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

Cyclostratigraphy is an important tool for understanding astronomical climate forcing and
reading geological time in sedimentary sequences, provided that an imprint of insolation …

This paper addresses two fundamental issues in cyclostratigraphy and paleoclimatology:
identification of astronomical forcing in sequences of stratigraphic cycles, and accurate …

Earth's climate system is complex and inherently nonlinear, which can induce some
extraneous cycles in paleoclimatic proxies at orbital time scales. The paleoenvironmental …

The linkages between the astronomical forcing of sea-level oscillations, the environment,
and climate change during the Late Paleozoic Ice Age (LPIA) add to our understanding of …

After more than a century of doubt and equivocation, cyclostratigraphy–the stratigraphic
record of astronomically forced paleoclimatic change–has come to be widely accepted in the …

Cyclic sedimentation has varied at several timescales and this variability has been
geologically well documented at Milankovitch timescales, controlled in part by climatically …

Periodicity is a fundamental phenomenon occurring throughout the history of our planet
Earth. Investigations into the mechanics of terrestrial cyclicity should consider short-term …

Astronomical forcing associated with Earth's orbital and inclination exerts a major control on
climate as recorded in the sedimentary rocks. Alkaline lake deposits in the second member …

The sediments deposited in continental lake systems record sensitive palaeoclimate signals
and provide better perspectives for understanding rapid palaeoclimate changes and their …