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Main Stages of Evolution of Pacific Ferromanganese Stromatolites and Oncolites


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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.

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V. Avdonin

Moscow State University

编辑信件的主要联系方式.
Email: avdonin@geol.msu.ru
俄罗斯联邦, Moscow, 119991

N. Eremin

Moscow State University

Email: avdonin@geol.msu.ru
俄罗斯联邦, Moscow, 119991

E. Zhegallo

Borissiak Paleontological Institute

Email: avdonin@geol.msu.ru
俄罗斯联邦, Moscow, 117647

N. Segreeva

Moscow State University

Email: avdonin@geol.msu.ru
俄罗斯联邦, Moscow, 119991

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