Richness of Famennian-Tournaisian (Late Devonian-early Carboniferous) bryozoans in shallow areas of Palaeotethys and Palaeoasian oceans

Author:

Tolokonnikova ZoyaORCID,Ernst AndrejORCID

Funder

Российский Фонд Фундаментальных Исследований

Publisher

Springer Science and Business Media LLC

Subject

Paleontology,Geology,Ecology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference189 articles.

1. Alekseev, A. S. (1983). Methodic base of numeral analyses of the exchanges in taxonomic diversity of the organic world during “great extinctions”. Bulleten’ MOIP. Otdel Geologicheskiu, 58(5), 126–136. [in Russian]

2. Alekseev, A. S. (1989). Global biotic crises and mass extinctions in Phanerozoic history of the earth. In V. V. Menner (Ed.), Biotic events on the main boundaries of the Phanerozoic (pp. 22–47). Moscow: MGU. [in Russian]

3. Alekseev, A. S. (1998). Mass extinctions in Phanerozoic. MGU: Thesis D. dissertation. Moscow 76 p. [in Russian]

4. Aretz, M., Nardin, E., & Vachard, D. (2014). Diversity patterns and palaeobiogeographical relationships of latest Devonian-lower Carboniferous foraminifers from South China: What is global, what is local? Journal of Palaeontology, 3(1), 35–59.

5. Ariunchimeg, Y. (2000). The first finds of Famennian bryozoans in Mongolia. Paleontological Journal, 34(1), 47–52.

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