The link between the Permian–Triassic mass extinction (252 million years ago) and the emplacement of the Siberian Traps Large Igneous Province (STLIP) was first proposed in …
The Siberian Traps large igneous province (STLIP) is commonly invoked as the primary driver of global environmental changes that triggered the end-Permian mass extinction …
A timeframe of glacial and nonglacial intervals in the Carboniferous and Permian systems of eastern Australia was published by Fielding et al.(2008a). In this scheme, eight discrete …
An oxygen-rich atmosphere is essential for complex animals. The early Earth had an anoxic atmosphere, and understanding the rise and maintenance of high O2 levels is critical for …
The latest Permian mass extinction (LPME) was triggered by magmatism of the Siberian Traps Large Igneous Province (STLIP), which left an extensive record of sedimentary Hg …
Current large-scale deforestation poses a threat to ecosystems globally, and imposes substantial and prolonged changes on the hydrological and carbon cycles. The tropical …
Abstract The Permian–Triassic mass extinction was marked by a massive release of carbon into the ocean-atmosphere system, evidenced by a sharp negative carbon isotope …
Earth's largest biotic crisis occurred during the Permo–Triassic Transition (PTT). On land, this event witnessed a turnover from synapsid-to archosauromorph-dominated assemblages …
Ikaite is a metastable calcium carbonate hexahydrate (CaCO3· 6H2O), which naturally occurs in environments characterized by temperatures of− 2 to+ 7° C. It is therefore …