Discovery of shallow-marine biofacies conodonts in a bioherm within the Carboniferous-Permian transition in the Omolon Massif, NE Russia near the North paleo-pole: Correlation with a warming spike in the southern hemisphere

cited authors

  • Davydov, Vladimir I; Biakov, Alexander S

fiu authors

publication date

  • September 1, 2015

keywords

  • AMMONOIDS
  • BIOSTRATIGRAPHY
  • BIVALVES
  • Conodonts
  • Geology
  • Geosciences, Multidisciplinary
  • HINDEODUS
  • KOLYMA-OMOLON
  • NE Russia
  • OKHOTSK REGION
  • Omolon Massif
  • Physical Sciences
  • Science & Technology
  • Shelly fauna
  • Uppermost Carboniferous to Permian transition
  • Warming event

WoS ID

  • 000359169600026

Digital Object Identifier (DOI)

start page

  • 888

end page

  • 897

volume

  • 28

issue

  • 2