4.1 Article

Late Devonian ostracods (Crustacea) from the Hushoot Shiveetiin gol section (Baruunhuurai Terrane, Mongolia) and their palaeoenvironmental implication and palaeobiogeographic relationship

Journal

PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS
Volume 101, Issue 3, Pages 689-706

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s12549-020-00446-z

Keywords

Ostracods; Mega-Assemblage; Zoogeography; Famennian; Mongolia

Funding

  1. German Academic Exchange Service (DAAD, Research Grant-Doctoral Programme in Germany) [57381412]
  2. German Science Foundation (DFG) [KO 1622-19/1]

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An Upper Devonian to (?)Lower Mississippian section in the Baruunhuurai Terrane of the CAOB was investigated, revealing a well-preserved and diverse ostracod fauna. The Mongolian ostracod fauna shows similarities to coeval faunas in western China and Laurussia, but also includes new, endemic species.
An Upper Devonian to (?)Lower Mississippian section at Hushoot Shiveetiin gol in the Baruunhuurai Terrane of the Central Asian Orogenic Belt (CAOB) was investigated. A generally well-preserved and diverse ostracod fauna was collected from the Late Devonian (Famennian) Samnuuruul Formation in western Mongolia. It is the first rich assemblage described from this area. The ostracod fauna consists of 19 genera and 25 species. Two of the species are proposed new species, and 13 species are described in open nomenclature. The Mongolian ostracod fauna is similar to coeval faunas in western China and Laurussia, but also contains new, endemic species. Two new taxa are described: Beyrichiopsis hushootensis and Ampuloides beckeri. Ostracod findings are characterized by the Eifelian Mega-Assemblage (I-III) representing a nearshore, variable palaeoenvironment which is in accordance with facies analysis provided by other studies.

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