Receding ice drove parallel expansions in Southern Ocean penguins

Theresa L. Cole, Ludovic Dutoit, Nicolas Dussex, Tom Hart, Alana Alexander, Jane L. Younger, Gemma V. Clucas, Marμa José Frugone, Yves Cherel, Richard Cuthbert, Ursula Ellenberg, Steven R. Fiddaman, Johanna Hiscock, David Houston, Pierre Jouventin, Thomas Mattern, Gary Miller, Colin Miskelly, Paul Nolan, Michael J. PolitoPetra Quillfeldt, Peter G. Ryan, Adrian Smith, Alan J.D. Tennyson, David Thompson, Barbara Wienecke, Juliana A. Vianna, Jonathan M. Waters

Research output: Contribution to journalArticlepeer-review

6 Citations (Scopus)
12 Downloads (Pure)

Abstract

Climate shifts are key drivers of ecosystem change. Despite the critical importance of Antarctica and the Southern Ocean for global climate, the extent of climate-driven ecological change in this region remains controversial. In particular, the biological effects of changing sea ice conditions are poorly understood.We hypothesize that rapid postglacial reductions in sea ice drove biological shifts across multiple widespread Southern Ocean species. We test for demographic shifts driven by climate events over recent millennia by analyzing population genomic datasets spanning 3 penguin genera (Eudyptes, Pygoscelis, and Aptenodytes). Demographic analyses for multiple species (macaroni/royal, eastern rockhopper, Adélie, gentoo, king, and emperor) currently inhabiting southern coastlines affected by heavy sea ice conditions during the Last Glacial Maximum (LGM) yielded genetic signatures of near-simultaneous population expansions associated with postglacial warming. Populations of the ice-adapted emperor penguin are inferred to have expanded slightly earlier than those of species requiring ice-free terrain. These concerted high-latitude expansion events contrast with relatively stable or declining demographic histories inferred for 4 penguin species (northern rockhopper, western rockhopper, Fiordland crested, and Snares crested) that apparently persisted throughout the LGM in ice-free habitats. Limited genetic structure detected in all ice-affected species across the vast Southern Ocean may reflect both rapid postglacial colonization of subantarctic and Antarctic shores, in addition to recent genetic exchange among populations. Together, these analyses highlight dramatic, ecosystem-wide responses to past Southern Ocean climate change and suggest potential for further shifts as warming continues.

Original languageEnglish
Pages (from-to)26690-26696
Number of pages7
JournalProceedings of the National Academy of Sciences of the United States of America
Volume116
Issue number52
Early online date16 Dec 2019
DOIs
Publication statusPublished - 26 Dec 2019

Keywords

  • Climate change
  • Genomics
  • Last Glacial Maximum
  • Refugia
  • Sphenisciformes

ASJC Scopus subject areas

  • General

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