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

doi:10.1080/00206814.2015.1055597

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 岩石圈演化国家重点实验室

	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
	Deng, Xiguang 1; Yi, Liang 2,3; Paterson, Greig A.4; Qin, Huafeng 2; Wang, Haifeng 1; Yao, Huiqiang 1; Ren, Jiangbo 1; Ge, Junyi 5; Xu, Hongzhou 3; Deng, Chenglong 2
刊名	INTERNATIONAL GEOLOGY REVIEW
	2016-01-02
卷号	58 期号:1 页码:49-57
关键词	Mariana Trench magnetostratigraphy Plio-Pleistocene abyssal erosion
DOI	10.1080/00206814.2015.1055597
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
资助机构	China Geological Survey Programme(FZH201100303) ; China Geological Survey Programme(FZH201100303) ; National Natural Science Foundation of China(41402153 ; National Natural Science Foundation of China(41402153 ; National Key Basic Research Programme of China(2012CB821900) ; National Key Basic Research Programme of China(2012CB821900) ; Strategic Priority Research Programme of CAS(XDB06020101) ; Strategic Priority Research Programme of CAS(XDB06020101) ; 40925012) ; 40925012) ; China Geological Survey Programme(FZH201100303) ; China Geological Survey Programme(FZH201100303) ; National Natural Science Foundation of China(41402153 ; National Natural Science Foundation of China(41402153 ; National Key Basic Research Programme of China(2012CB821900) ; National Key Basic Research Programme of China(2012CB821900) ; Strategic Priority Research Programme of CAS(XDB06020101) ; Strategic Priority Research Programme of CAS(XDB06020101) ; 40925012) ; 40925012)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/62239]
专题	地质与地球物理研究所_岩石圈演化国家重点实验室
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.