Magnetostratigraphic evidence for deep-sea erosion on the Pacific Plate, south of Mariana Trench, since the middle Pleistocene: potential constraints for Antarctic bottom water circulation
文献类型：期刊论文
| 作者 | Deng, Xiguang1; Yi, Liang2,3; Paterson, Greig A.4; Qin, Huafeng2; Wang, Haifeng1; Yao, Huiqiang1; Ren, Jiangbo1; Ge, Junyi5; Xu, Hongzhou3; Deng, Chenglong2 |
| 刊名 | INTERNATIONAL GEOLOGY REVIEW
 |
| 出版日期 | 2016-01-02 |
| 卷号 | 58期号:1页码:49-57 |
| 关键词 | Mariana Trench Magnetostratigraphy Plio-pleistocene Abyssal Erosion |
| 文献子类 | Article |
| 英文摘要 | The Antarctic Bottom Water (AABW) current plays a crucial role in storing and transporting heat, water, and nutrients around the world. However, it is impossible to monitor AABW in the Plio-Pleistocene by direct measurement. Hence, abyssal erosion was usually chosen as an effective indicator of the presence of the AABW in the Indian and Eastern Pacific Oceans during that period. Here, we report a high-resolution magnetostratigraphy of a gravity core, the JL7KGC-01A from the south of the Mariana Trench, northwest Pacific Ocean. The main results are as follows: (1) polarity data suggest that the sequence recorded the late Gauss chron to the early Brunhes chron, including the Jaramillo, Cobb Mountain, and Olduvai normal subchrons; (2) the sedimentary processes in the study area since 2.9Ma show three stages of sedimentation: 83cm/Ma during 2.9-1.2Ma, 183cm/Ma during 1.2-0.7Ma, and no sedimentation since similar to 0.7Ma; (3) the area south of the Mariana Trench experienced a significant change in the deposition rate at 1.2Ma, which could be correlated with the intensified desertification in inland Asia, and experienced a prominent depositional hiatus since the early middle Pleistocene, which likely resulted from the enhanced/expanded AABW. Based on these new polarity data and comparisons with previous studies around the Pacific Ocean, we therefore propose that the AABW experienced a notable change during the early-mid Pleistocene transition. |
| WOS关键词 | ISOTHERMAL REMANENT MAGNETIZATION ; MANGANESE-NODULE DEVELOPMENT ; RARE-EARTH-ELEMENTS ; ACQUISITION CURVES ; ROSS-SEA ; MYR AGO ; OCEAN ; SEDIMENTS ; HYSTERESIS ; CONTRASTS |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000361703200004 |
| 源URL | [http://124.16.247.212/handle/311034/7193]  |
| 专题 | 古脊椎动物与古人类研究所_图书馆1 |
| 作者单位 | 1.Guangzhou Marine Geol Survey, Minist Land & Resources, Key Lab Marine Mineral Resources, Guangzhou, Guangdong, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 3.Chinese Acad Sci, Sanya Inst Deep Sea Sci & Engn, Sanya, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earths Deep Interior, Beijing, Peoples R China 5.Chinese Acad Sci, Inst Vertebrate Palaeontol & Palaeoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing, Peoples R China |
| 推荐引用方式 GB/T 7714 | Deng, Xiguang,Yi, Liang,Paterson, Greig A.,et al. Magnetostratigraphic evidence for deep-sea erosion on the Pacific Plate, south of Mariana Trench, since the middle Pleistocene: potential constraints for Antarctic bottom water circulation[J]. INTERNATIONAL GEOLOGY REVIEW,2016,58(1):49-57. |
| APA | Deng, Xiguang.,Yi, Liang.,Paterson, Greig A..,Qin, Huafeng.,Wang, Haifeng.,...&Zhu, Rixiang.(2016).Magnetostratigraphic evidence for deep-sea erosion on the Pacific Plate, south of Mariana Trench, since the middle Pleistocene: potential constraints for Antarctic bottom water circulation.INTERNATIONAL GEOLOGY REVIEW,58(1),49-57. |
| MLA | Deng, Xiguang,et al."Magnetostratigraphic evidence for deep-sea erosion on the Pacific Plate, south of Mariana Trench, since the middle Pleistocene: potential constraints for Antarctic bottom water circulation".INTERNATIONAL GEOLOGY REVIEW 58.1(2016):49-57. |
入库方式： OAI收割
来源：古脊椎动物与古人类研究所
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