Email this article 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
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Affiliations:
- Moscow State University
- 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.
About the authors
V. V. Avdonin
Moscow State University
Author for correspondence.
Email: avdonin@geol.msu.ru
Russian Federation, Moscow, 119991
N. I. Eremin
Moscow State University
Email: avdonin@geol.msu.ru
Russian Federation, Moscow, 119991
E. A. Zhegallo
Borissiak Paleontological Institute
Email: avdonin@geol.msu.ru
Russian Federation, Moscow, 117647
N. E. Segreeva
Moscow State University
Email: avdonin@geol.msu.ru
Russian Federation, Moscow, 119991
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