Coupled Fe-S isotope composition of sulfide chimneys dominated by temperature heterogeneity in seafloor hydrothermal systems

doi:10.1016/j.scib.2020.06.017

	Coupled Fe-S isotope composition of sulfide chimneys dominated by temperature heterogeneity in seafloor hydrothermal systems
	Wang, Shujie 1,2,3; Sun, Weidong1,2,3,4 ; Huang, Jing 1,2,3; Zhai, Shikui 5; Li, Huaiming 6
	2020-10-30
发表期刊	SCIENCE BULLETIN
ISSN	2095-9273
卷号	65 期号:20 页码:1767-1774
通讯作者	Huang, Jing([email protected])
摘要	Seafloor hydrothermal chimneys are significant metal resources and have fundamental effects on marine chemistry balance. Previous studies on growth of the chimneys focused on mineral composition and elemental distribution in chimney walls, but the isotopic composition of different elements and their correlations remain poorly understood. Here, we report lateral Fe and S isotopes from sulfides across a chimney wall in detail from the Deyin-1 hydrothermal field (DHF) on the South Mid-Atlantic Ridge. Pyrite was characterized by increases in both delta S-34 and delta Fe-56 from the exterior to the interior within the chimney wall, which is likely related to enhanced S and Fe isotope fractionation between pyrite and fluids derived from the temperature gradient. Furthermore, delta Fe-56 displayed a well-defined, linear, positive correlation with delta S-34 in pyrite from the DHF as well as in pyrite from other areas. A model of hydrothermal pyrite formation suggests that, under conditions with uniform hydrothermal fluid, different temperatures and similar pyrite-fluid exchange degrees could result in the observed linear relationships between delta S-34 and delta Fe-56. The regular and coupled Fe-S isotope variations within the chimney wall efficiently constrain the process of hydrothermal sulfide formation. (C) 2020 Science China Press. Published by Elsevier B.V. and Science China Press. All rights reserved.
关键词	Sulfide chimney Iron isotope Sulfur isotope Temperature
DOI	10.1016/j.scib.2020.06.017
收录类别	SCI
语种	英语
资助项目	Strategic Priority Research Program (B) of Chinese Academy of Sciences[XDB42000000]; National Natural Science Foundation of China[41806061]; National Key Research & Development Program of China[2016YFC0600408]; Strategic Priority Research Program (A) of the Chinese Academy of Sciences[XDA22050103]; Taishan Scholar Program of Shandong[ts201712075]; AoShan Talents Cultivation Program; Qingdao Pilot National Laboratory for Marine Science and Technology[2017ASTCPOS07]
WOS研究方向	Science & Technology - Other Topics
WOS类目	Multidisciplinary Sciences
WOS记录号	WOS:000567497700017
出版者	ELSEVIER
引用统计	被引频次：20[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/168759
专题	深海极端环境与生命过程研究中心
通讯作者	Huang, Jing
作者单位	1.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, Qingdao 266071, Peoples R China 2.Pilot Natl Lab Marine Sci & Technol Qingdao, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China 3.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 5.Ocean Univ China, Coll Marine Geosci, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China 6.Minist Nat Resources, Inst Oceanog 2, Key Lab Submarine Geosci, Hangzhou 310012, Peoples R China
第一作者单位	深海极端环境与生命过程研究中心
通讯作者单位	深海极端环境与生命过程研究中心
推荐引用方式 GB/T 7714	Wang, Shujie,Sun, Weidong,Huang, Jing,et al. Coupled Fe-S isotope composition of sulfide chimneys dominated by temperature heterogeneity in seafloor hydrothermal systems[J]. SCIENCE BULLETIN,2020,65(20):1767-1774.
APA	Wang, Shujie,Sun, Weidong,Huang, Jing,Zhai, Shikui,&Li, Huaiming.(2020).Coupled Fe-S isotope composition of sulfide chimneys dominated by temperature heterogeneity in seafloor hydrothermal systems.SCIENCE BULLETIN,65(20),1767-1774.
MLA	Wang, Shujie,et al."Coupled Fe-S isotope composition of sulfide chimneys dominated by temperature heterogeneity in seafloor hydrothermal systems".SCIENCE BULLETIN 65.20(2020):1767-1774.

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