It is generally accepted that photosynthetic marine planktonic bacteria were responsible for
the oxidation of dissolved ferrous iron (Fe (II)) and the subsequent deposition of iron …

Precambrian iron formation provides valuable windows onto ancient marine environments,
but exactly how these Fe-and Si-rich chemical sedimentary rocks formed have remained a …

Paleoarchean jaspilites are used to track ancient ocean chemistry and photoautotrophy
because they contain hematite interpreted to have formed following biological oxidation of …

Host to some of Earth's earliest evidence of life, the fossiliferous lowermost chert-barite
sequence (DFc1) in the∼ 3.5 Ga Dresser Formation of the Pilbara Craton, Western Australia …

原生矿物信息作为前寒武纪条带状铁建造(BIF) 研究的最基本命题, 是研究BIF
成矿规律及其早期地球环境效应的基础. 长期以来, 将低级变质且保存部分原始矿物及沉积结构 …

Sedimentary Fe deposits are both scientifically and economically important. As a major ore
mineral of these deposits, siderite is generally assumed to have been formed via diagenetic …