Environmental crises at the Permian–Triassic mass extinction
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 …
emplacement of the Siberian Traps Large Igneous Province (STLIP) was first proposed in …
The Permian chert event in South China: new geochemical constraints and global implications
B Zhang, J Cao, L Mu, S Yao, W Hu, H Huang… - Earth-Science …, 2023 - Elsevier
Abstract The Permian Chert Event (PCE) was an unusual global chert accumulation that
reflects tectonic–climatic–environmental changes during the late Paleozoic. South China …
reflects tectonic–climatic–environmental changes during the late Paleozoic. South China …
Recovery from persistent nutrient-N limitation following the Permian–Triassic mass extinction
Global warming, widespread oceanic anoxia and stagnation, and large perturbations of the
global carbon cycle characterized the end-Permian to Middle Triassic interval. Nitrogen …
global carbon cycle characterized the end-Permian to Middle Triassic interval. Nitrogen …
Recovery of lacustrine ecosystems after the end-Permian mass extinction
The end-Permian mass extinction (EPME; ca. 252 Ma) led to profound changes in lacustrine
ecosystems. However, whether or not post-extinction recovery of lacustrine ecosystems was …
ecosystems. However, whether or not post-extinction recovery of lacustrine ecosystems was …
[HTML][HTML] Continental records of organic carbon isotopic composition (δ13Corg), weathering, paleoclimate and wildfire linked to the End-Permian Mass Extinction
J Lu, P Zhang, M Yang, L Shao, J Hilton - Chemical Geology, 2020 - Elsevier
The late Permian was the acme of Pangea assembly, with collision and subduction of global
plates accompanied by major changes in atmospheric composition, paleoclimates and …
plates accompanied by major changes in atmospheric composition, paleoclimates and …
Palaeoenvironmental variability and carbon cycle perturbations during the Smithian-Spathian (Early Triassic) in Central Spitsbergen
FR Blattmann, E Schneebeli-Hermann, T Adatte… - Lethaia, 2024 - idunn.no
The Early Triassic Smithian and Spathian time intervals are characterized by perturbations
in the global carbon cycle, fluctuations in sea surface temperature, high turnover rates of …
in the global carbon cycle, fluctuations in sea surface temperature, high turnover rates of …
Integrated bio-chemostratigraphy of Lower and Middle Triassic marine successions at Spiti in the Indian Himalaya: Implications for the Early Triassic nutrient crisis
In this paper we study the Lilang Super Group in the Spiti area, Indian Himalaya to
understand environmental changes in the aftermath of the end-Permian mass extinction. We …
understand environmental changes in the aftermath of the end-Permian mass extinction. We …
Occurrence and preservation of primary organic matter in a hybrid unconventional reservoir: Montney Formation, Western Canada Sedimentary Basin
Abstract The Lower Triassic Montney Formation of the Western Canada Sedimentary Basin
(WCSB) is a world-class unconventional hydrocarbon resource in North America. It was …
(WCSB) is a world-class unconventional hydrocarbon resource in North America. It was …
Linking sediment supply variations and tectonic evolution in deep time, source-to-sink systems—The Triassic Greater Barents Sea Basin
Triassic strata in the Greater Barents Sea Basin are important records of geodynamic activity
in the surrounding catchments and sediment transport in the Arctic basins. This study is the …
in the surrounding catchments and sediment transport in the Arctic basins. This study is the …
The great catastrophe: causes of the Permo-Triassic marine mass extinction
PB Wignall, DPG Bond - National Science Review, 2024 - academic.oup.com
The marine losses during the Permo-Triassic mass extinction were the worst ever
experienced. All groups were badly affected, especially amongst the benthos (eg …
experienced. All groups were badly affected, especially amongst the benthos (eg …