Astronomical insolation forcing is well established as the underlying metronome of
Quaternary ice ages and Cenozoic climate changes. Yet its effects on earlier eras …

Milankovitch cycles are quasi-periodic fluctuations in insolation forced by the variation in
Earth's astronomical parameters. The astronomically induced climate change affected the …

The end-Ordovician was an enigmatic interval in the Phanerozoic, known for massive
glaciation potentially at elevated CO2 levels, biogeochemical cycle disruptions recorded as …

A high‐resolution stratigraphy is essential toward deciphering climate variability in detail
and understanding causality arguments of events in earth history. Because the middle to late …

The early Eocene climatic optimum was a period of major climatic and environmental
change that was caused by perturbations to the global carbon cycle. Recent work from …

Here we present a high-resolution cyclostratigraphy based on X-ray fluorescence (XRF)
core scanning data from a new record retrieved from the tropical western Atlantic (Demerara …

Facies indicators and geochemical proxies of early Palaeozoic global climate cooling
suggest episodes of fluctuating glacio-eustasy and severe cold or glaciation from the Mid …

Falling atmospheric CO2 levels led to cooling through the Eocene and the expansion of
Antarctic ice sheets close to their modern size near the beginning of the Oligocene, a period …

Abstract The Last Interglacial (LIG) represents an invaluable case study to investigate the
response of components of the Earth system to global warming. However, the scarcity of …

Astronomical cycles are strongly expressed in marine geological records, providing
important insights into Earth system dynamics and an invaluable means of constructing age …