Extracting the most from terrestrial plant-derived n-alkyl lipids and their carbon isotopes from the sedimentary record: A review
AF Diefendorf, EJ Freimuth - Organic Geochemistry, 2017 - Elsevier
Terrestrial plant biomarkers and their carbon isotopes provide insights into carbon cycling,
paleovegetation and paleoclimate, ranging in scale from local to global. Over the past …
paleovegetation and paleoclimate, ranging in scale from local to global. Over the past …
[HTML][HTML] Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
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 …
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …
[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 …
Simulation of Eocene extreme warmth and high climate sensitivity through cloud feedbacks
The Early Eocene, a period of elevated atmospheric CO2 (> 1000 ppmv), is considered an
analog for future climate. Previous modeling attempts have been unable to reproduce major …
analog for future climate. Previous modeling attempts have been unable to reproduce major …
Paleocene/Eocene carbon feedbacks triggered by volcanic activity
Abstract The Paleocene–Eocene Thermal Maximum (PETM) was a period of geologically-
rapid carbon release and global warming~ 56 million years ago. Although modelling …
rapid carbon release and global warming~ 56 million years ago. Although modelling …
Extreme warmth and heat-stressed plankton in the tropics during the Paleocene-Eocene Thermal Maximum
Global ocean temperatures rapidly warmed by~ 5° C during the Paleocene-Eocene Thermal
Maximum (PETM;~ 56 million years ago). Extratropical sea surface temperatures (SSTs) met …
Maximum (PETM;~ 56 million years ago). Extratropical sea surface temperatures (SSTs) met …
Confounding effects of oxygen and temperature on the TEX86 signature of marine Thaumarchaeota
W Qin, LT Carlson, EV Armbrust… - Proceedings of the …, 2015 - National Acad Sciences
Marine ammonia-oxidizing archaea (AOA) are among the most abundant of marine
microorganisms, spanning nearly the entire water column of diverse oceanic provinces …
microorganisms, spanning nearly the entire water column of diverse oceanic provinces …
Mercury anomalies across the Palaeocene–Eocene thermal maximum
Large-scale magmatic events like the emplacement of the North Atlantic Igneous Province
(NAIP) are often coincident with periods of extreme climate change such as the Palaeocene …
(NAIP) are often coincident with periods of extreme climate change such as the Palaeocene …
An early Cambrian greenhouse climate
The oceans of the early Cambrian (~ 541 to 509 million years ago) were the setting for a
marked diversification of animal life. However, sea temperatures—a key component of the …
marked diversification of animal life. However, sea temperatures—a key component of the …
The PhanSST global database of Phanerozoic sea surface temperature proxy data
Paleotemperature proxy data form the cornerstone of paleoclimate research and are integral
to understanding the evolution of the Earth system across the Phanerozoic Eon. Here, we …
to understanding the evolution of the Earth system across the Phanerozoic Eon. Here, we …