Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Vasiliy V. Marusin"'
Publikováno v:
Lethaia. 55:1-17
Autor:
A. V. Shatsillo, S. V. Rud’ko, N. B. Kuznetsov, T. V. Romanyuk, G. A. Karlova, Boris G. Pokrovsky, Alena A. Kolesnikova, Vasiliy V. Marusin, B. B. Kochnev, A.S. Dubenskiy, S. M. Lyapunov, V. S. Sheshukov
Publikováno v:
Geological Magazine. 158:1156-1172
A number of ecological and geochemical transformations occurred during late Ediacaran and early Cambrian time, the effects of which are difficult to overestimate. However, the strong linkage of biostratigraphic and chemostratigraphic methods with lit
Autor:
Boris B. Kochnev, Andrey K. Khudoley, Nadezhda S. Priyatkina, S. Andrew Dufrane, Boris G. Pokrovsky, Anton B. Kuznetsov, Olga K. Kaurova, Vasiliy V. Marusin
Publikováno v:
Precambrian Research. 382:106877
Publikováno v:
Paleontological Journal. 53:566-574
The Vendian–Cambrian transitional strata of the Igarka Uplift (northwestern Siberian Platform), originally erected as the Sukharikha Formation, are one of the key objects revealing evolution of marine ecosystems in the late Vendian. Herein we descr
Publikováno v:
Lethaia. 52:464-485
Autor:
Vasiliy V. Marusin, Natalia Bykova
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
G. A. Karlova, Vasiliy V. Marusin, B. B. Kochnev, Huan Cui, Alan J. Kaufman, Dmitriy V. Grazhdankin, K.E. Nagovitsin, Sara Peek, Zhiger Sarsembaev, Olga P. Izokh, Georgiy E. Markov
The concept of the Tommotian Regional Stage of the Siberian Platform has been closely linked to the idea of the ‘Cambrian Explosion’ of animals and protists when the entire Earth system shifted rapidly into Phanerozoic mode. We conducted a multid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2d625a14cd880f4839071b088250d78
https://hdl.handle.net/20.500.14017/a0f28786-c5b7-4a9c-89b9-9248d764ff2f
https://hdl.handle.net/20.500.14017/a0f28786-c5b7-4a9c-89b9-9248d764ff2f
Publikováno v:
PalZ. 92:557-560
Publikováno v:
Russian Geology and Geophysics. 59:585-605
We propose a detailed δ13C curve for the Vendian and Lower Cambrian (Tommotian) strata of the central Siberian Platform. Two positive carbon isotope excursions identified near the base of the Yuryakh Formation (up to 5.5‰) and in the lower Bilir F