A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2 - Concepedia

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A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2

184

Citations

43

References

2010

Year

Jaap S. Sinninghe Damsté, Elisabeth C. van Bentum, Gert‐Jan Reichart, Jörg Pross, Stefan Schouten

Earth and Planetary Science Letters

EngineeringLatitudinal Temperature GradientCretaceous PeriodOceanographyCo2 Decrease-driven CoolingCretaceous-paleogene BoundaryPaleoclimatologyEarth Science

References

	Year	Citations

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