The link between the Permian–Triassic mass extinction (252 million years ago) and the
emplacement of the Siberian Traps Large Igneous Province (STLIP) was first proposed in …

Woese and Fox's 1977 paper on the discovery of the Archaea triggered a revolution in the
field of evolutionary biology by showing that life was divided into not only prokaryotes and …

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 …

Theory regarding the causation of mass extinctions is in need of systematization, which is
the focus of this contribution. Every mass extinction has both an ultimate cause, ie the trigger …

INTRODUCTION Climate change triggered by volcanic greenhouse gases is hypothesized
to have caused the largest mass extinction in Earth's history at the end of the Permian Period …

The aftermath of the great end-Permian period mass extinction 252 Myr ago shows how life
can recover from the loss of> 90% species globally. The crisis was triggered by a number of …

Changes in oceanic primary production, linked to changes in the network of global
biogeochemical cycles, have profoundly influenced the geochemistry of Earth for over 3 …

Negative carbon isotope anomalies in carbonate rocks bracketing Neoproterozoic glacial
deposits in Namibia, combined with estimates of thermal subsidence history, suggest that …

The community structure and ecological function of contemporary marine ecosystems are
critically dependent on eukaryotic phytoplankton. Although numerically inferior to …

An Introduction to Organic Geochemistry explores the fate of organic matter of all types,
biogenic and man-made, in the Earth System. investigates the variety of pathways and …