This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …

Ocean acidification is rapidly changing the carbonate system of the world oceans. Past mass
extinction events have been linked to ocean acidification, and the current rate of change in …

The temporal link between large igneous province (LIP) eruptions and at least half of the
major extinctions of the Phanerozoic implies that large scale volcanism is the main driver of …

Abstract Large Igneous Provinces (LIPs) can have a significant global climatic effect as
monitored by sedimentary trace and isotopic compositions that record paleo …

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 …

Most carbon dioxide released into the atmosphere as a result of the burning of fossil fuels
will eventually be absorbed by the ocean, with potentially adverse consequences for marine …

Variations in the 13C/12C value of total dissolved inorganic carbon (DIC) in the world's
oceans through time have been documented through stratigraphic study of marine …

The Central Atlantic Magmatic Province (CAMP) has long been proposed as having a
causal relationship with the end-Triassic extinction event (∼ 201.5 Ma). In North America …

The term" carbon cycle" is normally thought to mean those processes that govern the
present-day transfer of carbon between life, the atmosphere, and the oceans. This book …

New high-precision U/Pb geochronology from volcanic ashes shows that the Triassic-
Jurassic boundary and end-Triassic biological crisis from two independent marine …