Mercury enrichments provide evidence of Early Triassic volcanism following the end-Permian mass extinction
Oceanic environments and biotas were in a state of near-continuous perturbation during the
Early Triassic, the~ 5-million-year interval following the latest Permian mass extinction …
Early Triassic, the~ 5-million-year interval following the latest Permian mass extinction …
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 …
Marine anoxia and delayed Earth system recovery after the end-Permian extinction
Delayed Earth system recovery following the end-Permian mass extinction is often attributed
to severe ocean anoxia. However, the extent and duration of Early Triassic anoxia remains …
to severe ocean anoxia. However, the extent and duration of Early Triassic anoxia remains …
Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction
Explaining the~ 5-million-year delay in marine biotic recovery following the latest Permian
mass extinction, the largest biotic crisis of the Phanerozoic, is a fundamental challenge for …
mass extinction, the largest biotic crisis of the Phanerozoic, is a fundamental challenge for …
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 …
Persistent late Permian to Early Triassic warmth linked to enhanced reverse weathering
In the Precambrian, reverse weathering—a process consuming oceanic silica, metal cations
and alkalinity to form marine clays—was a key control of the long-term carbon cycle …
and alkalinity to form marine clays—was a key control of the long-term carbon cycle …
Integrated Sr isotope variations and global environmental changes through the Late Permian to early Late Triassic
Abstract New 87 Sr/86 Sr data based on 127 well-preserved and well-dated conodont
samples from South China were measured using a new technique (LA-MC-ICPMS) based …
samples from South China were measured using a new technique (LA-MC-ICPMS) based …
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 …
Two distinct episodes of marine anoxia during the Permian-Triassic crisis evidenced by uranium isotopes in marine dolostones
The end-Permian mass extinction (EPME; ca. 251.94 Ma) is the most severe mass extinction
in the geological record. Detailed paleobiological investigations show a very rapid EPME …
in the geological record. Detailed paleobiological investigations show a very rapid EPME …
Strontium isotope (87Sr/86Sr) stratigraphy of Ordovician bulk carbonate: Implications for preservation of primary seawater values
The present study on bulk carbonate 87Sr/86Sr stratigraphy represents a companion work to
earlier research that presented a conodont apatite-based Ordovician seawater 87Sr/86Sr …
earlier research that presented a conodont apatite-based Ordovician seawater 87Sr/86Sr …