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Reduced ice extent on the western Antarctic Peninsula at 700-970 cal. yr B.P
Rapid warming and consequent ice-shelf collapse have focused attention on the glacial record of the Antarctic Peninsula. Here, we present the first record of terrestrial organic material exposed by recently retreating ice that bears on past glacier extent and climate in this sensitive region. Radioc...
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Published in: | Geology (Boulder) 2010-07, Vol.38 (7), p.635-638 |
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creator | Hall, B. L Koffman, T Denton, G. H |
description | Rapid warming and consequent ice-shelf collapse have focused attention on the glacial record of the Antarctic Peninsula. Here, we present the first record of terrestrial organic material exposed by recently retreating ice that bears on past glacier extent and climate in this sensitive region. Radiocarbon dates show that ice on Anvers Island was at or behind its present position at 700-970 cal. yr B.P., coincident with ice reduction elsewhere in the Southern Hemisphere. Moreover, the data indicate that present reduced ice extent on the western Antarctic Peninsula is not unprecedented and is similar to that experienced during at least three periods in the last 5600 yr. |
doi_str_mv | 10.1130/G30932.1 |
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Moreover, the data indicate that present reduced ice extent on the western Antarctic Peninsula is not unprecedented and is similar to that experienced during at least three periods in the last 5600 yr.</description><subject>absolute age</subject><subject>Antarctic Peninsula</subject><subject>Antarctica</subject><subject>Anvers Island</subject><subject>Bryophyta</subject><subject>C-14</subject><subject>carbon</subject><subject>Cenozoic</subject><subject>Climate</subject><subject>dates</subject><subject>deglaciation</subject><subject>glacial extent</subject><subject>glacial geology</subject><subject>Global warming</subject><subject>Holocene</subject><subject>Ice</subject><subject>ice shelves</subject><subject>isotopes</subject><subject>Musci</subject><subject>Plantae</subject><subject>Quaternary</subject><subject>Quaternary geology</subject><subject>radioactive isotopes</subject><subject>shells</subject><subject>upper Holocene</subject><issn>0091-7613</issn><issn>1943-2682</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNqN0E1r3DAQBmBRUuhmW-hPEL00ELyd0ciWdUyWZBNYaCjt2SjSOPHilVPJJs2_j8MWAjnlNJdn3vkQ4ivCCpHgx4bAklrhB7FAq6lQVa2OxALAYmEqpE_iOOcdAOrS1Aux_cVh8hxk51nyv5HjKIcox3uWj5xHTlGexdElP3Ze3nDsYp56J90oDUBhDUjv-pV8SvJ8dfNZfGxdn_nL_7oUfy4vfq-viu3PzfX6bFs4rWksSk8qtBUHdNi2LrCtawO3pq2NJqiUt6XSrEuv6tuyZUtANgSrDEKLEAwtxfdD7kMa_k7zms2-y5773kUeptyYUpdEBqv3SZzxLL-9kbthSnE-oymNqYAUvQw-OSCfhpwTt81D6vYuPTUIzcv7m8P7G5zp6YHe8ZB9x9Hz45D68BqrYG6CSitCegbKK4F3</recordid><startdate>20100701</startdate><enddate>20100701</enddate><creator>Hall, B. 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ispartof | Geology (Boulder), 2010-07, Vol.38 (7), p.635-638 |
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language | eng |
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source | AUTh Library subscriptions: Society of Exploration Geophysicists |
subjects | absolute age Antarctic Peninsula Antarctica Anvers Island Bryophyta C-14 carbon Cenozoic Climate dates deglaciation glacial extent glacial geology Global warming Holocene Ice ice shelves isotopes Musci Plantae Quaternary Quaternary geology radioactive isotopes shells upper Holocene |
title | Reduced ice extent on the western Antarctic Peninsula at 700-970 cal. yr B.P |
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