Enrichment mechanism of critical metals and records of paleoenvironment in a polymetallic nodule from the Somali Basin
Cheng YuLong1,2,3,4; Xu YongHang3,4; Li DonYi3,4; Chen Jian3,4; Li YunHai3,4; Lin FanYu4; Yin XiJie4
刊名ACTA PETROLOGICA SINICA
2023-09-01
卷号39期号:9页码:2778-2794
关键词Somali Basin Polymetallic nodule Critical metal Enrichment mechanism Paleoenvironment record
ISSN号1000-0569
DOI10.18654/1000-0569/2023.09.14
通讯作者Xu YongHang(xuyonghang@tio.org.cn)
英文摘要Polymetallic nodules are important oceanic mineral resources, which are rich in Mn, Fe, Ni, Cu and critical metals, such as Co and REY (rare earth elements plus yttrium). In order to explore the enrichment mechanism of critical metals and records of paleoenvironment in a nodule from the Somali Basin, Northwest Indian Ocean, its mineral compositions were analyzed by X-ray diffraction (XRD) and fine scale elemental changes were analyzed in situ by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS) and electron probe microanalysis (EPMA). The results show that the structures of the nodule change outward from columnar to palmar and then to columnar. The nodule is primarily composed of hydrogenetic Fe-rich layers with averaged contents of MnO 25. 1%, FeO 30.4%, Co 0.26%, Ni 0.24%, Cu 0.09% and Sigma REY 1981 x 10(-6). However, there is a thin (100 similar to 200 mu m) diagenetic Mn-rich layer in the outer part of the nodule with averaged contents of MnO 52. 0%, FeO 7. 40%, Co 0. 09%, Ni 2.45%, Cu 0.53% and Sigma REY 719 x 10(-6). The Fe -rich layers may mainly contain Fe-vernadite, while the Mn-rich layer may mainly be composed of buserite I Ni and Cu in the nodule are primarily enriched in buserite I, while Co and REY mainly occur in Fe-vernadite and Co shows an "inflection point". HREE are relatively enriched in Mn-rich minerals (buserite I), while LREE are relatively enriched in Fe-vernadite. Sigma REY show a downward trend from inside to outside in the nodule and the change of REY is dominant by Ce. Furthermore, there is a negative correlation between the growth rate of the nodule and its delta Ce while no obvious correlation between Mn/Fe and delta Ce, indicating that the Ce anomaly of the nodule is likely controlled by its growth rate and cannot distinguish the fine scale origin of the nodule and the redox environment alone. According to the empirical formula of Co, the age of the nodule is similar to 1. 46Ma. The initial formation of its columnar structure maybe related to the paleooceanic transition in the late Early Pleistocene, while the palmar structure may grow since similar to 0. 6Ma when intensed dust input after MPT (Middle Pleistocene Climate Transition) caused high Si and Al contents and diluted other metallogenic elements. The Mn-rich layer may origin from the suboxic environment during the Last Interglacial and exhibits symmetry and gradient, which indicates a gradual change and recovery of the redox environment.
WOS关键词CENTRAL INDIAN BASIN ; MANGANESE NODULES ; FERROMANGANESE NODULES ; MINERALOGY ; ELEMENTS
WOS研究方向Geology
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:001059083200014
内容类型期刊论文
源URL[http://ir.qdio.ac.cn/handle/337002/181740]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Xu YongHang
作者单位1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
3.Fujian Prov Key Lab Marine Phys & Geol Proc, Xiamen 361005, Peoples R China
4.Minist Nat Resources, Inst Oceanog 3, Lab Ocean & Coast Geol, Xiamen 361005, Peoples R China
推荐引用方式
GB/T 7714
Cheng YuLong,Xu YongHang,Li DonYi,et al. Enrichment mechanism of critical metals and records of paleoenvironment in a polymetallic nodule from the Somali Basin[J]. ACTA PETROLOGICA SINICA,2023,39(9):2778-2794.
APA Cheng YuLong.,Xu YongHang.,Li DonYi.,Chen Jian.,Li YunHai.,...&Yin XiJie.(2023).Enrichment mechanism of critical metals and records of paleoenvironment in a polymetallic nodule from the Somali Basin.ACTA PETROLOGICA SINICA,39(9),2778-2794.
MLA Cheng YuLong,et al."Enrichment mechanism of critical metals and records of paleoenvironment in a polymetallic nodule from the Somali Basin".ACTA PETROLOGICA SINICA 39.9(2023):2778-2794.
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