Iron and manganese diagenesis in deep sea volcanogenic sediments and the origins of pore water colloids
Iron and manganese diagenesis in deep sea volcanogenic sediments and the origins of pore water colloids
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DOI：
10.1016/j.gca.2011.06.019
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发表时间：
2011-09-01
影响因子：
5
通讯作者：
Palmer, M. R.
中科院分区：
文献类型：
--
作者：
Homoky, W. B.;Hembury, D. J.;Palmer, M. R.
火山沉积物中富含铁、锰矿物，这些矿物在海洋早期成岩作用中发生了大量的蚀变，但它们对全球铁、锰地球化学循环的影响尚未得到广泛的研究。这项研究比较了近表面（海底以下0-20厘米[cmbsf]）含水（
Volcanogenic sediments are typically rich in Fe and Mn-bearing minerals that undergo substantial alteration during early marine diagenesis, however their impact on the global biogeochemical cycling of Fe and Mn has not been widely addressed. This study compares the near surface (0-20 cm below sea floor [cmbsf]) aqueous (