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DOI | 10.1146/annurev-marine-010419-010906 |
The Biological Pump during the Last Glacial Maximum | |
Galbraith E.D.; Skinner L.C. | |
发表日期 | 2020 |
ISSN | 1941-1405 |
起始页码 | 559 |
结束页码 | 586 |
卷号 | 12 |
英文摘要 | Much of the global cooling during ice ages arose from changes in ocean carbon storage that lowered atmospheric CO2. A slew of mechanisms, both physical and biological, have been proposed as key drivers of these changes. Here we discuss the current understanding of these mechanisms with a focus on how they altered the theoretically defined soft-tissue and biological disequilibrium carbon storage at the peak of the last ice age. Observations and models indicate a role for Antarctic sea ice through its influence on ocean circulation patterns, but other mechanisms, including changes in biological processes, must have been important as well, and may have been coordinated through links with global air temperature. Further research is required to better quantify the contributions of the various mechanisms, and there remains great potential to use the Last Glacial Maximum and the ensuing global warming as natural experiments from which to learn about climate-driven changes in the marine ecosystem. © 2020 by Annual Reviews. All rights reserved. |
英文关键词 | biogeochemistry; carbon dioxide; ice ages; marine ecosystem; ocean circulation |
语种 | 英语 |
scopus关键词 | Aquatic ecosystems; Biogeochemistry; Carbon dioxide; Ecosystems; Global warming; Oceanography; Sea ice; Air temperature; Antarctic sea ice; Biological process; Biological pumps; Ice age; Last Glacial Maximum; Natural experiment; Ocean circulation; Glacial geology; atmosphere-ocean coupling; biogeochemistry; biological pump; carbon dioxide; carbon storage; cooling; global warming; Last Glacial Maximum; Little Ice Age; marine ecosystem; oceanic circulation; sea ice; Antarctica; carbon dioxide; carrier protein; sea water; Antarctica; aquatic species; carbon cycle; chemistry; ecosystem; environmental monitoring; greenhouse effect; ice cover; metabolism; procedures; temperature; Antarctic Regions; Aquatic Organisms; Carbon Cycle; Carbon Dioxide; Ecosystem; Environmental Monitoring; Global Warming; Ice Cover; Membrane Transport Proteins; Seawater; Temperature |
来源期刊 | Annual Review of Marine Science
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/161941 |
作者单位 | Department of Earth and Planetary Sciences, McGill University, Montreal, H3A 0E8, Canada; Institut de Ciència i Tecnologia Ambientals (ICTA-UAB), Universitat Autònoma de Barcelona, Cerdanyola del Vallès, Barcelona, 08193, Spain; Institució Catalana de Recerca i Estudis Avançats (ICREA), Barcelona, 08010, Spain; Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, United Kingdom |
推荐引用方式 GB/T 7714 | Galbraith E.D.,Skinner L.C.. The Biological Pump during the Last Glacial Maximum[J],2020,12. |
APA | Galbraith E.D.,&Skinner L.C..(2020).The Biological Pump during the Last Glacial Maximum.Annual Review of Marine Science,12. |
MLA | Galbraith E.D.,et al."The Biological Pump during the Last Glacial Maximum".Annual Review of Marine Science 12(2020). |
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