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An atlas of Phanerozoic paleogeographic maps: the seas come in and the seas go out
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 …
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 …
A 485-million-year history of Earth's surface temperature
A long-term record of global mean surface temperature (GMST) provides critical insight into
the dynamical limits of Earth's climate and the complex feedbacks between temperature and …
the dynamical limits of Earth's climate and the complex feedbacks between temperature and …
Ocean temperatures through the Phanerozoic reassessed
The oxygen isotope compositions of carbonate and phosphatic fossils hold the key to
understanding Earth-system evolution during the last 500 million years. Unfortunately, the …
understanding Earth-system evolution during the last 500 million years. Unfortunately, the …
A Great late Ediacaran ice age
The emergence of the Ediacara biota soon after the Gaskiers glaciation ca. 580 million years
ago (Ma) implies a possible glacial fuse for the evolution of animals. However, the timing of …
ago (Ma) implies a possible glacial fuse for the evolution of animals. However, the timing of …
Earth history events shaped the evolution of uneven biodiversity across tropical moist forests
Far from a uniform band, the biodiversity found across Earth's tropical moist forests varies
widely between the high diversity of the Neotropics and Indomalaya and the relatively lower …
widely between the high diversity of the Neotropics and Indomalaya and the relatively lower …
Acceleration of phosphorus weathering under warm climates
L Guo, S ** paleo-Köppen climatic zones using a Bayesian statistical analysis of lithologic, paleontologic, and geochemical proxies
Abstract The Cretaceous Period (145 to 66 Ma) was a prolonged warmhouse to hothouse
period characterized by high atmospheric CO 2 conditions, elevated surface temperatures …
period characterized by high atmospheric CO 2 conditions, elevated surface temperatures …