Serial population extinctions in a small mammal indicate Late Pleistocene ecosystem instability

The Late Pleistocene global extinction of many terrestrial mammal species has been a subject of intensive scientific study for over a century, yet the relative contributions of environmental changes and the global expansion of humans remain unresolved. A defining component of these extinctions is a...

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Published inProceedings of the National Academy of Sciences - PNAS Vol. 109; no. 50; pp. 20532 - 20536
Main Authors Brace, Selina, Palkopoulou, Eleftheria, Dalén, Love, Lister, Adrian M, Miller, Rebecca, Otte, Marcel, Germonpré, Mietje, Blockley, Simon P. E, Stewart, John R, Barnes, Ian
Format Journal Article Web Resource
LanguageEnglish
Published United States National Academy of Sciences 11.12.2012
National Acad Sciences
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Summary:The Late Pleistocene global extinction of many terrestrial mammal species has been a subject of intensive scientific study for over a century, yet the relative contributions of environmental changes and the global expansion of humans remain unresolved. A defining component of these extinctions is a bias toward large species, with the majority of small-mammal taxa apparently surviving into the present. Here, we investigate the population-level history of a key tundra-specialist small mammal, the collared lemming (Dicrostonyx torquatus), to explore whether events during the Late Pleistocene had a discernible effect beyond the large mammal fauna. Using ancient DNA techniques to sample across three sites in North-West Europe, we observe a dramatic reduction in genetic diversity in this species over the last 50,000 y. We further identify a series of extinction-recolonization events, indicating a previously unrecognized instability in Late Pleistocene small-mammal populations, which we link with climatic fluctuations. Our results reveal climate-associated, repeated regional extinctions in a keystone prey species across the Late Pleistocene, a pattern likely to have had an impact on the wider steppe-tundra community, and one that is concordant with environmental change as a major force in structuring Late Pleistocene biodiversity.
Bibliography:http://dx.doi.org/10.1073/pnas.1213322109
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EU FP6 ERA-NET project CLIMIGRATE
info:eu-repo/grantAgreement/EC/FP7/226506
scopus-id:2-s2.0-84884714291
Edited by Donald K. Grayson, University of Washington, Seattle, WA, and approved October 9, 2012 (received for review August 3, 2012)
2J.R.S. and I.B. contributed equally to this work.
1S.B. and E.P. contributed equally to this work.
Author contributions: S.B., L.D., J.R.S., and I.B. designed research; S.B., E.P., and I.B. performed research; S.B., L.D., A.M.L., R.M., M.O., M.G., S.P.E.B., J.R.S., and I.B. contributed new reagents/analytic tools; S.B., E.P., S.P.E.B., and I.B. analyzed data; and S.B., E.P., L.D., A.M.L., S.P.E.B., J.R.S., and I.B. wrote the paper.
ISSN:0027-8424
1091-6490
1091-6490
DOI:10.1073/pnas.1213322109