4.7 Article

Ancient Adelie penguin colony revealed by snowmelt at Cape Irizar, Ross Sea, Antarctica

Journal

GEOLOGY
Volume 49, Issue 2, Pages 145-149

Publisher

GEOLOGICAL SOC AMER, INC
DOI: 10.1130/G48230.1

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Funding

  1. U.S. National Science Foundation [ANT-1443386]

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Research in Ross Sea revealed that fresh penguin remains exposed by melting snow are actually ancient, suggesting recent snowmelt has revealed previously frozen carcasses. This indicates enhanced marine productivity during a warm period from 4000-2000 years ago in the penguin optimum phase.
The Ross Sea (Antarctica) is one of the most productive marine ecosystems in the Southern Ocean and supports nearly one million breeding pairs of Adelie penguins (Pygoscelis adeliae) annually. There also is a well-preserved record of abandoned penguin colonies that date from before the Last Glacial Maximum (>45,000 C-14 yr B.P.) through the Holocene. Cape Irizar is a rocky cape located just south of the Drygalski Ice Tongue on the Scott Coast. In January 2016, several abandoned Adelie penguin sites and abundant surface remains of penguin bones, feathers, and carcasses that appeared to be fresh were being exposed by melting snow and were sampled for radiocarbon analysis. The results indicate the fresh remains are actually ancient and that three periods of occupation by Adelie penguins are represented beginning ca. 5000 calibrated calendar (cal.) yr B.P., with the last occupation ending by ca. 800 cal. yr B.P. The presence of fresh-appearing remains on the surface that are actually ancient in age suggests that only recently has snowmelt exposed previously frozen carcasses and other remains for the first time in similar to 800 yr, allowing them to decay and appear fresh. Recent warming trends and historical satellite imagery (Landsat) showing decreasing snow cover on the cape since 2013 support this hypothesis. Increased delta C-13 values of penguin bone collagen further indicate a period of enhanced marine productivity during the penguin optimum, a warm period at 4000-2000 cal. yr B.P., perhaps related to an expansion of the Terra Nova Bay polynya with calving events of the Drygalski Ice Tongue.

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