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

A long-term record of global mean surface temperature (GMST) provides critical insight into
the dynamical limits of Earth's climate and the complex feedbacks between temperature and …

The spatial coverage and temporal resolution of the Early Paleozoic paleoclimate record are
limited, primarily due to the paucity of well-preserved skeletal material commonly used for …

The rise of animals occurred during an interval of Earth history that witnessed dynamic
marine redox conditions, potentially rapid plate motions, and uniquely large perturbations to …

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 …

Carbonate mud represents one of the most important geochemical archives for
reconstructing ancient climatic, environmental, and evolutionary change from the rock …

Abstract The Ediacaran Shuram carbon isotope excursion (CIE) follows the regional
Gaskiers glaciation and occurs before the appearance of macroscopic animal fossils …

Earth's persistent habitability since the Archean remains poorly understood. Using an
oxygen isotope ensemble approach—comprising shale, iron oxide, carbonate, silica, and …

Determining causal relationships between environmental change and early animal
evolution has been limited by our lack of a robust temporal framework for the Ediacaran …

Clumped isotope thermometry is an effective tool which allows to understand the post-
depositional alteration, including recrystallization and solid-state reordering, of carbonate …