[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 organic geochemistry of glycerol dialkyl glycerol tetraether lipids: A review
S Schouten, EC Hopmans, JSS Damsté - Organic geochemistry, 2013 - Elsevier
Glycerol dialkyl glycerol tetraether (GDGT) lipids are membrane lipids which were long
thought to be synthesized mainly by archaea, organisms thought to be limited to extreme …
thought to be synthesized mainly by archaea, organisms thought to be limited to extreme …
The geological record of ocean acidification
Ocean acidification may have severe consequences for marine ecosystems; however,
assessing its future impact is difficult because laboratory experiments and field observations …
assessing its future impact is difficult because laboratory experiments and field observations …
[HTML][HTML] The DeepMIP contribution to PMIP4: Methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data …
CJ Hollis, T Dunkley Jones… - Geoscientific Model …, 2019 - gmd.copernicus.org
The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …
Evolution of middle to Late Cretaceous oceans—a 55 my record of Earth's temperature and carbon cycle
A new 55 my global compilation of benthic foraminifera δ13C and δ18O for the middle to
Late Cretaceous shows that there was widespread formation of bottom waters with …
Late Cretaceous shows that there was widespread formation of bottom waters with …
New thoughts about the Cretaceous climate and oceans
WW Hay, S Floegel - Earth-Science Reviews, 2012 - Elsevier
Several new discoveries suggest that the climate of the Cretaceous may have been more
different from that of today than has been previously supposed. Detailed maps of climate …
different from that of today than has been previously supposed. Detailed maps of climate …
Black shale deposition, atmospheric CO2 drawdown, and cooling during the Cenomanian‐Turonian Oceanic Anoxic Event
Oceanic Anoxic Event 2 (OAE2), spanning the Cenomanian‐Turonian boundary (CTB),
represents one of the largest perturbations in the global carbon cycle in the last 100 Myr …
represents one of the largest perturbations in the global carbon cycle in the last 100 Myr …
Cretaceous paleogeography and paleoclimate and the setting of SKI borehole sites in Songliao Basin, northeast China
As a paradigm of greenhouse climate in Earth's history, the Cretaceous provides significant
rock records of global climate changes under conditions of greenhouse climate. The …
rock records of global climate changes under conditions of greenhouse climate. The …
Arctic amplification: can the past constrain the future?
Arctic amplification, the observation that surface air temperature changes in the Arctic
exceed those of the Northern Hemisphere as a whole, is a pervasive feature of climate …
exceed those of the Northern Hemisphere as a whole, is a pervasive feature of climate …
Evolving ideas about the Cretaceous climate and ocean circulation
WW Hay - Cretaceous Research, 2008 - Elsevier
The Cretaceous is a special episode in the history of the Earth named for a unique rock type,
chalk. Chalk is similar to modern deep-sea calcareous ooze and its deposition in …
chalk. Chalk is similar to modern deep-sea calcareous ooze and its deposition in …