Long-Term Variability in Pliocene North Pacific Ocean Export Production and Its Implications for Ocean Circulation in a Warmer World
Unlike in the high-latitude North Atlantic, no deep water is formed in the modern subarctic North Pacific. It has previously been suggested that during climate states different from today, this dichotomy did not endure, and the formation of North Pacific Deepwater (NPDW) occurred in the subarctic No...
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ftunivarizona:oai:repository.arizona.edu:10150/673271 2024-09-15T18:24:18+00:00 Long-Term Variability in Pliocene North Pacific Ocean Export Production and Its Implications for Ocean Circulation in a Warmer World Abell, J.T. Winckler, G. Department of Geosciences, University of Arizona 2023-08-17 http://hdl.handle.net/10150/673271 https://doi.org/10.1029/2022AV000853 en eng John Wiley and Sons Inc Abell, J. T., & Winckler, G. (2023). Long-term variability in Pliocene North Pacific Ocean export production and its implications for ocean circulation in a warmer world. AGU Advances, 4, e2022AV000853. https://doi.org/10.1029/2022AV000853 2576-604X doi:10.1029/2022AV000853 http://hdl.handle.net/10150/673271 AGU Advances © 2023. The Authors. This is an open access article under the terms of the Creative Commons Attribution License. https://creativecommons.org/licenses/by/4.0/ AGU Advances constant flux proxy North Pacific Deep Water Pliocene subarctic North Pacific Article text 2023 ftunivarizona https://doi.org/10.1029/2022AV000853 2024-08-05T23:37:16Z Unlike in the high-latitude North Atlantic, no deep water is formed in the modern subarctic North Pacific. It has previously been suggested that during climate states different from today, this dichotomy did not endure, and the formation of North Pacific Deepwater (NPDW) occurred in the subarctic North Pacific, which supported an active Pacific meridional overturning circulation (PMOC). Here we provide new records of productivity and sedimentary redox conditions from the central subarctic North Pacific spanning the late Miocene to early Pleistocene. These reconstructions indicate greater-than-modern and temporally varying North Pacific export production across the interval of ∼2.7–6 Ma. Our time series, combined with previously published data sets and model output for Pliocene North Pacific Ocean dynamics, support the presence of an active PMOC during the Pliocene, and suggest that the characteristics of NPDW formation varied during this warmer interval of Earth's history. This finding of elevated export production at a time of deep water formation presents a conundrum when considering Quaternary North Pacific Ocean dynamics, where subarctic North Pacific productivity declines during intervals when enhanced overturning is posited to occur. We evaluate our data considering the caveats of both (i.e., Pliocene and Quaternary North Pacific circulation) hypotheses, as well as additional mechanisms unrelated to ocean circulation. Because the Pliocene is a possible analogue for near-future climate, our results and analyses have important ramifications for our understanding of regional and global climate in the coming decades as the planet continues to warm. © 2023. The Authors. Open access journal This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. Article in Journal/Newspaper North Atlantic Subarctic The University of Arizona: UA Campus Repository AGU Advances 4 4 |
institution |
Open Polar |
collection |
The University of Arizona: UA Campus Repository |
op_collection_id |
ftunivarizona |
language |
English |
topic |
constant flux proxy North Pacific Deep Water Pliocene subarctic North Pacific |
spellingShingle |
constant flux proxy North Pacific Deep Water Pliocene subarctic North Pacific Abell, J.T. Winckler, G. Long-Term Variability in Pliocene North Pacific Ocean Export Production and Its Implications for Ocean Circulation in a Warmer World |
topic_facet |
constant flux proxy North Pacific Deep Water Pliocene subarctic North Pacific |
description |
Unlike in the high-latitude North Atlantic, no deep water is formed in the modern subarctic North Pacific. It has previously been suggested that during climate states different from today, this dichotomy did not endure, and the formation of North Pacific Deepwater (NPDW) occurred in the subarctic North Pacific, which supported an active Pacific meridional overturning circulation (PMOC). Here we provide new records of productivity and sedimentary redox conditions from the central subarctic North Pacific spanning the late Miocene to early Pleistocene. These reconstructions indicate greater-than-modern and temporally varying North Pacific export production across the interval of ∼2.7–6 Ma. Our time series, combined with previously published data sets and model output for Pliocene North Pacific Ocean dynamics, support the presence of an active PMOC during the Pliocene, and suggest that the characteristics of NPDW formation varied during this warmer interval of Earth's history. This finding of elevated export production at a time of deep water formation presents a conundrum when considering Quaternary North Pacific Ocean dynamics, where subarctic North Pacific productivity declines during intervals when enhanced overturning is posited to occur. We evaluate our data considering the caveats of both (i.e., Pliocene and Quaternary North Pacific circulation) hypotheses, as well as additional mechanisms unrelated to ocean circulation. Because the Pliocene is a possible analogue for near-future climate, our results and analyses have important ramifications for our understanding of regional and global climate in the coming decades as the planet continues to warm. © 2023. The Authors. Open access journal This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. |
author2 |
Department of Geosciences, University of Arizona |
format |
Article in Journal/Newspaper |
author |
Abell, J.T. Winckler, G. |
author_facet |
Abell, J.T. Winckler, G. |
author_sort |
Abell, J.T. |
title |
Long-Term Variability in Pliocene North Pacific Ocean Export Production and Its Implications for Ocean Circulation in a Warmer World |
title_short |
Long-Term Variability in Pliocene North Pacific Ocean Export Production and Its Implications for Ocean Circulation in a Warmer World |
title_full |
Long-Term Variability in Pliocene North Pacific Ocean Export Production and Its Implications for Ocean Circulation in a Warmer World |
title_fullStr |
Long-Term Variability in Pliocene North Pacific Ocean Export Production and Its Implications for Ocean Circulation in a Warmer World |
title_full_unstemmed |
Long-Term Variability in Pliocene North Pacific Ocean Export Production and Its Implications for Ocean Circulation in a Warmer World |
title_sort |
long-term variability in pliocene north pacific ocean export production and its implications for ocean circulation in a warmer world |
publisher |
John Wiley and Sons Inc |
publishDate |
2023 |
url |
http://hdl.handle.net/10150/673271 https://doi.org/10.1029/2022AV000853 |
genre |
North Atlantic Subarctic |
genre_facet |
North Atlantic Subarctic |
op_source |
AGU Advances |
op_relation |
Abell, J. T., & Winckler, G. (2023). Long-term variability in Pliocene North Pacific Ocean export production and its implications for ocean circulation in a warmer world. AGU Advances, 4, e2022AV000853. https://doi.org/10.1029/2022AV000853 2576-604X doi:10.1029/2022AV000853 http://hdl.handle.net/10150/673271 AGU Advances |
op_rights |
© 2023. The Authors. This is an open access article under the terms of the Creative Commons Attribution License. https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1029/2022AV000853 |
container_title |
AGU Advances |
container_volume |
4 |
container_issue |
4 |
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1810464635597357056 |