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- W2364906838 abstract "The Mid-Cretaceous (125~90 Ma) was one of the warmest greenhouse climate periods of the Phanerozoic, and was characterized by extraordinary igneous events, oceanic anoxia, biotic turnovers and mass extinctions, normal superchron, and oceanic red beds. These geological events were the results of the interactions between the lithosphere, the biosphere and the atmosphere. Each geological event would give rise to a special global change which would play an important role in engendering other events through a system of positive or negative feedbacks. This paper focuses on the introduction of these geological events, the global changes that they caused, and especially climate-ocean system. A special effort is given to the potential linkage and feedback mechanism of these geological events in the the Mid-Cretaceous. It is concluded that the igneous events, such as the emplacement of Large Igneous Provinces were the primary force to cause the abnormal ocean and greenhouse climate through outgas of CO_2, which would have further accelerated the formation of the oceanic anoxia, biotic mass extinctions, and a change in the nature of the sedimentary record." @default.
- W2364906838 created "2016-06-24" @default.
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- W2364906838 date "2005-01-01" @default.
- W2364906838 modified "2023-09-24" @default.
- W2364906838 title "Middle Cretaceous abnormal geological events and global change" @default.
- W2364906838 hasPublicationYear "2005" @default.
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