D Sachse, I Billault, GJ Bowen… - Annual Review of …, 2012 - annualreviews.org
Hydrogen-isotopic abundances of lipid biomarkers are emerging as important proxies in the study of ancient environments and ecosystems. A decade ago, pioneering studies made use …
The Paleocene–Eocene Thermal Maximum (PETM; 56 Ma) is one of our best geological analogs for understanding climate dynamics in a “greenhouse” world. However, proxy data …
FA McInerney, SL Wing - Annual Review of Earth and Planetary …, 2011 - annualreviews.org
During the Paleocene-Eocene Thermal Maximum (PETM),∼ 56 Mya, thousands of petagrams of carbon were released into the ocean-atmosphere system with attendant …
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 …
Abstract The Palaeocene/Eocene thermal maximum,∼ 55 million years ago, was a brief period of widespread, extreme climatic warming,,, that was associated with massive …
Leaf waxes (ie, n-alkyl lipids or n-alkanes) are land-plant biomarkers widely used to reconstruct changes in climate and the carbon isotopic composition of the atmosphere …
The Toarcian Oceanic Anoxic Event (OAE) in the Early Jurassic (∼ 183 Ma ago) was characterized by widespread near-synchronous deposition of organic-rich shales in marine …
Seawater lithium isotopes (δ7Li) record changes over Earth history, including a∼ 9‰ increase during the Cenozoic interpreted as reflecting either a change in continental silicate …
MJ Carmichael, GN Inglis, MPS Badger… - Global and Planetary …, 2017 - Elsevier
Abstract The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal,~ 56 million years ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …