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 …
Extant diversity of bryophytes emerged from successive post-Mesozoic diversification bursts
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 …
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 …
End Permian to Middle Triassic plant species richness and abundance patterns in South China: Coevolution of plants and the environment through the Permian …
This study reviews plant species richness and abundance change from the End Permian to
Middle Triassic in South China and examines the co-evolutionary relationship between the …
Middle Triassic in South China and examines the co-evolutionary relationship between the …
Ultra-shallow-marine anoxia in an Early Triassic shallow-marine clastic ramp (Spitsbergen) and the suppression of benthic radiation
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 …
Ancient large‐scale gene duplications and diversification in bryophytes illuminate the plant terrestrialization
C Shen, H Li, L Shu, WZ Huang, RL Zhu - New Phytologist, 2024 - Wiley Online Library
Large‐scale gene duplications (LSGDs) are crucial for evolutionary adaptation and
recurrent in vascular plants. However, the role of ancient LSGDs in the terrestrialization and …
recurrent in vascular plants. However, the role of ancient LSGDs in the terrestrialization and …