This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …

The glacial-interglacial transitions of ice ages are associated with large, rapid changes in
climate, which potentially can be reconstructed from stratigraphic profiles of the chemical …

The recurrence of the same types of sequence stratigraphic surface through geologic time
defines cycles of change in accommodation or sediment supply, which correspond to …

Sequence stratigraphy emphasizes facies relationships and stratal architecture within a
chronological framework. Despite its wide use, sequence stratigraphy has yet to be included …

Stratal stacking patterns provide the basis for the definition of all units and surfaces of
sequence stratigraphy. The same types of stacking patterns may be observed at different …

The late Paleozoic icehouse was the longest-lived ice age of the Phanerozoic, and its
demise constitutes the only recorded turnover to a greenhouse state. This review …

The late Paleozoic ice age (LPIA) consists of multiple glaciations that waxed and waned
across Gondwana during the Carboniferous and Permian. Three key intervals are evaluated …

The conventional view of the late Paleozoic ice age is that it was a single long, protracted
event some tens of millions of years in duration, with some internal waxing and waning of …

Twenty-eight new high-precision Chemical Abrasion Isotope Dilution Thermal Ionisation
Mass Spectrometry U-Pb zircon dates for tuffs in the Sydney and Bowen Basins are …

Stratigraphic cyclicity can be observed at different scales. At each scale of observation (ie,
hierarchical level), the building blocks of the sequence stratigraphic framework are …