A Jurassic Anoxic Event in the Pacific Based on Data from the West Kamchatka–Asian Region


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

Based on allochthonous complexes of the Asian–West Kamchatka region, an Early Jurassic (Sinemurian–Toarcian) oceanic anoxic event (J-OAE) in the Nothern Pacific has been revealed for the first time. This event is indicated by sulfide-containing bituminous black cherts that accumulated under euxinic conditions of deep oceanic basins. The anoxia gradually weakened to end completely by the beginning of the Late Jurassic, when hematite jaspers began to accumulate in the aerated water mass. The J-OAE in the Pacific was synchronous to the global warming stage caused by worldwide magmatism; gas-hydrothermal contribution induced a euxinic regime of oceanic water, a change in the carbon cycle, and the change in the taxonomy of radiolarians revealed by Hori [3]. The J-OAE of the Pacific expands the time interval of the known T-OAE and is also supported by the data from other oceanic basins of the world.

作者简介

N. Filatova

Geological Institute, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: filatova.nadezhda.2012@mail.ru
俄罗斯联邦, Moscow, 119017

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2019