Reduction–oxidation (redox) reactions occur during burial because sediments contain
reactive mixtures of oxidised and reduced components. Diagenetic chemical reactions …

New values for the astronomical parameters of the Earth's orbit and rotation (eccentricity,
obliquity and precession) are proposed for paleoclimatic research related to the Late …

Circumbinary planets, those that orbit around both stars of a central binary star system,
challenge our understanding of planet formation. With only 12 binary systems known to host …

Research on global ice-volume changes during Pleistocene glacial cycles is hindered by a
lack of detailed sea-level records for time intervals older than the last interglacial. Here we …

We present here a new solution for the astronomical computation of the orbital motion of the
Earth spanning from 0 to− 250 Myr. The main improvement with respect to our previous …

Context. Searching for planets around stars with different masses helps us to assess the
outcome of planetary formation for different initial conditions. The low-mass M dwarfs are …

Astronomical calculations reveal the Solar System's dynamical evolution, including its
chaoticity, and represent the backbone of cyclostratigraphy and astrochronology. An …

We present here a new solution for the astronomical computation of the insolation quantities
on Earth spanning from-250 Myr to 250 Myr. This solution has been improved with respect to …

Astronomical forcing of Earth's climate is embedded in the rhythms of stratigraphic records,
most famously as short-period (104–105 year) Milankovitch cycles. Astronomical grand …

Over the past 25 yr, the science of stratigraphy has evolved to include time-correlative data
from vastly disparate components of the Earth system. Not least of these is the global signal …