Specific microaggregates and problematic microfossils as satellites of biochenogenic rocks

Pseudomorphs are formed along the envelopes of whole and destroyed cells as a result of a high rate of fossilization in microbial ecosystems. The destroyed cells may be mistaken for chemogenic formations of colloidal compounds, in particular, aqueous silicon dioxide. This paper focuses on microfacie...

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Veröffentlicht in:Paleontological journal 2014-12, Vol.48 (14), p.1552-1556
Hauptverfasser: Leonova, L. V., Litvinova, T. V., Glavatskikh, S. P.
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Litvinova, T. V.
Glavatskikh, S. P.
description Pseudomorphs are formed along the envelopes of whole and destroyed cells as a result of a high rate of fossilization in microbial ecosystems. The destroyed cells may be mistaken for chemogenic formations of colloidal compounds, in particular, aqueous silicon dioxide. This paper focuses on microfacies, which are either mineralized biofilms or fragments of fossilized bacterial envelopes, as shown by electron microscopy and energy-dispersive spectrometry. In particular, we establish the biomineral origin of a number of mineral aggregates of specific appearance found in the samples studied: stromatolites and segregations.
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subjects Biofilms
Earth and Environmental Science
Earth Sciences
Ecosystems
Electron microscopy
Fossilization
Microfossils
Paleontology
Pseudomorphs
Silica
Spectrometry
title Specific microaggregates and problematic microfossils as satellites of biochenogenic rocks
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