[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 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 …
A 485-million-year history of Earth's surface temperature
A long-term record of global mean surface temperature (GMST) provides critical insight into
the dynamical limits of Earth's climate and the complex feedbacks between temperature and …
the dynamical limits of Earth's climate and the complex feedbacks between temperature and …
The cretaceous period
The breakup of the former Pangea supercontinent culminated in the modern drifting
continents. Increased rifting caused the establishment of the Atlantic Ocean in the middle …
continents. Increased rifting caused the establishment of the Atlantic Ocean in the middle …
Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate
Abstract The Early Eocene Climate Optimum (EECO, which occurred about 51 to 53 million
years ago), was the warmest interval of the past 65 million years, with mean annual surface …
years ago), was the warmest interval of the past 65 million years, with mean annual surface …
Ocean temperatures through the Phanerozoic reassessed
The oxygen isotope compositions of carbonate and phosphatic fossils hold the key to
understanding Earth-system evolution during the last 500 million years. Unfortunately, the …
understanding Earth-system evolution during the last 500 million years. Unfortunately, the …
[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 …
[HTML][HTML] The DeepMIP contribution to PMIP4: Methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data …
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 …
[كتاب][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 …
The magnitude and duration of Late Ordovician–Early Silurian glaciation
Understanding ancient climate changes is hampered by the inability to disentangle trends in
ocean temperature from trends in continental ice volume. We used carbonate “clumped” …
ocean temperature from trends in continental ice volume. We used carbonate “clumped” …