplast phylogenies yielded concordant estimates of the arrival ofZ. marinain the Atlantic through the Canadian Arctic, suggesting that eelgrass-based ecosystems, hotspots of biodiversity and carbon sequestration, have only been present there for ~243 ky (thousand years). Mediterranean populations were founded ~44 kya, while extant distributions along western and eastern Atlantic shores were founded at the end of the Last Glacial Maximum (~19 kya), with at least one major refuge being the North Carolina region. The recent colonization and five- to sevenfold lower genomic diversity of the Atlantic compared to the Pacific populations raises concern and opportunity about how Atlantic eelgrass might respond to rapidly warming coastal oceans.
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- Award ID(s):
- 1829976
- PAR ID:
- 10482442
- Author(s) / Creator(s):
- ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; more »
- Publisher / Repository:
- Springer Nature
- Date Published:
- Journal Name:
- Nature Plants
- Volume:
- 9
- Issue:
- 8
- ISSN:
- 2055-0278
- Page Range / eLocation ID:
- 1207-1220
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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- Free Publicly Accessible Full Text
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Accepted Manuscript
- Journal Article:
- https://doi.org/10.1038/s41477-023-01464-3
