Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Geology Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Geology; January 2007; v. 35; no. 1; p. 61-64; DOI: 10.1130/G23011A.1
© 2007 Geological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (12)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Emslie, S. D.
Right arrow Articles by Licht, K.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

A 45,000 yr record of Adélie penguins and climate change in the Ross Sea, Antarctica

Steven D. Emslie*,1, Larry Coats2 and Kathy Licht3

1 Department of Biology and Marine Biology, University of North Carolina, 601 S. College Road, Wilmington, North Carolina 28403, USA
2 Department of Geography, University of Utah, 260 S. Central Campus Drive, Room 270, Salt Lake City, Utah 84112, USA
3 Geology Department, Indiana University-Purdue University Indianapolis, 723 W. Michigan Street, Room SL118, Indianapolis, Indiana 46202, USA

Well-preserved remains of bone, tissue, and eggshell of Adélie Penguin (Pygoscelis adeliae) have been recovered from numerous abandoned colonies in the Ross Sea region, Antarctica. Radiocarbon dates on these remains provide an occupation history for this species ranging from hundreds to tens of thousands of years ago. We completed 62 new radiocarbon dates on these remains, which now indicate that an open-water marine environment existed in the Ross Sea from ca. 45,000 to 27,000 14C yr before present (B.P.) and provide constraints for the timing of the last advance of the Ross Ice Sheet. Penguins did not recolonize the Ross Sea until ca. 8000 calendar years (cal yr) B.P., after the early Holocene retreat of the Ross Ice Sheet. Two subsequent periods of abandonment at 5000–4000 and 2000–1100 cal yr B.P. correlate with cooling episodes that caused unfavorable marine conditions for breeding penguins. Most modern colonies were established only within the past 2000 yr.

Key Words: Adélie Penguin • abandoned colonies • occupation history • Ross Sea • ice sheet




This article has been cited by other articles:


Home page
The HoloceneHome page
T. E. Whittaker, B. L. Hall, C. H. Hendy, and S. A. Spaulding
Holocene depositional environments and surface-level changes at Lake Fryxell, Antarctica
The Holocene, August 1, 2008; 18(5): 775 - 786.
[Abstract] [PDF]


Home page
Proc. Natl. Acad. Sci. USAHome page
S. D. Emslie and W. P. Patterson
From the Cover: Abrupt recent shift in {delta}13C and {delta}15N values in Adelie penguin eggshell in Antarctica
PNAS, July 10, 2007; 104(28): 11666 - 11669.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Geological Society of America