Phanerozoic paleotemperatures: The earth's changing climate during the last 540 million years
This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …
have changed during the last 540 million years. It combines paleotemperature …
An atlas of Phanerozoic paleogeographic maps: the seas come in and the seas go out
CR Scotese - Annual Review of Earth and Planetary Sciences, 2021 - annualreviews.org
Paleogeography is the study of the changing surface of Earth through time. Driven by plate
tectonics, the configuration of the continents and ocean basins has been in constant flux …
tectonics, the configuration of the continents and ocean basins has been in constant flux …
[HTML][HTML] Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes
It is well established that greenhouse conditions prevailed during the Cretaceous Period (~
145–66 Ma). Determining the exact nature of the greenhouse-gas forcing, climatic warming …
145–66 Ma). Determining the exact nature of the greenhouse-gas forcing, climatic warming …
The cretaceous period
The breakup of the former Pangea supercontinent culminated in the modern drifting
continents. Increased rifting caused the establishment of the Atlantic Ocean in the middle …
continents. Increased rifting caused the establishment of the Atlantic Ocean in the middle …
[HTML][HTML] Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events
During the mid-Cretaceous, the Earth experienced several environmental perturbations,
including an extremely warm climate and Oceanic Anoxic Events (OAEs). Submarine …
including an extremely warm climate and Oceanic Anoxic Events (OAEs). Submarine …
Glendonites throughout the Phanerozoic
Ikaite is a metastable calcium carbonate hexahydrate (CaCO3· 6H2O), which naturally
occurs in environments characterized by temperatures of− 2 to+ 7° C. It is therefore …
occurs in environments characterized by temperatures of− 2 to+ 7° C. It is therefore …
The magnitude and cause of short-term eustatic Cretaceous sea-level change: A synthesis
DC Ray, FSP van Buchem, G Baines, A Davies… - Earth-Science …, 2019 - Elsevier
No consensus currently exists regarding the magnitude of Cretaceous short-term (less than
3 Ma in duration) eustatic sea-level change. The lack of a consensus limits the ability to …
3 Ma in duration) eustatic sea-level change. The lack of a consensus limits the ability to …
[HTML][HTML] Extinction of fish-shaped marine reptiles associated with reduced evolutionary rates and global environmental volatility
Despite their profound adaptations to the aquatic realm and their apparent success
throughout the Triassic and the Jurassic, ichthyosaurs became extinct roughly 30 million …
throughout the Triassic and the Jurassic, ichthyosaurs became extinct roughly 30 million …
[HTML][HTML] Marine Os isotopic evidence for multiple volcanic episodes during Cretaceous Oceanic Anoxic Event 1b
Abstract The Aptian–Albian boundary is marked by one of the major oceanic perturbations
during the Cretaceous, called Oceanic Anoxic Event (OAE) 1b. Extensive volcanic episodes …
during the Cretaceous, called Oceanic Anoxic Event (OAE) 1b. Extensive volcanic episodes …
[HTML][HTML] Database of global glendonite and ikaite records throughout the Phanerozoic
M Rogov, V Ershova, O Vereshchagin… - Earth System …, 2020 - essd.copernicus.org
This database of Phanerozoic occurrences and isotopic characteristics of metastable cold-
water calcium carbonate hexahydrate (ikaite; CaCO 3· 6H 2 O) and their associated …
water calcium carbonate hexahydrate (ikaite; CaCO 3· 6H 2 O) and their associated …