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Main Stages of Evolution of Pacific Ferromanganese Stromatolites and Oncolites

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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.

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References

  1. V. V. Avdonin, V. V. Kruglyakov, T. I. Lygina, M. E. Mel’-nikov, and N. E. Sergeeva, Oxide Ferromanganese Ores in the Ocean: Genetic Interpretation for Textures and Structures (GEOS, Moscow, 2014) [in Russian].

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Authors and Affiliations

  1. Moscow State University, Moscow, 119991, Russia

    V. V. Avdonin, N. I. Eremin & N. E. Segreeva

  2. Borissiak Paleontological Institute, Russian Academy of Sciences, Moscow, 117647, Russia

    E. A. Zhegallo

Authors
  1. V. V. Avdonin
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  2. N. I. Eremin
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  3. E. A. Zhegallo
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  4. N. E. Segreeva
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Corresponding author

Correspondence to V. V. Avdonin.

Additional information

Original Russian Text © V.V. Avdonin, N.I. Eremin, E.A. Zhegallo, N.E. Segreeva, 2018, published in Doklady Akademii Nauk, 2018, Vol. 481, No. 1.

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Avdonin, V.V., Eremin, N.I., Zhegallo, E.A. et al. Main Stages of Evolution of Pacific Ferromanganese Stromatolites and Oncolites. Dokl. Earth Sc. 481, 839–841 (2018). https://doi.org/10.1134/S1028334X18070012

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  • DOI: https://doi.org/10.1134/S1028334X18070012

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