Biogenically induced bedded chert formation in the alkaline palaeo-lake of the Green River Formation
Biogenically induced bedded chert formation in the alkaline palaeo-lake of the Green River Formation
复制标题
格林河组碱性古湖中生物诱发的层状燧石形成
DOI:
10.1038/s41598-019-52862-7
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发表时间:
2019
影响因子:
4.6
通讯作者:
Ikeda Masayuki
中科院分区:
文献类型:
--
作者:
Kuma Ryusei;Hasegawa Hitoshi;Yamamoto Koshi;Yoshida Hidekazu;Whiteside Jessica H.;Katsuta Nagayoshi;Ikeda Masayuki
Rhythmically bedded cherts are observed in both pelagic marine and lacustrine deposits, but the formation mechanism in the latter remains highly uncertain. Our study of alternating chert–dolomite beds in the Eocene Green River Formation, Utah, USA reveals dense accumulations of organic-matter spheres (30–50 μm diameter) of probable algal cyst origin in the chert layers, and centennial- to millennial-scale periodicities in chert layer deposition. A positive correlation between the degree of degradation of the organic spheres and Si distribution implies decomposition of algal organic matter lead to precipitation of lacustrine chert. As both alkalinity and dissolved silica were likely high in the palaeo-lake waters of the Green River Formation, we hypothesize that decomposition of algal organic matter lowered the pH of sediment pore waters and caused silica precipitation. We propose a formation model in which the initial abundance of algal organic matter in sediment varies with productivity at the lake surface, and the decomposition of this algal matter controls the extent of silica precipitation in sediment. The formation of rhythmically bedded chert–dolomite may be linked to centennial- to millennial-scale climatic/environmental factors that modulate algal productivity, which are possibly tied to solar activity cycles known to have similar periodicities.