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Novo (Mitta, 2007, in press), the species close to K. ) peramplus Spath, but not identical. The work was supported by the Programme "Origin and Evolution of the Biosphere" of Russian Academy of Sciences, project "Coevolutionary processes in the Marine Pelagic Biota and Its Response to the Abiotic Changes in the Critical Epochs of the Paleozoic and Mesozoic". 37 South German Substage, Ammonites Zone Callo- S. calloviense Central Russia Zone Ammonites Calloviense G. galilaeii G. galilaeii, G. densicostatus, Ch.

The BathonianlCallovian boundary was established by the appearance ofK. keppleri (Oppel). The similar morphospecies, K. traillensis Donovan, could be found both in the highest levels of the Bathonian, and in bottoms of the Callovian; its definition (and a recognition of specific independence) very often depends on different standpoints of different researchers. No section which is suitable for the Callovian GSSP is revealed on Russian platform now. ) in Central Russian 36 Upper Bathonian. This interval hasn't been studied sufficiently yet in Northern Caucasus and Central Asia.

Groenlandicus were determined from Subcrassum Zone of the Lopsia river. Ammonoids of the Pectinatites genus are One of the most characteristic ones among the Boreal ammonite assemblages of the North-East Europe. New Pectinatites records as well as revision of the previously collected faunas leads to conclusion about the wide faunal exchange within Boreal basin during the whole Early Volgian. Perhaps, unfigured Ilowaiskya from the 33 Lena Basin, Yakutia (Djinoridze, Meledina, 1965; Bidjiev, Mikhailov, 1966) possibly also belongs to Pectinatites (Rogov, 2004).

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