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机译:二叠纪-三叠纪过渡期中上层泛海深海中的硫同位素分布
Graduate School of Science, Tohoku University, Aoba-ku, Sendai 980-8578, Japan;
Graduate School of Science, Tohoku University, Aoba-ku, Sendai 980-8578, Japan;
Department of Earth Sciences, Graduate School of Science and Engineering, Ehime University 790-8577, Japan;
Department of Earth and Planetary Science, Washington University, St Louis MO 63130, USA;
Graduate School of Science, Tohoku University, Aoba-ku, Sendai 980-8578, Japan;
Department of Earth Sciences, Faculty of Education and Culture, University of Miyazaki 889-2192, Japan;
Department of Geology, Faculty of Agriculture, Utsunomiya University, Utsunomiya 321-8505, Japan;
Geosciences Institute, Hyogo University of Teacher Education, Hyogo 673-1494, Japan;
Geology, School of Environment, The University of Auckland, Private Bag 92019, Auckland 1142, New Zealand;
Graduate School of Science, Tohoku University, Aoba-ku, Sendai 980-8578, Japan;
Graduate School of Science, Tohoku University, Aoba-ku, Sendai 980-8578, Japan;
mass extinction; Panthalassa; pelagic deep sea; Permian; Triassic; sulfur isotope; Japan; New Zealand;
机译:追踪中三叠世至侏罗纪中上层泛海的深海中的氧化还原历史和氮循环:对氧化还原敏感元素和氮同位素的见解
机译:使用稳定的碳和硫同位素的表层环境中深液的进化:德克萨斯州南部艾德华岛含水层过渡区的情况
机译:来自深海水热系统的大规模硫化物的硫和铅同位素组合物:对矿石创世纪和流体循环的影响
机译:同位素富集硅中深双供体硫的杂质吸收光谱
机译:深海热液喷口中硫同位素分馏的地质生物学控制。
机译:SUP05在中波罗的海和黑海的中上层氧化还原系中占主导地位的是γ变形菌硫氧化剂。
机译:来自深海热液系统的块状硫化物的硫和铅同位素组成:对矿石成因和流体循环的影响。