Main Stages of Evolution of Pacific Ferromanganese Stromatolites and Oncolites

V. V. Avdonin; N. I. Eremin; E. A. Zhegallo; N. E. Segreeva

doi:10.1134/S1028334X18070012

Main Stages of Evolution of Pacific Ferromanganese Stromatolites and Oncolites

Authors: Avdonin V.V.¹, Eremin N.I.¹, Zhegallo E.A.², Segreeva N.E.¹
Affiliations:
1. Moscow State University
2. Borissiak Paleontological Institute
Issue: Vol 481, No 1 (2018)
Pages: 839-841
Section: Geology
URL: https://journals.rcsi.science/1028-334X/article/view/193521
DOI: https://doi.org/10.1134/S1028334X18070012
ID: 193521

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Abstract

As exemplified by cobalt–bearing Fe–Mn crusts (ferromanganese stromatolite) of the Magellan Seamounts (Clarion–Clipperton Province), the main stages of the structural evolution of bacterial communities have been recognized. It has been demonstrated that the change of the stages is caused by the effect of major tectonic, volcanic, and other geological events.