Surface temperature is a fundamental parameter of Earth's climate. Its evolution through time
is commonly reconstructed using the oxygen isotope and the clumped isotope compositions …

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 application of carbonate clumped isotope (Δ 47) thermometry in deep-time is often
limited by modification of the original temperature signal by thermal resetting. New modeling …

Reconstructing temperatures of ancient oceans is important for understanding Earth's
climate in deep time. Belemnites have been used widely to estimate Mesozoic seawater …

The cephalopod arm armature is certainly one of the most important morphological
innovations responsible for the evolutionary success of the Cephalopoda. New …

Fossils from the Jurassic succession of the Neuquén Basin (Argentina) were analysed for
their stable isotope (δ13C, δ18O) and elemental (Mg/Ca, Sr/Ca) composition. Mg/Ca ratios …

Clumped isotope based temperature estimates from exceptionally well-preserved
belemnites from Staffin Bay (Isle of Skye, Scotland) reveal that seawater temperatures …

Late Cretaceous sea surface temperatures (SST) are, amongst others, traditionally
reconstructed by compiling oxygen isotope records of planktonic foraminifera obtained from …

The purpose of this work is to test the ability of laser ablation inductively coupled plasma
mass spectrometry (LA-ICPMS) to provide absolute ages of useful precision on calcitic …

Assessing the climatic perturbations during the Cretaceous when atmospheric CO 2 levels
were high is critical for understanding the nature of environmental responses to greenhouse …