Mercury as a proxy for volcanic emissions in the geologic record
SE Grasby, TR Them II, Z Chen, R Yin… - Earth-Science …, 2019 - Elsevier
Large igneous province (LIP) eruptions are increasingly considered to have driven mass
extinction events throughout the Phanerozoic; however, uncertainties in radiometric age …
extinction events throughout the Phanerozoic; however, uncertainties in radiometric age …
Microbes, mud and methane: cause and consequence of recurrent E arly J urassic anoxia following the end‐T riassic mass extinction
The end‐T riassic mass extinction (c. 201.6 Ma) was one of the five largest mass‐extinction
events in the history of animal life. It was also associated with a dramatic, long‐lasting …
events in the history of animal life. It was also associated with a dramatic, long‐lasting …
Large igneous provinces and mass extinctions: an update
DPG Bond, PB Wignall, G Keller… - Volcanism, impacts, and …, 2014 - books.google.com
The temporal link between mass extinctions and large igneous provinces is well known.
Here, we examine this link by focusing on the potential climatic effects of large igneous …
Here, we examine this link by focusing on the potential climatic effects of large igneous …
Cryosphere carbon dynamics control early Toarcian global warming and sea level evolution
The Earth's cryosphere represents a huge climate-sensitive carbon reservoir capable of
releasing carbon dioxide (CO 2) and methane (CH 4) from permafrost soils or gas reservoirs …
releasing carbon dioxide (CO 2) and methane (CH 4) from permafrost soils or gas reservoirs …
Secular environmental precursors to Early Toarcian (Jurassic) extreme climate changes
The Early Toarcian Oceanic Anoxic Event (T-OAE), about 183myr ago, was a global event of
environmental and carbon cycle perturbations, which deeply affected both marine biota and …
environmental and carbon cycle perturbations, which deeply affected both marine biota and …
How contact metamorphism can trigger global climate changes: Modeling gas generation around igneous sills in sedimentary basins
I Aarnes, H Svensen, JAD Connolly… - … et Cosmochimica Acta, 2010 - Elsevier
Large volumes of greenhouse gases such as CH4 and CO2 form by contact metamorphism
of organic-rich sediments in aureoles around sill intrusions in sedimentary basins …
of organic-rich sediments in aureoles around sill intrusions in sedimentary basins …
δ13C of terrestrial vegetation records Toarcian CO2 and climate gradients
Throughout Earth's history, variations in atmospheric CO2 concentration modulated climate.
Understanding changes in atmospheric carbon cycle is therefore pivotal in predicting …
Understanding changes in atmospheric carbon cycle is therefore pivotal in predicting …
A carbon-isotope perturbation at the Pliensbachian–Toarcian boundary: evidence from the Lias Group, NE England
A perturbation in the carbon-isotope record at the time of the Pliensbachian–Toarcian
boundary (~ 184 Ma) in the Early Jurassic is reported, based on new data from Yorkshire …
boundary (~ 184 Ma) in the Early Jurassic is reported, based on new data from Yorkshire …
Polar record of Early Jurassic massive carbon injection
The Toarcian Oceanic Anoxic Event (T-OAE)(ca. 182Myr, Early Jurassic) represents one of
the best-recognized examples of greenhouse warming, decreased seawater oxygenation …
the best-recognized examples of greenhouse warming, decreased seawater oxygenation …
Emplacement characteristics, time scales, and volcanic gas release rates of continental flood basalt eruptions on Earth
Continental flood basalt provinces are the subaerial expression of large igneous province
volcanism. The emplacement of a continental flood basalt is an exceptional volcanic event in …
volcanism. The emplacement of a continental flood basalt is an exceptional volcanic event in …