中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The Geochemistry and Bioturbation of Clay Sediments Associated with Amalgamated Crusts at the Gagua Ridge

文献类型:期刊论文

作者Chen, Shuai1,2,3; Zeng, Zhigang1,2,3; Wang, Xiaoyuan1,2,3; Yin, Xuebo1,3; Zhu, Bowen1,4; Guo, Kun2,5; Huang, Xin2,6
刊名MINERALS
出版日期2019-03-13
卷号9期号:3页码:16
ISSN号2075-163X
关键词Gagua Ridge amalgamated crusts clay sediments eolian dust bioturbation
DOI10.3390/min9030177
通讯作者Chen, Shuai(chenshuai@qdio.ac.cn) ; Wang, Xiaoyuan(wangxiaoyuan@qdio.ac.cn)
英文摘要Based on the analysis of geochemical and mineralogical compositions, deep sea clay sediment characteristics and their material sources were examined in the eastern flank of the Gagua Ridge. The mineralogy mainly consists of detrital clay minerals, quartz, and authigenic phillipsite. There is scarce biogenic debris (siliceous or calcareous). The consolidated sediments are more enriched in Si, Al, K, Na, Li, Sc, Cr, Rb, and Cs than the associated crusts and nodules. The unmixed sediment samples were mainlycontributed by Asian eolian dust. The onset of the outer Fe-Mn crust growth nearly coincides with the Central Asia aridification event at similar to 3.5 Ma, which resulted in an abrupt increase in eolian flux of Asian dust. Intensified surface primary productivity is assumed to bring more metals to deep waters, and eventually facilitate the outer Fe-Mn crust formation. Authigenic phillipsite may come from the alteration of local basic volcanic glasses and cause excess Al, high Al/Ti, and low Si/Al ratios. However, phillipsites hardly affect the abundance of rare earth elements (REEs) and their patterns. In addition, the investigation of two kinds of burrows inside the consolidated sediments reveals that the inner nodules of the amalgamated crusts may remain on the oxic sediment surface, due to frequent benthic activities.
资助项目Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology[MMRKF201808] ; National Programme on Global Change and Air-Sea Interaction[GASI-GEOGE-02] ; National Natural Science Foundation of China[41306053] ; National Natural Science Foundation of China[41476044] ; National Natural Science Foundation of China[41706052] ; National Natural Science Foundation of China[41325021] ; Open Fund of the Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences[MGE2015KG01] ; Open Fund of the Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences[MGE2011KG09] ; Special Fund for the Taishan Scholar Program of Shandong Province[ts201511061] ; AoShan Talents Program - Qingdao National Laboratory for Marine Science and Technology[2015ASTP-0S17]
WOS研究方向Mineralogy ; Mining & Mineral Processing
语种英语
出版者MDPI
WOS记录号WOS:000464434500003
源URL[http://ir.qdio.ac.cn/handle/337002/161080]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Chen, Shuai; Wang, Xiaoyuan
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Shandong, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266061, Shandong, Peoples R China
3.Chinese Acad Sci, Ctr Ocean Mega Sci, 7 Nanhai Rd, Qingdao 266071, Shandong, Peoples R China
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
5.Shandong Univ Sci & Technol, Coll Earth Sci & Engn, Qingdao 266590, Shandong, Peoples R China
6.Guangdong Ocean Univ, Guangdong Prov Key Lab Coastal Ocean Variat & Dis, Zhanjiang 524088, Peoples R China
推荐引用方式
GB/T 7714
Chen, Shuai,Zeng, Zhigang,Wang, Xiaoyuan,et al. The Geochemistry and Bioturbation of Clay Sediments Associated with Amalgamated Crusts at the Gagua Ridge[J]. MINERALS,2019,9(3):16.
APA Chen, Shuai.,Zeng, Zhigang.,Wang, Xiaoyuan.,Yin, Xuebo.,Zhu, Bowen.,...&Huang, Xin.(2019).The Geochemistry and Bioturbation of Clay Sediments Associated with Amalgamated Crusts at the Gagua Ridge.MINERALS,9(3),16.
MLA Chen, Shuai,et al."The Geochemistry and Bioturbation of Clay Sediments Associated with Amalgamated Crusts at the Gagua Ridge".MINERALS 9.3(2019):16.

入库方式: OAI收割

来源:海洋研究所

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