Thriving or surviving? The isotopic record of the Wrangel Island woolly mammoth population

QUATERNARY SCIENCE REVIEWS

卷:222

Article

Arppe, Laura¹  Karhu, Juha A.²  Vartanyan, Sergey³  Drucker, Dorothee G.⁴  Etu-Sihvola, Heli¹  Bocherens, Herve^4,5 

[1] Univ Helsinki, Finnish Museum Nat Hist LUOMUS, POB 64, FIN-00014 Helsinki, Finland

[2] Univ Helsinki, Dept Geosci & Geog, POB 64, FIN-00014 Helsinki, Finland

[3] RAS, FEB, NEISRI, 16 Portovaya Str, Magadan 685000, Russia

[4] Senckenberg Ctr Human Evolut & Palaeoenvironm S H, Sigwartstr 10, D-72076 Tubingen, Germany

[5] Univ Tubingen, Dept Geosci, Biogeol, Holderlinstr 12, D-72074 Tubingen, Germany

关键词: Holocene;    Pleistocene;    Paleoclimatology;    Paleoecology;    Russia;    Beringia;    Stable isotopes;    Radiogenic isotopes;    Mammoths;    Extinction;   

DOI  :  10.1016/j.quascirev.2019.105884

来源: Elsevier

【 摘 要 】

The world's last population of woolly mammoths (Mammuthus primigenius) lived on Wrangel Island persisting well into the Holocene, going extinct at ca. 4000 cal BP. According to the frequency of 'radiocarbon dated mammoth remains from the island, the extinction appears fairly abrupt. This study investigates the ecology of the Wrangel Island mammoth population by means of carbon, nitrogen and sulfur isotope analyses. We report new isotope data on 77 radiocarbon dated mammoth specimens from Wrangel Island and Siberia, and evaluate them in relation to previously published isotope data for Pleistocene mammoths from Beringia and lower latitude Eurasia, and the other insular Holocene mammoth population from St. Paul Island. Contrary to prior suggestions of gradual habitat deterioration, the nitrogen isotope values of the Wrangel Island mammoths do not support a decline in forage quality/quantity, and are in fact very similar to their north Beringian forebears right to the end. However, compared to Siberian mammoths, those from Wrangel Island show a difference in their energy economy as judged by the carbon isotope values of structural carbonate, possibly representing a lower need of adaptive strategies for survival in extreme cold. Increased mid-Holocene weathering of rock formations in the central mountains is suggested by sulfur isotope values. Scenarios related to water quality problems stemming from increased weathering, and a possibility of a catastrophic starvation event as a cause of, or contributing factor in their demise are discussed. (C) 2019 The Authors. Published by Elsevier Ltd.

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