Abstract The 'COPSE'(Carbon, Oxygen, Phosphorus, Sulphur and Evolution)
biogeochemical model predicts the coupled histories and controls on atmospheric O 2, CO 2 …

The temperature of ancient oceans is an important constraint for understanding the climate
history of our planet. The classical oxygen isotope paleothermometry on fossil shells, while …

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 …

The long-term diversification of the biosphere responds to changes in the physical
environment. Yet, over the continents, the nearly monotonic expansion of life started later in …

Global mean sea level is a key component within the fields of climate and oceanographic
modelling in the Anthropocene. Hence, an improved understanding of eustatic sea level in …

Traditional stable isotope geochemistry involves isotopes of light elements such as H, C, N,
O, and S, which are measured predominantly by gas-source mass spectrometry (Valley et al …

In the Precambrian, reverse weathering—a process consuming oceanic silica, metal cations
and alkalinity to form marine clays—was a key control of the long-term carbon cycle …

Abstract The Permian/Triassic boundary approximately 251.9 million years ago marked the
most severe environmental crisis identified in the geological record, which dictated the …

Calcium carbonate formation is the primary pathway by which carbon is returned from the
ocean–atmosphere system to the solid Earth,. The removal of dissolved inorganic carbon …

Groundwater-derived solute fluxes to the ocean have long been assumed static and
subordinate to riverine fluxes, if not neglected entirely, in marine isotope budgets. Here we …