End-Permian mass extinction in the oceans: an ancient analog for the twenty-first century?
JL Payne, ME Clapham - Annual Review of Earth and Planetary …, 2012 - annualreviews.org
The greatest loss of biodiversity in the history of animal life occurred at the end of the
Permian Period (∼ 252 million years ago). This biotic catastrophe coincided with an interval …
Permian Period (∼ 252 million years ago). This biotic catastrophe coincided with an interval …
The Smithian/Spathian boundary (late Early Triassic): A review of ammonoid, conodont, and carbon-isotopic criteria
The transition from the Smithian substage to the Spathian substage of the Olenekian stage
of the late Early Triassic was a critical time marked by a series of biological and …
of the late Early Triassic was a critical time marked by a series of biological and …
The triassic period
The Triassic is bound by two mass extinctions that coincide with vast outpourings of volcanic
flood basalts. The Mesozoic begins with a gradual recovery of plant and animal life after the …
flood basalts. The Mesozoic begins with a gradual recovery of plant and animal life after the …
An evaporite-based high-resolution sulfur isotope record of Late Permian and Triassic seawater sulfate
Variations in the sulfur isotope composition of dissolved marine sulfate through time reflect
changes in the global sulfur cycle and are intimately related to changes in the carbon and …
changes in the global sulfur cycle and are intimately related to changes in the carbon and …
Variability in sulfur isotope records of Phanerozoic seawater sulfate
TM Present, JF Adkins… - Geophysical Research …, 2020 - Wiley Online Library
The δ34S of seawater sulfate reflects processes operating at the nexus of sulfur, carbon, and
oxygen cycles. However, knowledge of past seawater sulfate δ34S values must be derived …
oxygen cycles. However, knowledge of past seawater sulfate δ34S values must be derived …
Subsequent biotic crises delayed marine recovery following the late Permian mass extinction event in northern Italy
The late Permian mass extinction event was the largest biotic crisis of the Phanerozoic and
has the longest recovery interval of any extinction event. It has been hypothesised that …
has the longest recovery interval of any extinction event. It has been hypothesised that …
Marine sulfur cycle evidence for upwelling and eutrophic stresses during Early Triassic cooling events
A Stebbins, TJ Algeo, L Krystyn, H Rowe… - Earth-Science …, 2019 - Elsevier
Perturbations to the global carbon and sulfur cycles recurred episodically throughout the~ 5-
Myr-long Early Triassic, in the aftermath of the end-Permian mass extinction, the largest …
Myr-long Early Triassic, in the aftermath of the end-Permian mass extinction, the largest …
[HTML][HTML] Environmental controls on the post-Permian recovery of benthic, tropical marine ecosystems in western Palaeotethys (Aggtelek Karst, Hungary)
Climate warming during the late Permian is associated with the most severe mass extinction
event of the Phanerozoic, and the expansion of hypoxic and anoxic conditions in shallow …
event of the Phanerozoic, and the expansion of hypoxic and anoxic conditions in shallow …
A transient oxygen increase in the Mesoproterozoic ocean at∼ 1.44 Ga: Geochemical evidence from the Tieling Formation, North China Platform
Y Yu, Y Chen, D Li, J Su - Precambrian Research, 2022 - Elsevier
Oxygen availability is crucial for the evolution of eukaryotes in geological history, yet
detailed Mesoproterozoic oceanic-atmospheric redox conditions remain enigmatic. In …
detailed Mesoproterozoic oceanic-atmospheric redox conditions remain enigmatic. In …
Global-ocean circulation changes during the Smithian–Spathian transition inferred from carbon‑sulfur cycle records
Early Triassic marine ecosystems experienced multiple environmental perturbations and a
delayed biotic recovery following the end-Permian mass extinction. The Smithian–Spathian …
delayed biotic recovery following the end-Permian mass extinction. The Smithian–Spathian …