Holocene occupation history of pygoscelid penguins at Stranger Point, King George 25 de Mayo Island, northern Antarctic Peninsula/ (Record no. 15018)

MARC details
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fixed length control field 02221nab a2200217 4500
005 - DATE & TIME
control field 20231025102623.0
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100 ## - MAIN ENTRY--PERSONAL NAME
Personal name Emslie, Steven D
245 ## - TITLE STATEMENT
Title Holocene occupation history of pygoscelid penguins at Stranger Point, King George 25 de Mayo Island, northern Antarctic Peninsula/
260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Name of publisher, distributor, etc Sage,
Date of publication, distribution, etc 2020.
300 ## - PHYSICAL DESCRIPTION
Pages Vol. 30, issue 1, 2020 ( 190–196 p.).
520 ## - SUMMARY, ETC.
Summary, etc We report additional fossil evidence for pygoscelid penguins breeding on King George (25 de Mayo) Island, South Shetland Islands, in the Holocene beginning at ~7000 cal. yr BP. This evidence comes from a raised marine beach deposit formerly studied and described as Pingfo I at Stranger Point, Potter Peninsula. We relocated and exposed deposits at this site and recovered additional samples of penguin bones from five stratigraphic beds that are redescribed here. Most of these bones are from juvenile penguins and exhibit little or no wear indicating minimal transport to the beach deposits. Some of the bones are developed enough to be identifiable to Adélie (Pygoscelis adeliae), Gentoo (Pygoscelis papua), and Chinstrap (Pygoscelis antarctica) penguins, indicating that all three species were breeding at Stranger Point from ~7320 to 4865 cal. yr BP. This breeding occupation corresponds with the first warming and deglaciation that occurred in the northern Antarctic Peninsula by this time and ends with the onset of reglaciation of the Peninsula. At least 31 abandoned penguin mounds and ornithogenic soils also were located and sampled at Stranger Point and indicate that the current occupation of this area by all three pygoscelid penguins dates no older than ~535 cal. yr BP. The absence of ornithogenic soils from earlier Holocene breeding was probably due to glacial activity and soil solifluction during periods of warming in the mid to late Holocene.
700 ## - Added Entry Personal Name
Added Entry Personal Name Romero, Matias
700 ## - Added Entry Personal Name
Added Entry Personal Name Juares, Mariana A
700 ## - Added Entry Personal Name
Added Entry Personal Name Argota, Martin R
773 0# - HOST ITEM ENTRY
Host Biblionumber 12756
Host Itemnumber 17200
Place, publisher, and date of publication London: Sage Publication Ltd, 2019.
Title Holocene/
International Standard Serial Number 09596836
856 ## - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier https://doi.org/10.1177/0959683619875814
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Koha item type E-Journal
100 ## - MAIN ENTRY--PERSONAL NAME
-- 58779
700 ## - Added Entry Personal Name
-- 58780
700 ## - Added Entry Personal Name
-- 58781
700 ## - Added Entry Personal Name
-- 58782
942 ## - ADDED ENTRY ELEMENTS (KOHA)
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