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 …

Silicate weathering is critical to global carbon cycle and climate change, and has attracted
considerable attention in Earth science studies. Chemical weathering intensity evaluation …

The end-Permian mass extinction was the most severe ecological event during the
Phanerozoic and has long been presumed contemporaneous across terrestrial and marine …

Although the prime causation of the Late Devonian Frasnian–Famennian (F–F) mass
extinction remains conjectural, such destructive factors as the spread of anoxia and rapid …

A synthesis of Cenozoic detrital suites from the Internal Betic-Rif Cordilleras is discussed in
relations with major paleotectonic phases during growth of orogenic belts. The discussion …

Weathering profiles of granitoid rocks from the Sila Massif (southern Italy) have been studied
to characterize weathering processes that affect this area. Chemical weathering indices of …

The collapse of late Permian (Lo**ian) Gondwanan floras, characterized by the extinction
of glossopterid gymnosperms, heralded the end of one of the most enduring and extensive …

Organic matter enrichment in lacustrine shale is significantly influenced by paleoclimate and
paleoenvironment. In this study, a total of 24 shale samples were vertically collected from the …

Rapid climate change was a major contributor to the end-Permian extinction (EPE).
Although well constrained for the marine realm, relatively few records document the pace …

Abstract Many Middle-Late Triassic (Ladinian-Carnian) global and local humid climate
events that impacted on global palaeontological evolution and mineral distribution have …