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 …
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 …
The Permian marine-terrestrial system of the North China block provides an exceptional window into the evolution of northern temperate ecosystems during the critical transition …
Atmospheric CO2 is thought to play a fundamental role in Earth's climate regulation. Yet, for much of Earth's geological past, atmospheric CO2 has been poorly constrained, hindering …
Paleotemperature proxy data form the cornerstone of paleoclimate research and are integral to understanding the evolution of the Earth system across the Phanerozoic Eon. Here, we …
Abstract The Carboniferous-Permian strata in the North China Block (NCB) contain abundant fossils, coals and natural gases. Establishing a high-resolution timescale for the …
W Wang, C Garbelli, F Zhang, Q Zheng, Y Zhang… - Earth and Planetary …, 2020 - Elsevier
Climatic warming has been widely cited as a driver for many mass extinction events in Earth history, including the middle-late Permian Guadalupian-Lopingian boundary (GLB) mass …
Y Li, L Shao, CR Fielding, TD Frank, D Wang… - Global and Planetary …, 2023 - Elsevier
Abstract Comparison of chemical index of alteration (CIA) values and estimated land surface temperatures (LSTs) from upper Carboniferous-Permian successions in low paleolatitude …
Abstract The Guadalupian Epoch is marked by the formation of the Pangean supercontinent, global sea-level change, rifting and drifting of the Cimmerian continents, formation of large …