Journal Article10.1016/J.EARSCIREV.2021.103503
Phanerozoic Paleotemperatures: The Earth’s Changing Climate during the Last 540 million years
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TL;DR: In this article, the history of global changes in temperature during the Phanerozoic has been summarized in a “paleotemperature timescale” that subdivides the many past climatic events into 8 major climate modes; each climate mode is made up of 3-4 pairs of warming and cooling episodes (chronotemps) and a detailed narrative describes how these past temperature events have been affected by geological processes such as the eruption of Large Igneous Provinces (LIPS) (warming) and bolide impacts (cooling).
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About: This article is published in Earth-Science Reviews. The article was published on 01 Apr 2021. The article focuses on the topics: Global warming & Climate change.
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References
Chapter 2Toward understanding Late Devonian global events: few answers, many questions
TL;DR: In particular, the emerging severity of the end-Givetian and end-Famennian extinctions contrasts with the current overemphasis on the stepwise F-F crisis.
131
Isotopic signals from late Jurassic–early Cretaceous (Volgian–Valanginian) sub-Arctic belemnites, Yatria River, Western Siberia
Gregory D. Price,Jörg Mutterlose +1 more
TL;DR: The first detailed oxygen and carbon isotope record from the latest Jurassic-early Cretaceous interval of the Yatria River, subpolar Urals, Siberia was presented in this paper.
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Development of the circum-antarctic current.
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TL;DR: Deep-sea drilling in the Southern Ocean south of Australia and New Zealand shows that the Circum-Antarctic Current developed about 30 million years ago in the middle to late Oligocene when final separation occurred between Antarctica and the continental South Tasman Rise.
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Modeling the early Paleozoic long-term climatic trend
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The architecture of oceanic plateaus revealed by the volcanic stratigraphy of the accreted Wrangellia oceanic plateau
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