[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 …
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 …
[图书][B] Introduction to organic geochemistry
SD Killops, VJ Killops - 2013 - books.google.com
An Introduction to Organic Geochemistry explores the fate of organic matter of all types,
biogenic and man-made, in the Earth System. investigates the variety of pathways and …
biogenic and man-made, in the Earth System. investigates the variety of pathways and …
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 …
CO2-forced climate thresholds during the Phanerozoic
DL Royer - Geochimica et Cosmochimica Acta, 2006 - Elsevier
The correspondence between atmospheric CO2 concentrations and globally averaged
surface temperatures in the recent past suggests that this coupling may be of great antiquity …
surface temperatures in the recent past suggests that this coupling may be of great antiquity …
Evidence for rapid climate change in the Mesozoic–Palaeogene greenhouse world
HC Jenkyns - … Transactions of the Royal Society of …, 2003 - royalsocietypublishing.org
The best–documented example of rapid climate change that characterized the so–called
'greenhouse world'took place at the time of the Palaeocene–Eocene boundary: introduction …
'greenhouse world'took place at the time of the Palaeocene–Eocene boundary: introduction …
The latitudinal temperature gradient and its climate dependence as inferred from foraminiferal δ18O over the past 95 million years
The latitudinal temperature gradient is a fundamental state parameter of the climate system
tied to the dynamics of heat transport and radiative transfer. Thus, it is a primary target for …
tied to the dynamics of heat transport and radiative transfer. Thus, it is a primary target for …
Mesozoic climates: General circulation models and the rock record
BW Sellwood, PJ Valdes - Sedimentary geology, 2006 - Elsevier
General circulation models (GCMs) use the laws of physics and an understanding of past
geography to simulate climatic responses. They are objective in character. However, they …
geography to simulate climatic responses. They are objective in character. However, they …
Global sediment core-top calibration of the TEX86 paleothermometer in the ocean
JH Kim, S Schouten, EC Hopmans, B Donner… - … et Cosmochimica Acta, 2008 - Elsevier
The TEX86 (TetraEther indeX of tetraethers consisting of 86 carbon atoms)
paleothermometer is based on the relative distribution of archaeal lipids, ie isoprenoid …
paleothermometer is based on the relative distribution of archaeal lipids, ie isoprenoid …
Basalt‐seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: deconstructing Oceanic Anoxic Event 2 (Cenomanian–Turonian …
Abstract Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major
palaeoceanographic phenomenon that took place during an interval of extreme global …
palaeoceanographic phenomenon that took place during an interval of extreme global …