Flood basalts and mass extinctions
ME Clapham, PR Renne - Annual Review of Earth and …, 2019 - annualreviews.org
Flood basalts were Earth's largest volcanic episodes that, along with related intrusions, were
often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events …
often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events …
Quantifying early marine diagenesis in shallow-water carbonate sediments
Shallow-water carbonate sediments constitute one of the most abundant and widely used
archives of Earth's surface evolution. One of the main limitations of this archive is the …
archives of Earth's surface evolution. One of the main limitations of this archive is the …
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 …
Anomalous marine calcium cycle linked to carbonate factory change after the Smithian Thermal Maximum (Early Triassic)
Extreme greenhouse warming in the latest Permian played a key role in the largest animal
extinction event ever recorded in Earth history. The extinction was likely triggered by …
extinction event ever recorded in Earth history. The extinction was likely triggered by …
Calcium isotope compositions of subduction-related leucite-bearing rocks: Implications for the calcium isotope heterogeneity of the mantle and carbonate recycling in …
H Ren, M Casalini, S Conticelli, C Chen… - … et Cosmochimica Acta, 2024 - Elsevier
Large Ca isotope variations recorded in mantle xenoliths and mantle-derived igneous rocks
have been widely used to decode the origin of mantle heterogeneity, especially to trace …
have been widely used to decode the origin of mantle heterogeneity, especially to trace …
Uranium isotope evidence for an expansion of marine anoxia during the end‐T riassic extinction
The end‐Triassic extinction coincided with an increase in marine black shale deposition and
biomarkers for photic zone euxinia, suggesting that anoxia played a role in suppressing …
biomarkers for photic zone euxinia, suggesting that anoxia played a role in suppressing …
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 …
Calcium isotopes in deep time: Potential and limitations
Calcium is an essential element in the biogeochemical cycles that regulate the long-term
climate state of Earth. The removal of CO 2 from the ocean-atmosphere system is controlled …
climate state of Earth. The removal of CO 2 from the ocean-atmosphere system is controlled …
[HTML][HTML] Uranium isotope evidence for extensive seafloor anoxia after the end-Triassic mass extinction
The end-Triassic extinction (ETE) ranks as one of the 'Big Five'biotic crises of the
Phanerozoic and is thought to be triggered by volcanism of the Central Atlantic Magmatic …
Phanerozoic and is thought to be triggered by volcanism of the Central Atlantic Magmatic …
Coupled δ44/40Ca, δ88/86Sr, and 87Sr/86Sr geochemistry across the end-Permian mass extinction event
J Wang, AD Jacobson, H Zhang, J Ramezani… - … et Cosmochimica Acta, 2019 - Elsevier
We report high-resolution, high-precision δ 44/40 Ca, δ 88/86 Sr, and 87 Sr/86 Sr records
spanning the Permian-Triassic boundary (PTB) from the Meishan and Dajiang carbonate …
spanning the Permian-Triassic boundary (PTB) from the Meishan and Dajiang carbonate …