From the latest Cretaceous (late Campanian to Maastrichtian,~ 75–66 Ma) to the earliest
Paleogene, fluctuations in greenhouse climate, inferred primarily from marine sediments …

Stable isotope paleoaltimetry makes use of systematic trends in the distribution and isotopic
composition of modern precipitation with climate and topography, and of the potential to …

Stable oxygen isotope ratios (δ18O) of Precambrian cherts have been used to establish
much of our understanding of the early climate history of Earth,, and suggest that ocean …

We seek to better understand growth of the Tibetan plateau and associated climate change
by presenting the first regionally extensive set of oxygen isotope data obtained from ca. 40 …

Meteoric water convection has long been recognized as an efficient means to cool magmatic
intrusions in the Earth's upper crust. This interplay between magmatic and hydrothermal …

The silicification of carbonate rocks is a diagenetic process that involves the major
replacement of carbonate minerals by silica minerals (opaline phases, quartz and …

The surface uplift of mountain belts caused by tectonism plays an important role in
determining the long-term climate evolution of the Earth. However, the general lack of …

The advent of continuous-flow isotope-ratio mass spectrometry (CF-IRMS) coupled with a
high temperature conversion (HTC) system enabled faster, more cost effective, and more …

Triple oxygen isotope measurements are an emerging tool in paleoclimate reconstructions.
In this contribution we develop the application of triple oxygen isotope measurements to …

The oxygen-18 isotopic composition (δ 18 O) of silica preserved in oceanic sediments is an
important archive of Earth's temperature and/or seawater δ 18 O from the Archean to …