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Vol 200
Pages:
336-341
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RUS
Article

About objective and subjective approach to recurrent complexes (for example, brachiopods and bivalves of the ilmen and bureg beds of the middle frasnian, ilmen glint)

Authors:
M. G. Tsinkoburova
About authors
  • Ph.D. associate professor National Mineral Resources University (Mining University)
Date submitted:
2012-07-07
Date accepted:
2012-09-03
Date published:
2013-04-16

Abstract

At the present time researchers are considering recurrence (return of fauna and flora after the return of physical and geographical conditions) one of the drawbacks of biostratigraphic methods. Comparing the features of complex brachiopods and pelecypods of the Ilmen and Bureg beds (middle Frasnian) Ilmen cliff, the author demonstrates the great complexity of the mechanism of recurrence, which depends not only on environmental but also on biological factors. Also a significant role in reducing the reliability of the analysis of systematic diversity of fossiles has biological and paleontological problem species diagnostics (distinction used by different researchers species criteria).

Область исследования:
(Archived) Geology and metallogeny
Keywords:
recurrent complexes brachiopoda bivalvia species criteria Ilmen Glint
Funding:

None

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References

  1. Venyukov P.N. Devonian sediments of the European Russia. Experience of the subdivision sediments and parallelization. Saint Peterburg, Type. B. Demakova. 1884. 333.
  2. Venyukov P.N. Devonian fauna of the North-Western and Central Russia // Reprint of transactions Saint Peterburg of the Society of Naturalists. 1886. V.17, N.2. P.22.
  3. Nalivkin B.V. Ecology of some Devonian bivalves of the Russian platform // Organism and environment in the geological past. Moscow: Nauka, 1966. P.172-181.
  4. Nalivkin B.V. Devonian bivalves of the European part of the USSR: Research Paper...Dr. geol.-mineral. sc. Leningrad: Publshig nouse of the Leningr. State university. 1972. 46.5. Sorokin V.S. Stages of the development of the North-West of the Russian platform in the Frasnian age. Riga: Zinatne. 1978. 282.
  5. Tarasenko A.B. Tempesta beds in the Ilmen clay layers in the Frasnian stage GFC (on the North -West of the Russian plate) // Transactions of the Kazan's University. A series of the natural sciences. 2011. V.153, book.4. P.260-266.

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