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 …

Paleosols are ancient soils that have been incorporated into the geological record. Soils
form in response to interactions among the lithosphere, hydrosphere, biosphere, and …

Abstract The Late Paleozoic (Early Devonian to Middle Permian) was an interval of profound
changes in Earth-surface systems, reflected in dynamic interplay among the biosphere …

Paleosols preserved within the Carboniferous–Permian succession of the Lodève Basin,
Massif Central, France change stratigraphically from Histosols to calcic Vertisols and …

We evaluate the influences of elevation and climate on the spatio-temporal distribution of
wetland and dryland biomes during the Pennsylvanian and early Permian in tropical …

Phytoplankton form the base of most marine trophic chains and studying their past diversity
at regional and global scales can provide valuable insights into the evolution of marine …

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

Forty-seven rock samples from the stratotypes of three upper Paleogene formations–
Prussian, Palvé, and Kurshskaya formations–were collected from the biggest amber deposit …

Volcanism was intense in western European basins during the Late Carboniferous–Early
Permian transition, related to the late Variscan extension and associated magmatism. In the …

Although continental weathering intensity has been invoked as a primary control on
biogeochemistry, tectonics, and the carbon cycle throughout geologic history, it remains …