Since 65 million years ago (Ma), Earth's climate has undergone a significant and complex
evolution, the finer details of which are now coming to light through investigations of deep …

Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

Abstract The Palaeocene–Eocene Thermal Maximum 1, 2 (PETM) was a global warming
event that occurred about 56 million years ago, and is commonly thought to have been …

The nine editions of Stable Isotope Geochemistry have appeared over a time span of nearly
50 years. The first edition (1973) appeared as a slim book of 135 pages. Due to the rapid …

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 …

The Paleocene-Eocene thermal maximum (PETM) has been attributed to the rapid release
of∼ 2000× 109 metric tons of carbon in the form of methane. In theory, oxidation and ocean …

On-line analysis of split sediment cores by XRF core scanners has become increasingly
popular in the past decade, because it allows nondestructive extraction of near-continuous …

XRF core scanners, with their rapid and non-destructive analytical capability, have now
been used for two decades in the analysis of marine sediments. Initially they were used to …

The Paleocene-Eocene Thermal Maximum (PETM) has been attributed to a rapid rise in
greenhouse gas levels. If so, warming should have occurred at all latitudes, although …

Abstract The Palaeocene/Eocene thermal maximum,∼ 55 million years ago, was a brief
period of widespread, extreme climatic warming,,, that was associated with massive …