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Upper Llandovery and Lower Wenlock boundary of the Central part of Chernyshev ridge
Пограничные отложения лландовери и венлока в опорном разрезе силура центральной части гряды Чернышева
2015
Vestnik of Institute of Geology of Komi Science Center of Ural Branch RAS
Пограничные отложения лландовери и венлока в опорном разрезе силура центральной части гряды Чернышева
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ñòàòüå ïðèâîäÿòñÿ íîâûå õåìî-è áèîñòðàòèãðàôè÷åñêèå äàííûå, õàðàêòåðèçóþùèå õðîíîëîãèþ ñìåíû ôàóíèñ-òè÷åñêèõ êîìïëåêñîâ â îòëîaeåíèÿõ íèaeíåãî ñèëóðà îïîðíîãî ðàçðåçà ð. Øàðúþ, è äàííûå ïî ïàëåîíòîëîãèè è ïàëåîýêîëîãèè, èñïîëüçóåìûå äëÿ äèàãíîñòèêè è êîððåëÿöèè ñòðàòèãðàôè÷åñêèõ ãðàíèö. Êëþ÷åâûå ñëîâà: áðàõèîïîäû, êîíîäîíòû, ëëàíäîâåðè -âåíëîê, èçîòîïû δC 13 . Research aimed at identifying changes in biota due to large-scale geological events, using isotope stratigraphy, changed understanding
doi:10.19110/2221-1381-2015-12-24-30
fatcat:6vy22nuyrnglveptxed7o4fekm