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 supercontinent Pangea completes its assembly and moves north during the Permian.
The 47-million-year-long period begins with a great ice age and ends with the Earth's …

Icehouses are the less common climate state on Earth, and thus it is notable that the longest-
lived (c. 370 to 260 Ma) and possibly most extensive and intense of icehouse periods …

Abstract In Europe, North Africa and Asia Minor, the remains of Pennsylvanian sedimentary
basins bearing continental deposits either intimately mixed with shallow-marine strata or …

Several existing schemes for Carboniferous stratigraphy officially adopted in regions of the
Russian Federation are summarized and discussed. These regions with different geological …

The expansion of land plants is considered to have played a key role in triggering the Late
Paleozoic Ice Age (LPIA), but evidence linking climatic events to terrestrial floral changes is …

During the Mississippian period, metazoan reefs and other marine faunas gradually
recovered from the Late Devonian mass extinctions and reached a peak in the late Visean …

This paper proposes a synthesis of the taxonomy, phylogeny, palaeogeographic distribution,
regional biostratigraphy, and palaeobiogeographic faunal development of Carboniferous …

For the biostratigraphy of mixed continental-marine and purely continental sections in the
palaeotropical belt of Euramerica, 9 insect and 8 conchostracan zones are newly defined or …

The increasing number and size of detrital geochronology data sets offer new opportunities
for increased accuracy and resolution of sediment routing models. However, the new …