The late Paleozoic ice age (LPIA) during the Carboniferous and Permian (ca. 360–260 Ma) was vegetated Earth's only recorded icehouse-to-greenhouse transition provides a deep-time perspective for climate-glaciation-environment coevolution future climate change. During LPIA, changes in glacial-interglacial cycles have been closely linked to atmospheric pCO2. In this paper, we investigate relation...

Most of the research on Paleoentomology focuses describing morphology and classification one species fossil insects. However, there is little information temporal diversity insects during Permian Triassic periods. The end-Permian mass extinction (EPME) was greatest biological ecological crisis Phanerozoic Eon Earth, while pattern recovery terrestrial ecosystem still unclear. In this paper, popu...

New U–Pb detrital zircon and ages of metaigneous rocks in the Águilas Arc (Betic Chain, SE Spain) allow us to determine maximum depositional rocks. Within Nevado-Filábride Complex, a Late Carboniferous age for Lomo de Bas schists quartzites, Permian-Triassic Tahal Fm are determined. Alpujárride Micaschists Quartzite is Meta-detrital was deposited Early Permian. Furthermore, Saladilla Maláguide ...

This paper presents structural evidence of extensional activity in Central Alborz during Mesozoic. The structural evidence of homogenous early stage stretching such as layer-parallel to oblique boudinage of Permian and Triassic rocks in various portions of the study area accompanied by extensional-fibrous fractures were followed with more advanced extensional features. These extensional structu...

The Permian-Triassic alluvial rift succession in the Horda Platform area is analysed to construct a refined depositional model. study demonstrates how subsurface continental successions may be stratigraphically subdivided and correlated by integrating seismic well-log data concert with conceptual models. Regional unconformities mark top base of succession, which sub-divided into six stratigraph...

1 late Permian mass extinction event in northern Italy. ABSTRACT 10 The late Permian mass extinction event was the largest biotic crisis of the Phanerozoic and has 11 the longest recovery interval of any extinction event. It has been hypothesised that subsequent 12 carbon isotope perturbations during the Early Triassic are associated with biotic crises that 13 impeded benthic recovery. We test ...