Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene
An undergraduate thesis submitted in partial application for the Honors degree in Earth Sciences. The mid-to-late Pliocene (~3.3 – 2.5 Ma) is an intriguing period for investigating Earth’s past climate dynamics as a potential analogue for future warmth due to anthropogenic climate change. In the Sou...
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ftriceuniv:oai:scholarship.rice.edu:1911/109255 2023-06-11T04:06:56+02:00 Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene Nirenberg, Jared Ash, Jeanine Masiello, Carrie 2020-05 37 pp application/pdf https://hdl.handle.net/1911/109255 eng eng Rice University Nirenberg, Jared. "Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene." Undergraduate thesis, Rice University, 2020. https://doi.org/10.25611/5098-yx37. https://hdl.handle.net/1911/109255 https://doi.org/10.25611/5098-yx37 Copyright is held by author. Ross Sea Pliocene West Antarctic Ice Sheet biogeochemistry sedimentology Thesis Text 2020 ftriceuniv https://doi.org/10.25611/5098-yx37 2023-05-06T22:31:00Z An undergraduate thesis submitted in partial application for the Honors degree in Earth Sciences. The mid-to-late Pliocene (~3.3 – 2.5 Ma) is an intriguing period for investigating Earth’s past climate dynamics as a potential analogue for future warmth due to anthropogenic climate change. In the Southern Ocean, the Ross Sea and the adjacent West Antarctic Ice Sheet exert significant influence on global climate through their roles in carbon cycle processes, deep ocean circulation, and eustatic sea level. Previous ocean drilling records have shown that the marine-based West Antarctic Ice Sheet exhibited highly dynamic behavior in the Pliocene and responded to cyclical variations in Earth’s orbital geometry. However, fundamental questions remain regarding the biogeochemical response of Southern Ocean marine productivity to changes in ice sheet dynamics and sea ice cover. The International Ocean Discovery Program’s Expedition 374 to the Ross Sea (2018) recovered multiple sediment cores, including those from Site U1524 on the continental rise. I present a 900,000 year record of the carbon and nitrogen content in bulk sediment in the Pliocene-aged cores from Hole U1524A. This record shows the response of carbon export from the Ross Sea continental shelf to orbital and longer-term forcings of the West Antarctic Ice Sheet and global climate. From 3.3 to 3.0 million years ago, I observe a gradual, non-monotonic increase in organic carbon to nitrogen ratios, followed by a decrease from 3.0 to 2.8 million years ago. Sediment color reflectance measurements, implying changes in surface water productivity, are tightly anti-correlated with organic carbon to nitrogen ratios between 3.3 and 3.0 million years ago, but are positively correlated between 3.0 and 2.8 million years ago. I discuss these trends in the context of concurrent sedimentology, physical oceanography, and ice-sheet dynamics. Finally, I note that potential diagenetic effects limit interpretation of this record, and I suggest that bulk carbon and nitrogen ... Thesis Antarc* Antarctic Ice Sheet Ross Sea Sea ice Southern Ocean Rice University: Digital Scholarship Archive Antarctic Ross Sea Southern Ocean West Antarctic Ice Sheet |
institution |
Open Polar |
collection |
Rice University: Digital Scholarship Archive |
op_collection_id |
ftriceuniv |
language |
English |
topic |
Ross Sea Pliocene West Antarctic Ice Sheet biogeochemistry sedimentology |
spellingShingle |
Ross Sea Pliocene West Antarctic Ice Sheet biogeochemistry sedimentology Nirenberg, Jared Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene |
topic_facet |
Ross Sea Pliocene West Antarctic Ice Sheet biogeochemistry sedimentology |
description |
An undergraduate thesis submitted in partial application for the Honors degree in Earth Sciences. The mid-to-late Pliocene (~3.3 – 2.5 Ma) is an intriguing period for investigating Earth’s past climate dynamics as a potential analogue for future warmth due to anthropogenic climate change. In the Southern Ocean, the Ross Sea and the adjacent West Antarctic Ice Sheet exert significant influence on global climate through their roles in carbon cycle processes, deep ocean circulation, and eustatic sea level. Previous ocean drilling records have shown that the marine-based West Antarctic Ice Sheet exhibited highly dynamic behavior in the Pliocene and responded to cyclical variations in Earth’s orbital geometry. However, fundamental questions remain regarding the biogeochemical response of Southern Ocean marine productivity to changes in ice sheet dynamics and sea ice cover. The International Ocean Discovery Program’s Expedition 374 to the Ross Sea (2018) recovered multiple sediment cores, including those from Site U1524 on the continental rise. I present a 900,000 year record of the carbon and nitrogen content in bulk sediment in the Pliocene-aged cores from Hole U1524A. This record shows the response of carbon export from the Ross Sea continental shelf to orbital and longer-term forcings of the West Antarctic Ice Sheet and global climate. From 3.3 to 3.0 million years ago, I observe a gradual, non-monotonic increase in organic carbon to nitrogen ratios, followed by a decrease from 3.0 to 2.8 million years ago. Sediment color reflectance measurements, implying changes in surface water productivity, are tightly anti-correlated with organic carbon to nitrogen ratios between 3.3 and 3.0 million years ago, but are positively correlated between 3.0 and 2.8 million years ago. I discuss these trends in the context of concurrent sedimentology, physical oceanography, and ice-sheet dynamics. Finally, I note that potential diagenetic effects limit interpretation of this record, and I suggest that bulk carbon and nitrogen ... |
author2 |
Ash, Jeanine Masiello, Carrie |
format |
Thesis |
author |
Nirenberg, Jared |
author_facet |
Nirenberg, Jared |
author_sort |
Nirenberg, Jared |
title |
Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene |
title_short |
Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene |
title_full |
Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene |
title_fullStr |
Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene |
title_full_unstemmed |
Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene |
title_sort |
glacially-controlled variations in the biological pump of the ross sea in the mid-to-late pliocene |
publisher |
Rice University |
publishDate |
2020 |
url |
https://hdl.handle.net/1911/109255 |
geographic |
Antarctic Ross Sea Southern Ocean West Antarctic Ice Sheet |
geographic_facet |
Antarctic Ross Sea Southern Ocean West Antarctic Ice Sheet |
genre |
Antarc* Antarctic Ice Sheet Ross Sea Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Ice Sheet Ross Sea Sea ice Southern Ocean |
op_relation |
Nirenberg, Jared. "Glacially-controlled variations in the biological pump of the Ross Sea in the Mid-to-Late Pliocene." Undergraduate thesis, Rice University, 2020. https://doi.org/10.25611/5098-yx37. https://hdl.handle.net/1911/109255 https://doi.org/10.25611/5098-yx37 |
op_rights |
Copyright is held by author. |
op_doi |
https://doi.org/10.25611/5098-yx37 |
_version_ |
1768379194264256512 |