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 …
[HTML][HTML] Extant diversity of bryophytes emerged from successive post-Mesozoic diversification bursts
B Laenen, B Shaw, H Schneider, B Goffinet… - Nature …, 2014 - nature.com
Unraveling the macroevolutionary history of bryophytes, which arose soon after the origin of
land plants but exhibit substantially lower species richness than the more recently derived …
land plants but exhibit substantially lower species richness than the more recently derived …
[HTML][HTML] No mass extinction for land plants at the Permian–Triassic transition
H Nowak, E Schneebeli-Hermann… - Nature …, 2019 - nature.com
The most severe mass extinction among animals took place in the latest Permian (ca. 252
million years ago). Due to scarce and impoverished fossil floras from the earliest Triassic …
million years ago). Due to scarce and impoverished fossil floras from the earliest Triassic …
Ultra-shallow-marine anoxia in an Early Triassic shallow-marine clastic ramp (Spitsbergen) and the suppression of benthic radiation
PB Wignall, DPG Bond, Y Sun… - Geological …, 2016 - pubs.geoscienceworld.org
Lower Triassic marine strata in Spitsbergen accumulated on a mid-to-high latitude ramp in
which high-energy foreshore and shoreface facies passed offshore into sheet sandstones of …
which high-energy foreshore and shoreface facies passed offshore into sheet sandstones of …
Conodont calcium isotopic evidence for multiple shelf acidification events during the Early Triassic
The marine calcium (Ca) cycle is controlled by rates of continental weathering, seawater pH,
and carbonate deposition on the seafloor and is linked to atmospheric CO 2, climate …
and carbonate deposition on the seafloor and is linked to atmospheric CO 2, climate …
Cooling-driven oceanic anoxia across the Smithian/Spathian boundary (mid-Early Triassic)
Abstract The Smithian/Spathian boundary (SSB) represents a major climatic-oceanic-biotic
event within the~ 5-Myr-long recovery interval of the Early Triassic following the end …
event within the~ 5-Myr-long recovery interval of the Early Triassic following the end …
Lipid biomarkers for the reconstruction of deep-time environmental conditions
Lipids can survive long geological intervals within sediments and provide a unique tool that
allows the reconstruction of past organismic diversity and environmental conditions. The …
allows the reconstruction of past organismic diversity and environmental conditions. The …
Global-ocean redox variations across the Smithian-Spathian boundary linked to concurrent climatic and biotic changes
Abstract The Smithian-Spathian boundary (SSB) was an interval characterized by a major
global carbon cycle perturbation, climatic cooling from a middle/late Smithian boundary …
global carbon cycle perturbation, climatic cooling from a middle/late Smithian boundary …
87Sr/86Sr stratigraphy from the Early Triassic of Zal, Iran: Linking temperature to weathering rates and the tempo of ecosystem recovery
ARC Sedlacek, MR Saltzman, TJ Algeo… - …, 2014 - pubs.geoscienceworld.org
Abstract Recovery from the Late Permian mass extinction was slowed by continued
environmental perturbations during the Early Triassic. Rapid fluctuations of the Early Triassic …
environmental perturbations during the Early Triassic. Rapid fluctuations of the Early Triassic …