MESOZOIC RADIOLARIANS FROM RHYTHMICALLY LAYERED SEDIMENTS OF THE RIMSKY-KORSAKOV ISLANDS (PETER THE GREAT BAY, JAPAN SEA) AND THEIR SIGNIFICANCE FOR DETERMINING THE TRIASSIC-JURASSIC BOUNDARY
МЕЗОЗОЙСКИЕ РАДИОЛЯРИИ ИЗ РИТМИЧНО-СЛОИСТЫХ ОТЛОЖЕНИЙ ОСТРОВОВ АРХИПЕЛАГА РИМСКОГО-КОРСАКОВА (ЗАЛИВ ПЕТРА ВЕЛИКОГО, ЯПОНСКОЕ МОРЕ) И ИХ ЗНАЧЕНИЕ ДЛЯ ОПРЕДЕЛЕНИЯ ГРАНИЦЫ ТРИАСА И ЮРЫ release_kundfvva4re4pfce3yvact6f4m

by O.L. Smirnova, V.I.Ili'ichev Paific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences, E.A. Bessonova, T.A. Emelyanova, V.I.Ili'ichev Paific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences, V.I.Ili'ichev Paific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences

Published in Tikhookeanskaya Geologiya by Yu. A. Kosygin Institute of Tectonics and Geophysics, Far Eastern Branch, RAS.

2021   p39-54

Abstract

The results of the biostratigraphic study based on the radiolarian analysis of the rhythmically layered terrigenous deposits from the Islands of the Rimsky-Korsakov Archipelago (Peter the Great Bay, Japan Sea) have been presented. These deposits are most similar to the medium-grained turbidites. For the first time the distribution and stratigraphic division of the boundary sediments of the upper Triassic and lower Jurassic separated by a marking layer were substantiated in the research area. On the basis of comparisons with isochronous zonal units of the Pacific and Tethyan areas in the upper Triassic sediments of the studied sections, layers with Globolaxtorum tozeri (upper Rhaetian) were established, and in the lower Jurassic zone Pantanellium tanuense Zone (Hettangian) was traced and layers with Parahsuum simplum (Sinemurian – Pliensbachian) were established.
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