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dc.contributor.authorDuffy, J. Emmett
dc.contributor.authorStachowicz, John J.
dc.contributor.authorReynolds, Pamela L.
dc.contributor.authorHovel, Kevin A.
dc.contributor.authorJahnke, Marlene
dc.contributor.authorSotka, Erik E.
dc.contributor.authorBoström, Christoffer
dc.contributor.authorBoyer, Katharyn E.
dc.contributor.authorCusson, Mathieu
dc.contributor.authorEklöf, Johan
dc.contributor.authorEngelen, Aschwin H.
dc.contributor.authorEriksson, Britas Klemens
dc.contributor.authorFodrie, F. Joel
dc.contributor.authorGriffin, John N
dc.contributor.authorHereu, Clara M.
dc.contributor.authorHori, Masakazu
dc.contributor.authorHughes, A. Randall
dc.contributor.authorIvanov, Mikhail V.
dc.contributor.authorJorgensen, Pablo
dc.contributor.authorKruschel, Claudia
dc.contributor.authorLee, Kun-Seop
dc.contributor.authorLefcheck, Jonathan S.
dc.contributor.authorMoksnes, Per-Olav
dc.contributor.authorNakaoka, Masahiro
dc.contributor.authorO’Connor, Mary I.
dc.contributor.authorO’Connor, Nessa E.
dc.contributor.authorOrth, Robert J.
dc.contributor.authorPeterson, Bradley J.
dc.contributor.authorReiss, Henning
dc.contributor.authorReiss, Katrin
dc.contributor.authorRichardson, J. Paul
dc.contributor.authorRossi, Francesca
dc.contributor.authorRuesink, Jennifer L.
dc.contributor.authorSchultz, Stewart T.
dc.contributor.authorThormar, Jonas
dc.contributor.authorTomas, Fiona
dc.contributor.authorUnsworth, Richard
dc.contributor.authorVoigt, Erin
dc.contributor.authorWhalen, Matthew A.
dc.contributor.authorZiegler, Shelby L.
dc.contributor.authorOlsen, Jeanine L.
dc.date.accessioned2022-12-01T10:20:17Z
dc.date.available2022-12-01T10:20:17Z
dc.date.created2022-08-31T12:50:30Z
dc.date.issued2022
dc.identifier.citationProceedings of the National Academy of Sciences of the United States of America. 2022, 119 (32), .en_US
dc.identifier.issn0027-8424
dc.identifier.urihttps://hdl.handle.net/11250/3035268
dc.description.abstractDistribution of Earth’s biomes is structured by the match between climate and plant traits, which in turn shape associated communities and ecosystem processes and services. However, that climate–trait match can be disrupted by historical events, with lasting ecosystem impacts. As Earth’s environment changes faster than at any time in human history, critical questions are whether and how organismal traits and ecosystems can adjust to altered conditions. We quantified the relative importance of current environmental forcing versus evolutionary history in shaping the growth form (stature and biomass) and associated community of eelgrass (Zostera marina), a widespread foundation plant of marine ecosystems along Northern Hemisphere coastlines, which experienced major shifts in distribution and genetic composition during the Pleistocene. We found that eelgrass stature and biomass retain a legacy of the Pleistocene colonization of the Atlantic from the ancestral Pacific range and of more recent within-basin bottlenecks and genetic differentiation. This evolutionary legacy in turn influences the biomass of associated algae and invertebrates that fuel coastal food webs, with effects comparable to or stronger than effects of current environmental forcing. Such historical lags in phenotypic acclimatization may constrain ecosystem adjustments to rapid anthropogenic climate change, thus altering predictions about the future functioning of ecosystems.en_US
dc.language.isoengen_US
dc.titleA Pleistocene legacy structures variation in modern seagrass ecosystemsen_US
dc.title.alternativeA Pleistocene legacy structures variation in modern seagrass ecosystemsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber8en_US
dc.source.volume119en_US
dc.source.journalProceedings of the National Academy of Sciences of the United States of Americaen_US
dc.source.issue32en_US
dc.identifier.doi10.1073/pnas.2121425119
dc.identifier.cristin2047566
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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