Deepwater carbonate ion concentrations in the western tropical Pacific since 250ka: Evidence for oceanic carbon storage and global climate influence
文献类型：期刊论文
| 作者 | Qin, Bingbin1,3 ; Li, Tiegang2,3,4; Xiong, Zhifang1,2,4; Algeo, Thomas J.5,6; Chang, Fengming1,4
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| 刊名 | PALEOCEANOGRAPHY
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| 出版日期 | 2017-04-01 |
| 卷号 | 32期号:4页码:351-370 |
| 关键词 | shell weight planktonic foraminifera proxy calibration carbonate chemistry coral reef hypothesis ocean stratification |
| 英文摘要 | We present new size-normalized weight (SNW)-[CO32-] core-top calibrations for three planktonic foraminiferal species and assess their reliability as a paleo-alkalinity proxy. SNWs of Globigerina sacculifer and Neogloboquadrina dutertrei can be used to reconstruct past deep Pacific [CO32-], whereas SNWs of Pulleniatina obliquiloculata are controlled by additional environmental factors. Based on this methodological advance, we reconstruct SNW-based deepwater [CO32-] for core WP7 from the western tropical Pacific since 250ka. Secular variation in the SNW proxy documents little change in deep Pacific [CO32-] between the Last Glacial Maximum and the Holocene. Further back in time, deepwater [CO32-] shows long-term increases from marine isotope stage (MIS) 5e to MIS 3 and from early MIS 7 to late MIS 6, consistent with the coral reef hypothesis that the deep Pacific Ocean carbonate system responded to declining shelf carbonate production during these two intervals. During deglaciations, we have evidence of [CO32-] peaks coincident with Terminations 2 and 3, which suggests that a breakdown of oceanic vertical stratification drove a net transfer of CO2 from the ocean to the atmosphere, causing spikes in carbonate preservation (i.e., the deglacial ventilation hypothesis). During MIS 4, a transient decline in SNW-based [CO32-], along with other reported [CO32-] and/or dissolution records, implies that increased deep-ocean carbon storage resulted in a global carbonate dissolution event. These findings provide new insights into the role of the deep Pacific in the global carbon cycle during the late Quaternary. |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000401142500002 |
| 版本 | 出版稿 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/136864]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China 2.State Ocean Adm, Inst Oceanog 1, Qingdao, Peoples R China 3.Univ Chinese Acad Sci, Coll Earth Sci, Beijing, Peoples R China 4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China 5.China Univ Geosci, State Key Labs BGEG & GPMR, Wuhan, Peoples R China 6.Univ Cincinnati, Dept Geol, Cincinnati, OH USA |
| 推荐引用方式 GB/T 7714 | Qin, Bingbin,Li, Tiegang,Xiong, Zhifang,et al. Deepwater carbonate ion concentrations in the western tropical Pacific since 250ka: Evidence for oceanic carbon storage and global climate influence[J]. PALEOCEANOGRAPHY,2017,32(4):351-370. |
| APA | Qin, Bingbin,Li, Tiegang,Xiong, Zhifang,Algeo, Thomas J.,&Chang, Fengming.(2017).Deepwater carbonate ion concentrations in the western tropical Pacific since 250ka: Evidence for oceanic carbon storage and global climate influence.PALEOCEANOGRAPHY,32(4),351-370. |
| MLA | Qin, Bingbin,et al."Deepwater carbonate ion concentrations in the western tropical Pacific since 250ka: Evidence for oceanic carbon storage and global climate influence".PALEOCEANOGRAPHY 32.4(2017):351-370. |
入库方式： OAI收割
来源：海洋研究所
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