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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 …
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 …
An astronomically dated record of Earth's climate and its predictability over the last 66 million years
Much of our understanding of Earth's past climate comes from the measurement of oxygen
and carbon isotope variations in deep-sea benthic foraminifera. Yet, long intervals in …
and carbon isotope variations in deep-sea benthic foraminifera. Yet, long intervals in …
Cenozoic sea-level and cryospheric evolution from deep-sea geochemical and continental margin records
Using Pacific benthic foraminiferal δ18O and Mg/Ca records, we derive a Cenozoic (66 Ma)
global mean sea level (GMSL) estimate that records evolution from an ice-free Early Eocene …
global mean sea level (GMSL) estimate that records evolution from an ice-free Early Eocene …
The Miocene: The future of the past
Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …
to today. Continental configurations and mountain topography transitioned toward modern …
Late Miocene global cooling and the rise of modern ecosystems
During the late Miocene epoch, about seven million years ago, large areas of the continents
experienced drying, enhanced seasonality, and a restructuring of terrestrial plant and animal …
experienced drying, enhanced seasonality, and a restructuring of terrestrial plant and animal …
[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 fall of the Cretaceous Hot Greenhouse climate
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] 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 …
A new time tree reveals Earth history's imprint on the evolution of modern birds
Determining the timing of diversification of modern birds has been difficult. We combined
DNA sequences of clock-like genes for most avian families with 130 fossil birds to generate …
DNA sequences of clock-like genes for most avian families with 130 fossil birds to generate …