微生物垫
成岩作用
地质学
基质(水族馆)
火山
沉积物
地球化学
矿物学
古生物学
细菌
蓝藻
海洋学
作者
Francès Westall,Sjoukje T. de Vries,Wouter Nijman,Virgile Rouchon,Beate Orberger,V. K. Pearson,Jonathan S. Watson,A. B. Verchovsky,I. P. Wright,Jean‐Noël Rouzaud,Daniele Marchesini,Severine Anne
出处
期刊:Geological Society of America eBooks
[Geological Society of America]
日期:2006-01-01
被引量:108
标识
DOI:10.1130/2006.2405(07)
摘要
A multidisciplinary study of silicified volcanoclastic, near-shore deposits from the 3.446 Ga "Kitty's Gap Chert," Warrawoona Group, Pilbara, reveals that they contain a wealth of carbonaceous microbial fossil remains. The volcanoclastic sediments host predominantly colonies of coccoidal microorganisms that occur in two modal size ranges, 0.4–0.5 μm and 0.75–0.8 μm. These microbial colonies coat the surfaces of the volcanic particles and form either dense, carpetlike associations up to tens of micrometers in diameter comprising hundreds of individuals. They also form less dense concentrations that include many chainlike associations of coccoids. All colonies are associated with a polymer film (extracellular polymeric substances—EPS) that coats both the organisms and their substrate. Multispecies biofilms formed at a boundary representing a short period of nondeposition. They consisted predominantly of coccoids and EPS but also included common, small filaments tens of micrometers in length and 0.25 μm in width and rare, short rods 1 μm in length. Carbon isotopic compositions of about −26‰ to −30‰, measured on individual layers, are compatible with microbial fractionation. The biofilms include possible anoxygenic-photosynthesizing organisms (the filaments), whereas the colonies coating the volcanic clasts probably represent chemolithotrophic organisms. The interaction between the microbes, their colonies and biofilms, and their environment is intimate and complex. The environment provided the substrate and the nutrient, energy, and carbon sources, whereas the metabolic activity of the microbes contributed to the early diagenetic alteration of the volcanic particles, to the binding of the sediment, and to their silicification. The microorganisms were preserved by rapid silicification, with the silica coming partly from hydrothermal sources and partly from pore water enrichment in Si due to the devitrification of the volcanic protoliths (partially mediated by microbial activity).
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