Atmospheric CO2 over the Past 66 Million Years from Marine Archives
Throughout Earth's history, CO2 is thought to have exerted a fundamental control on
environmental change. Here we review and revise CO2 reconstructions from boron isotopes …
environmental change. Here we review and revise CO2 reconstructions from boron isotopes …
[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 rise and demise of the Paleogene Central Tibetan Valley
Reconstructing the Paleogene topography and climate of central Tibet informs
understanding of collisional tectonic mechanisms and their links to climate and biodiversity …
understanding of collisional tectonic mechanisms and their links to climate and biodiversity …
Asteroid impact, not volcanism, caused the end-Cretaceous dinosaur extinction
AA Chiarenza, A Farnsworth… - Proceedings of the …, 2020 - National Acad Sciences
The Cretaceous/Paleogene mass extinction, 66 Ma, included the demise of non-avian
dinosaurs. Intense debate has focused on the relative roles of Deccan volcanism and the …
dinosaurs. Intense debate has focused on the relative roles of Deccan volcanism and the …
Past East Asian monsoon evolution controlled by paleogeography, not CO2
The East Asian monsoon plays an integral role in human society, yet its geological history
and controlling processes are poorly understood. Using a general circulation model and …
and controlling processes are poorly understood. Using a general circulation model and …
Orographic evolution of northern Tibet shaped vegetation and plant diversity in eastern Asia
The growth of the Tibetan Plateau throughout the past 66 million years has profoundly
affected the Asian climate, but how this unparalleled orogenesis might have driven …
affected the Asian climate, but how this unparalleled orogenesis might have driven …
[HTML][HTML] The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons
Abstract The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …
No high Tibetan plateau until the Neogene
The Late Paleogene surface height and paleoenvironment for the core area of the Qinghai-
Tibetan Plateau (QTP) remain critically unresolved. Here, we report the discovery of the …
Tibetan Plateau (QTP) remain critically unresolved. Here, we report the discovery of the …
The rise and fall of the Cretaceous Hot Greenhouse climate
BT Huber, KG MacLeod, DK Watkins… - Global and Planetary …, 2018 - Elsevier
A compilation of foraminiferal stable isotope measurements from southern high latitude
(SHL) deep-sea sites provides a novel perspective important for understanding Earth's …
(SHL) deep-sea sites provides a novel perspective important for understanding Earth's …
[HTML][HTML] A high-resolution climate simulation dataset for the past 540 million years
Abstract The Phanerozoic Eon has witnessed considerable changes in the climate system
as well as abundant animals and plant life. Therefore, the evolution of the climate system in …
as well as abundant animals and plant life. Therefore, the evolution of the climate system in …