Glacial/Interglacial Export Production in the Subantarctic South Pacific

Atmospheric CO2 varied considerably in the past; however, the mechanisms that drive this variability are poorly understood. CO2 is linked to marine primary productivity through the biological carbon pump (BCP), leading to hypotheses that past increases in BCP efficiency in areas such as the Southern...

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Main Author: Adamic, Jessica
Format: Thesis
Language:English
Published: 2010
Subjects:
Online Access:http://hdl.handle.net/10484/972
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record_format openpolar
spelling ftindianastauniv:oai:scholars.indstate.edu:10484/972 2024-06-09T07:49:45+00:00 Glacial/Interglacial Export Production in the Subantarctic South Pacific Adamic, Jessica 2010 http://hdl.handle.net/10484/972 en_US eng http://hdl.handle.net/10484/972 Primary productivity (Biology) Oceania Geochemistry Export production South Pacific Phosphorus geochemistry Thesis 2010 ftindianastauniv 2024-05-16T08:40:02Z Atmospheric CO2 varied considerably in the past; however, the mechanisms that drive this variability are poorly understood. CO2 is linked to marine primary productivity through the biological carbon pump (BCP), leading to hypotheses that past increases in BCP efficiency in areas such as the Southern Ocean may have contributed to glacial CO2 drawdown (Sarmiento & Toggweiler, 1984). Productivity has varied considerably in the past, but the extent, timing, and impacts remain poorly understood. The Subantarctic South Pacific is an area of the ocean that is crucial to the understanding of both glacial climate and paleo-export productivity. Unfortunately, few studies have investigated the central South Pacific because it is so remote. The sediment core MV0502-04JC was recovered from the Subantarctic South Pacific in February-March 2005 at 50°S. The results of this study will be compared with data from ODP Leg 189, Site 1171, also in the Subantarctic South Pacific. Data from these cores will be used to evaluate glacial/interglacial paleo-export production and terrigenous provenance using bulk sediment geochemical proxies, including detailed P geochemistry, P, Ba, and metal elemental ratios, and Baxs. The results of this research suggest each site has variable terrigenous provenance that may have relatively different Fe content. Export production at MV0502-4JC is invariant down core; however, Site 1171 does exhibit glacial/interglacial variations in export production. Jessica Adamic Latimer, Jennifer Sandra Brake James Speer Master of Science Department of Earth and Environmental Science Cunningham Memorial library, Terre Haute,Indiana State University GS071610-201001 Masters Title from document title page. Document formatted into pages: contains 60 p.: ill. Includes abstract and appendix. Thesis Southern Ocean Sycamore Scholars at Indiana State University Pacific Sarmiento ENVELOPE(-68.000,-68.000,-72.000,-72.000) Southern Ocean
institution Open Polar
collection Sycamore Scholars at Indiana State University
op_collection_id ftindianastauniv
language English
topic Primary productivity (Biology)
Oceania
Geochemistry
Export production
South Pacific
Phosphorus geochemistry
spellingShingle Primary productivity (Biology)
Oceania
Geochemistry
Export production
South Pacific
Phosphorus geochemistry
Adamic, Jessica
Glacial/Interglacial Export Production in the Subantarctic South Pacific
topic_facet Primary productivity (Biology)
Oceania
Geochemistry
Export production
South Pacific
Phosphorus geochemistry
description Atmospheric CO2 varied considerably in the past; however, the mechanisms that drive this variability are poorly understood. CO2 is linked to marine primary productivity through the biological carbon pump (BCP), leading to hypotheses that past increases in BCP efficiency in areas such as the Southern Ocean may have contributed to glacial CO2 drawdown (Sarmiento & Toggweiler, 1984). Productivity has varied considerably in the past, but the extent, timing, and impacts remain poorly understood. The Subantarctic South Pacific is an area of the ocean that is crucial to the understanding of both glacial climate and paleo-export productivity. Unfortunately, few studies have investigated the central South Pacific because it is so remote. The sediment core MV0502-04JC was recovered from the Subantarctic South Pacific in February-March 2005 at 50°S. The results of this study will be compared with data from ODP Leg 189, Site 1171, also in the Subantarctic South Pacific. Data from these cores will be used to evaluate glacial/interglacial paleo-export production and terrigenous provenance using bulk sediment geochemical proxies, including detailed P geochemistry, P, Ba, and metal elemental ratios, and Baxs. The results of this research suggest each site has variable terrigenous provenance that may have relatively different Fe content. Export production at MV0502-4JC is invariant down core; however, Site 1171 does exhibit glacial/interglacial variations in export production. Jessica Adamic Latimer, Jennifer Sandra Brake James Speer Master of Science Department of Earth and Environmental Science Cunningham Memorial library, Terre Haute,Indiana State University GS071610-201001 Masters Title from document title page. Document formatted into pages: contains 60 p.: ill. Includes abstract and appendix.
format Thesis
author Adamic, Jessica
author_facet Adamic, Jessica
author_sort Adamic, Jessica
title Glacial/Interglacial Export Production in the Subantarctic South Pacific
title_short Glacial/Interglacial Export Production in the Subantarctic South Pacific
title_full Glacial/Interglacial Export Production in the Subantarctic South Pacific
title_fullStr Glacial/Interglacial Export Production in the Subantarctic South Pacific
title_full_unstemmed Glacial/Interglacial Export Production in the Subantarctic South Pacific
title_sort glacial/interglacial export production in the subantarctic south pacific
publishDate 2010
url http://hdl.handle.net/10484/972
long_lat ENVELOPE(-68.000,-68.000,-72.000,-72.000)
geographic Pacific
Sarmiento
Southern Ocean
geographic_facet Pacific
Sarmiento
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation http://hdl.handle.net/10484/972
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