Nikitenko, B.L. (2009) Stratigraphy, Paleobiogeography and Biofacies of the Jurassic of Siberia Based on Microfaunas (Foraminifera and Ostracods) [Stratigrafiya, paleobiogeografiya i biofatsii yury Sibiri po mikrofaune (foraminifery i ostrakody)]. Parallel, Novosibirsk, 675. (In Russian with Extended English Summary)

has been cited by the following article:

• TITLE: Kimmeridgian Foraminiferal Faunas of Northern Eurasia: Significance for Interregional Correlations and Palaeobiogeography

  AUTHORS: Clémentine Peggy Anne-Marie Colpaert, Boris Leonidovich Nikitenko

  KEYWORDS: Late Jurassic, Foraminifers, Palaeoceanography, Northern Eurasia

  JOURNAL NAME: Open Journal of Geology, Vol.9 No.10, September 23, 2019

  ABSTRACT: Foraminifer is a very useful microorganism to perform biostratigraphical zonation of the Upper Jurassic. Foraminiferal biozones are calibrated by the ammonite standard zones and can be used for intra- and interregional correlations. Furthermore, the fossil record of foraminiferal faunas is well known among basins of the Northern Eurasia and is also used for accurate palaeoenvironmental, palaeobiogeographical, or biofacial reconstructions. It allows identifying a complex set of biotic and abiotic events which may be used to propose a more general palaeoecoloecological and palaeoceanographical reconstruction of the Subboreal, Boreal, and Arctic seas. Then, the late Kimmeridgian Northern Eurasian seas formed a network of well-connected palaeobasins during the sea-level rise and resulted in rather similar palaeoenvironmental conditions.