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DOI | 10.1038/s41561-022-00978-3 |
Sustained mid-Pliocene warmth led to deep water formation in the North Pacific | |
Ford, H. L.; Burls, N. J.; Jacobs, P.; Jahn, A.; Caballero-Gill, R. P.; Hodell, D. A.; Fedorov, A., V | |
发表日期 | 2022 |
ISSN | 1752-0894 |
EISSN | 1752-0908 |
起始页码 | 658 |
结束页码 | + |
卷号 | 15期号:8页码:16 |
英文摘要 | Marine carbon isotope patterns point to substantial deep water formation in the North Pacific during the mid-Pliocene Warm Period, according to a synthesis of carbon isotope records and isotope-enabled climate modelling. Geologic intervals of sustained warmth such as the mid-Pliocene Warm Period can inform our understanding of future climate change, including the long-term consequences of oceanic uptake of anthropogenic carbon. Here we generate carbon isotope records and synthesize existing records to reconstruct the position of water masses and determine circulation patterns in the deep Pacific Ocean. We show that the mid-depth carbon isotope gradient in the North Pacific was reversed during the mid-Pliocene compared with today, which implies water flowed from north to south and deep water probably formed in the subarctic North Pacific Deep Water. An isotopically enabled climate model that simulates this North Pacific Deep Water reproduces a similar carbon isotope pattern. Modelled levels of dissolved inorganic carbon content in the North Pacific decrease slightly, although the amount of carbon stored in the ocean actually increases by 1.6% relative to modern due to an increase in dissolved inorganic carbon in the surface ocean. Although the modelled Pliocene ocean maintains a carbon budget similar to the present, the change in deep ocean circulation configuration causes pronounced downstream changes in biogeochemistry. |
学科领域 | Geosciences, Multidisciplinary |
语种 | 英语 |
WOS研究方向 | Geology |
WOS记录号 | WOS:000825177800001 |
来源期刊 | NATURE GEOSCIENCE |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/272487 |
作者单位 | University of London; Queen Mary University London; University of Cambridge; George Mason University; George Mason University; National Aeronautics & Space Administration (NASA); NASA Goddard Space Flight Center; University of Colorado System; University of Colorado Boulder; University of Colorado System; University of Colorado Boulder; Yale University |
推荐引用方式 GB/T 7714 | Ford, H. L.,Burls, N. J.,Jacobs, P.,et al. Sustained mid-Pliocene warmth led to deep water formation in the North Pacific[J],2022,15(8):16. |
APA | Ford, H. L..,Burls, N. J..,Jacobs, P..,Jahn, A..,Caballero-Gill, R. P..,...&Fedorov, A., V.(2022).Sustained mid-Pliocene warmth led to deep water formation in the North Pacific.NATURE GEOSCIENCE,15(8),16. |
MLA | Ford, H. L.,et al."Sustained mid-Pliocene warmth led to deep water formation in the North Pacific".NATURE GEOSCIENCE 15.8(2022):16. |
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