Holocene Diatoms Recovered from Shaldril I Cores, Maxwell Bay, Antarctica

High-resolution Holocene sediment cores from the continental shelf of Antarctica are integral to the study of recent climate transitions, but such records are rare. The inaugural SHALDRIL I cruise to Maxwell Bay along the Northern Antarctica Peninsula, however, recovered the most expanded record to...

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Other Authors: Geary, Lindsey Eileen (authoraut)
Format: Others
Language:English
English
Published: Florida State University
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Online Access:http://purl.flvc.org/fsu/fd/FSU_migr_etd-0129
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spelling ndltd-fsu.edu-oai-fsu.digital.flvc.org-fsu_1682092019-07-01T04:22:53Z Holocene Diatoms Recovered from Shaldril I Cores, Maxwell Bay, Antarctica Geary, Lindsey Eileen (authoraut) Wise, Sherwood W. (professor directing thesis) Georgen, Jennifer (committee member) Donoghue, Joseph F. (committee member) Department of Earth, Ocean and Atmospheric Sciences (degree granting department) Florida State University (degree granting institution) Text text Florida State University English eng 1 online resource computer application/pdf High-resolution Holocene sediment cores from the continental shelf of Antarctica are integral to the study of recent climate transitions, but such records are rare. The inaugural SHALDRIL I cruise to Maxwell Bay along the Northern Antarctica Peninsula, however, recovered the most expanded record to date at Site NBP05-02-1B. More than twice as long as any other such Antarctic sequence, the 108.2 m section dates back 13,480 yr B.P. Presented here is a record of climate variation interpreted from analyses of the diatom content. Diatoms have proven to be a useful tool in the study of paleoclimate. Analyses completed here include species diversity, total diatom abundance (valves per gram of sediment), Eucampia antarctica var. antarctica to E. antarctica var. recta ratio, Eucampia index, Chaetoceros resting-spore percent, Chaetoceros hyalochaete to C. vegetative ratio, and Thalassiosira antarctica T2 percentage. The analyses show a continuous sea-ice assemblage with minor fluctuations in response to changing sea-ice conditions. Other than the Thalassiosira antarctica T2 percentage, all analyses show a prominent warming period identified as the Mid-Holocene Climatic Optimum. Thalassiosira antarctica T2 percentage marks a period of deglaciation at approximately 11 ka. This episode of deglaciation has been documented in other studies and is believed to mark the onset of present-day ice conditions. A Thesis submitted to the Department of Geology in partial fulfillment of the requirements for the degree of Master of Science. Degree Awarded: Spring Semester, 2008. Date of Defense: December 6, 2007. Diatoms, Holocene, Antarctica Includes bibliographical references. Sherwood W. Wise, Professor Directing Thesis; Jennifer Georgen, Committee Member; Joseph F. Donoghue, Committee Member. Earth sciences FSU_migr_etd-0129 http://purl.flvc.org/fsu/fd/FSU_migr_etd-0129 http://diginole.lib.fsu.edu/islandora/object/fsu%3A168209/datastream/TN/view/Holocene%20Diatoms%20Recovered%20from%20Shaldril%20I%20Cores%2C%20Maxwell%20Bay%2C%20Antarctica.jpg
collection NDLTD
language English
English
format Others
sources NDLTD
topic Earth sciences
spellingShingle Earth sciences
Holocene Diatoms Recovered from Shaldril I Cores, Maxwell Bay, Antarctica
description High-resolution Holocene sediment cores from the continental shelf of Antarctica are integral to the study of recent climate transitions, but such records are rare. The inaugural SHALDRIL I cruise to Maxwell Bay along the Northern Antarctica Peninsula, however, recovered the most expanded record to date at Site NBP05-02-1B. More than twice as long as any other such Antarctic sequence, the 108.2 m section dates back 13,480 yr B.P. Presented here is a record of climate variation interpreted from analyses of the diatom content. Diatoms have proven to be a useful tool in the study of paleoclimate. Analyses completed here include species diversity, total diatom abundance (valves per gram of sediment), Eucampia antarctica var. antarctica to E. antarctica var. recta ratio, Eucampia index, Chaetoceros resting-spore percent, Chaetoceros hyalochaete to C. vegetative ratio, and Thalassiosira antarctica T2 percentage. The analyses show a continuous sea-ice assemblage with minor fluctuations in response to changing sea-ice conditions. Other than the Thalassiosira antarctica T2 percentage, all analyses show a prominent warming period identified as the Mid-Holocene Climatic Optimum. Thalassiosira antarctica T2 percentage marks a period of deglaciation at approximately 11 ka. This episode of deglaciation has been documented in other studies and is believed to mark the onset of present-day ice conditions. === A Thesis submitted to the Department of Geology in partial fulfillment of the requirements for the degree of Master of Science. === Degree Awarded: Spring Semester, 2008. === Date of Defense: December 6, 2007. === Diatoms, Holocene, Antarctica === Includes bibliographical references. === Sherwood W. Wise, Professor Directing Thesis; Jennifer Georgen, Committee Member; Joseph F. Donoghue, Committee Member.
author2 Geary, Lindsey Eileen (authoraut)
author_facet Geary, Lindsey Eileen (authoraut)
title Holocene Diatoms Recovered from Shaldril I Cores, Maxwell Bay, Antarctica
title_short Holocene Diatoms Recovered from Shaldril I Cores, Maxwell Bay, Antarctica
title_full Holocene Diatoms Recovered from Shaldril I Cores, Maxwell Bay, Antarctica
title_fullStr Holocene Diatoms Recovered from Shaldril I Cores, Maxwell Bay, Antarctica
title_full_unstemmed Holocene Diatoms Recovered from Shaldril I Cores, Maxwell Bay, Antarctica
title_sort holocene diatoms recovered from shaldril i cores, maxwell bay, antarctica
publisher Florida State University
url http://purl.flvc.org/fsu/fd/FSU_migr_etd-0129
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