[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 …
Flood basalts and mass extinctions
ME Clapham, PR Renne - Annual Review of Earth and …, 2019 - annualreviews.org
Flood basalts were Earth's largest volcanic episodes that, along with related intrusions, were
often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events …
often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events …
Synchronous tropical and polar temperature evolution in the Eocene
Palaeoclimate reconstructions of periods with warm climates and high atmospheric CO2
concentrations are crucial for developing better projections of future climate change. Deep …
concentrations are crucial for developing better projections of future climate change. Deep …
[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 …
Eocene greenhouse climate revealed by coupled clumped isotope-Mg/Ca thermometry
Past greenhouse periods with elevated atmospheric CO2 were characterized by globally
warmer sea-surface temperatures (SST). However, the extent to which the high latitudes …
warmer sea-surface temperatures (SST). However, the extent to which the high latitudes …
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 …
[HTML][HTML] Temperature dependency of metabolic rates in the upper ocean: A positive feedback to global climate change?
The temperature of seawater can affect marine plankton in various ways, including by
affecting rates of metabolic processes. This can change the way carbon and nutrients are …
affecting rates of metabolic processes. This can change the way carbon and nutrients are …
Ecological response of plankton to environmental change: thresholds for extinction
Severe climatic and environmental changes are far more prevalent in Earth history than
major extinction events, and the relationship between environmental change and extinction …
major extinction events, and the relationship between environmental change and extinction …
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 …