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Marine Biology

University of South Carolina

2016

California Current

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Development And Application Of Foraminiferal Carbonate System Proxies To Quantify Ocean Acidification In The California Current, Emily B. Osborne Jan 2016

Development And Application Of Foraminiferal Carbonate System Proxies To Quantify Ocean Acidification In The California Current, Emily B. Osborne

Theses and Dissertations

The oceanic uptake of anthropogenic carbon has mitigated climate change, but has also resulted in a global average 0.1 decline in surface ocean pH over 20th century known as ocean acidification. The parallel reduction in carbonate ion concentration ([CO32-]) and the saturation state of seawater (Ω) has caused many major calcium carbonate-secreting organisms such as planktonic foraminifera to exhibit impaired calcification. We develop proxy calibrations and down core records that use calcification and geochemical characteristics of planktonic foraminifera as proxies for the marine carbonate system. This study focuses specifically on the surface ocean chemistry of the California Current Ecosystem (CCE), …