The Late Triassic Extinction at the Norian/Rhaetian boundary: Biotic evidence and geochemical signature
The latest Triassic was an interval of prolonged biotic extinction culminating in the end-
Triassic Extinction (ETE). The ETE is now associated with a perturbation of the global carbon …
Triassic Extinction (ETE). The ETE is now associated with a perturbation of the global carbon …
Earth's impact events through geologic time: a list of recommended ages for terrestrial impact structures and deposits
M Schmieder, DA Kring - Astrobiology, 2020 - liebertpub.com
This article presents a current (as of September 2019) list of recommended ages for proven
terrestrial impact structures (n= 200) and deposits (n= 46) sourced from the primary …
terrestrial impact structures (n= 200) and deposits (n= 46) sourced from the primary …
Pseudosuchian thermometabolism: A review of the past two decades
MG Faure‐Brac - The Anatomical Record, 2025 - Wiley Online Library
Pseudosuchia, one of the two main clades of Archosauria, is today only represented by
some 20 extant species, the crocodilians, representing only a fraction of its extinct diversity …
some 20 extant species, the crocodilians, representing only a fraction of its extinct diversity …
The Triassic–Jurassic transition–A review of environmental change at the dawn of modern life
Abstract The Triassic–Jurassic transition, which is here broadly defined as extending from
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
Application of the 187Re-187Os geochronometer to crustal materials: Systematics, methodology, data reporting, and interpretation
Abstract The rhenium-osmium (187Re-187Os) system is a highly versatile chronometer that
is regularly applied to a wide range of geological and extraterrestrial materials. In addition to …
is regularly applied to a wide range of geological and extraterrestrial materials. In addition to …
Rhenium-osmium isotope evidence for the onset of volcanism in the central Panthalassa Ocean during the Norian “chaotic carbon episode”
The late Norian “chaotic carbon episode” in the Late Triassic has been identified in North
America, Italy, and China, reflecting a global carbon isotope perturbation. Although it has …
America, Italy, and China, reflecting a global carbon isotope perturbation. Although it has …
A new Rhaetian δ13Corg record: carbon cycle disturbances, volcanism, End-Triassic mass Extinction (ETE)
The links between large-scale volcanism, carbon cycle perturbations and the biotic crises at
the End-Triassic Extinction event (ETE) are not well understood. The ETE seems to be …
the End-Triassic Extinction event (ETE) are not well understood. The ETE seems to be …
Sixteen mass extinctions of the past 541 My correlated with 15 pulses of Large Igneous Province (LIP) volcanism and the 4 largest extraterrestrial impacts
Abstract We find that Large Igneous Province (LIP) volcanism, mostly continental flood
basalts (CFBs), along with the largest extraterrestrial impacts show significant correlations …
basalts (CFBs), along with the largest extraterrestrial impacts show significant correlations …
Carbon-isotope excursions in the Norian stage (Upper Triassic) of the Baoshan terrane, western Yunnan, China
The biostratigraphy and carbon stable isotopes of the Norian Stage (Upper Triassic) are well
studied in the western Tethys, but little information is available from the eastern Tethys …
studied in the western Tethys, but little information is available from the eastern Tethys …
The missing mass extinction at the Triassic-Jurassic boundary
SG Lucas, LH Tanner - The Late Triassic World: Earth in a Time of …, 2018 - Springer
Abstract The Late Triassic was a prolonged episode characterized by high rates of biotic
turnover and discrete extinction events due to elevated extinction rates for some biotic …
turnover and discrete extinction events due to elevated extinction rates for some biotic …