The Holocene environmental history of Lake Hoare, Taylor Valley, Antarctica, reconstructed from sediment cores

Abstract Up to 2.3 m long sediment sequences were recovered from the deepest part of Lake Hoare in Taylor Valley, southern Victoria Land, Antarctica. Sedimentological, biogeochemical, and mineralogical analyses revealed a high spatial variability of these parameters in Lake Hoare. Five distinct lith...

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Published in:Antarctic Science
Main Authors: Wagner, Bernd, Ortlepp, Sabrina, Doran, Peter T., Kenig, Fabien, Melles, Martin, Burkemper, Andy
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2011
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102011000125
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102011000125
id crcambridgeupr:10.1017/s0954102011000125
record_format openpolar
spelling crcambridgeupr:10.1017/s0954102011000125 2024-03-03T08:38:41+00:00 The Holocene environmental history of Lake Hoare, Taylor Valley, Antarctica, reconstructed from sediment cores Wagner, Bernd Ortlepp, Sabrina Doran, Peter T. Kenig, Fabien Melles, Martin Burkemper, Andy 2011 http://dx.doi.org/10.1017/s0954102011000125 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102011000125 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 23, issue 3, page 307-319 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2011 crcambridgeupr https://doi.org/10.1017/s0954102011000125 2024-02-08T08:35:50Z Abstract Up to 2.3 m long sediment sequences were recovered from the deepest part of Lake Hoare in Taylor Valley, southern Victoria Land, Antarctica. Sedimentological, biogeochemical, and mineralogical analyses revealed a high spatial variability of these parameters in Lake Hoare. Five distinct lithological units were recognized. Radiocarbon dating of bulk organic carbon samples from the sediment sequences yielded apparently too old ages and significant age reversals, which prevented the establishment of reliable age-depth models. However, cross correlation of the sedimentary characteristics with those of sediment records from neighbouring Lake Fryxell indicates that the lowermost two units of the Lake Hoare sediment sequences were probably deposited during the final phase of proglacial Lake Washburn, which occupied Taylor Valley during the late Pleistocene and early Holocene. High amounts of angular gravel and the absence of fine-grained material imply a complete desiccation with subaerial conditions in the Lake Hoare basin in the middle of the Holocene. The late Holocene (< c. 3300 calendar yr bp ) is characterized by the establishment of environmental conditions similar to those existing today. A late Holocene desiccation event, such as proposed in former studies, is not indicated in the sediment sequences recovered. Article in Journal/Newspaper Antarc* Antarctic Science Antarctica Victoria Land Cambridge University Press Victoria Land Taylor Valley ENVELOPE(163.000,163.000,-77.617,-77.617) Fryxell ENVELOPE(163.183,163.183,-77.617,-77.617) Hoare ENVELOPE(162.850,162.850,-77.633,-77.633) Lake Fryxell ENVELOPE(163.183,163.183,-77.617,-77.617) Washburn ENVELOPE(-86.133,-86.133,-77.617,-77.617) Lake Hoare ENVELOPE(162.850,162.850,-77.633,-77.633) Antarctic Science 23 3 307 319
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
spellingShingle Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Wagner, Bernd
Ortlepp, Sabrina
Doran, Peter T.
Kenig, Fabien
Melles, Martin
Burkemper, Andy
The Holocene environmental history of Lake Hoare, Taylor Valley, Antarctica, reconstructed from sediment cores
topic_facet Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
description Abstract Up to 2.3 m long sediment sequences were recovered from the deepest part of Lake Hoare in Taylor Valley, southern Victoria Land, Antarctica. Sedimentological, biogeochemical, and mineralogical analyses revealed a high spatial variability of these parameters in Lake Hoare. Five distinct lithological units were recognized. Radiocarbon dating of bulk organic carbon samples from the sediment sequences yielded apparently too old ages and significant age reversals, which prevented the establishment of reliable age-depth models. However, cross correlation of the sedimentary characteristics with those of sediment records from neighbouring Lake Fryxell indicates that the lowermost two units of the Lake Hoare sediment sequences were probably deposited during the final phase of proglacial Lake Washburn, which occupied Taylor Valley during the late Pleistocene and early Holocene. High amounts of angular gravel and the absence of fine-grained material imply a complete desiccation with subaerial conditions in the Lake Hoare basin in the middle of the Holocene. The late Holocene (< c. 3300 calendar yr bp ) is characterized by the establishment of environmental conditions similar to those existing today. A late Holocene desiccation event, such as proposed in former studies, is not indicated in the sediment sequences recovered.
format Article in Journal/Newspaper
author Wagner, Bernd
Ortlepp, Sabrina
Doran, Peter T.
Kenig, Fabien
Melles, Martin
Burkemper, Andy
author_facet Wagner, Bernd
Ortlepp, Sabrina
Doran, Peter T.
Kenig, Fabien
Melles, Martin
Burkemper, Andy
author_sort Wagner, Bernd
title The Holocene environmental history of Lake Hoare, Taylor Valley, Antarctica, reconstructed from sediment cores
title_short The Holocene environmental history of Lake Hoare, Taylor Valley, Antarctica, reconstructed from sediment cores
title_full The Holocene environmental history of Lake Hoare, Taylor Valley, Antarctica, reconstructed from sediment cores
title_fullStr The Holocene environmental history of Lake Hoare, Taylor Valley, Antarctica, reconstructed from sediment cores
title_full_unstemmed The Holocene environmental history of Lake Hoare, Taylor Valley, Antarctica, reconstructed from sediment cores
title_sort holocene environmental history of lake hoare, taylor valley, antarctica, reconstructed from sediment cores
publisher Cambridge University Press (CUP)
publishDate 2011
url http://dx.doi.org/10.1017/s0954102011000125
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102011000125
long_lat ENVELOPE(163.000,163.000,-77.617,-77.617)
ENVELOPE(163.183,163.183,-77.617,-77.617)
ENVELOPE(162.850,162.850,-77.633,-77.633)
ENVELOPE(163.183,163.183,-77.617,-77.617)
ENVELOPE(-86.133,-86.133,-77.617,-77.617)
ENVELOPE(162.850,162.850,-77.633,-77.633)
geographic Victoria Land
Taylor Valley
Fryxell
Hoare
Lake Fryxell
Washburn
Lake Hoare
geographic_facet Victoria Land
Taylor Valley
Fryxell
Hoare
Lake Fryxell
Washburn
Lake Hoare
genre Antarc*
Antarctic Science
Antarctica
Victoria Land
genre_facet Antarc*
Antarctic Science
Antarctica
Victoria Land
op_source Antarctic Science
volume 23, issue 3, page 307-319
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102011000125
container_title Antarctic Science
container_volume 23
container_issue 3
container_start_page 307
op_container_end_page 319
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