Spatiotemporal distribution of global mercury enrichments through the Paleocene-Eocene Thermal Maximum and links to volcanism
Abstract Mercury (Hg) concentrations and Hg isotopes have been widely used to fingerprint
geological volcanism. Mercury content, as a more accessible proxy, is more frequently used …
geological volcanism. Mercury content, as a more accessible proxy, is more frequently used …
The role of LIPs in Phanerozoic mass extinctions: An Hg perspective
Abstract All of the Big Five mass extinctions (BFMEs) of the Phanerozoic are postulated to
have been associated with eruptions of large igneous provinces (LIPs), although the role of …
have been associated with eruptions of large igneous provinces (LIPs), although the role of …
[HTML][HTML] Effects of redox variability and early diagenesis on marine sedimentary Hg records
Volcanism is a dominant natural source of mercury (Hg) to the atmosphere, biosphere,
ocean and sediments. In recent years, sedimentary Hg contents have emerged as a tool to …
ocean and sediments. In recent years, sedimentary Hg contents have emerged as a tool to …
Climax in Wrangellia LIP activity coincident with major Middle Carnian (Late Triassic) climate and biotic changes: Mercury isotope evidence from the Panthalassa …
Abstract The Carnian Pluvial Episode (CPE,∼ 233 Ma) was characterized by multiple
negative carbon-isotope excursions, turnovers in marine and terrestrial biota, and a Tethys …
negative carbon-isotope excursions, turnovers in marine and terrestrial biota, and a Tethys …
Pelagic responses to oceanic anoxia during the Carnian Pluvial Episode (Late Triassic) in Panthalassa Ocean
Abstract The Carnian Pluvial Episode (CPE) was a short interval of extreme rainfall in the
Late Triassic that caused significant changes in marine ecosystems. Global warming …
Late Triassic that caused significant changes in marine ecosystems. Global warming …
CO2 buildup drove global warming, the Marinoan deglaciation, and the genesis of the Ediacaran cap carbonates
What caused ocean/climate changes that drove Marinoan deglaciation, and the subsequent
genesis of Ediacaran cap carbonates remains unclear. To address this issue, we examined …
genesis of Ediacaran cap carbonates remains unclear. To address this issue, we examined …
[HTML][HTML] Four volcanically driven climatic perturbations led to enhanced continental weathering during the Late Triassic Carnian Pluvial Episode
P Zhang, M Yang, J Lu, Z Jiang, P Vervoort… - Earth and Planetary …, 2024 - Elsevier
The arid climate of the Late Triassic was interrupted by a particularly humid episode known
as the Carnian Pluvial Episode (CPE; ca. 234–232 million years ago). The CPE is often …
as the Carnian Pluvial Episode (CPE; ca. 234–232 million years ago). The CPE is often …
Weathering and sea level control on siliciclastic deposition during the Carnian Pluvial Episode (Southern Alps, Italy)
A higher precipitation regime during the early Late Triassic Carnian Pluvial Episode (CPE;
232–234 Ma) in many marine basins is evidenced by thick siliciclastic deposits, which are …
232–234 Ma) in many marine basins is evidenced by thick siliciclastic deposits, which are …
Palaeoenvironmental changes in the Late Triassic lacustrine facies of the Ordos Basin of Northwest China were driven by multistage volcanic activity: Implications for …
M Lin, K Xi, Y Cao, X Niu, W Ma, X Wang… - Palaeogeography …, 2024 - Elsevier
Abstract The Carnian Pluvial Event (CPE) induced an intense carbon-cycle disturbance and
biological crisis at a global scale. The eruption of the Wrangellia Large Igneous Province (W …
biological crisis at a global scale. The eruption of the Wrangellia Large Igneous Province (W …
Floral response to the late triassic carnian pluvial episode
P Zhang, M Yang, J Lu, Z Jiang, K Zhou… - Frontiers in Ecology …, 2023 - frontiersin.org
The Late Triassic Carnian Pluvial Episode (CPE; ca. 234–232 Ma) was characterized by
dramatic global temperature and humidity increases, which in many terrestrial settings was …
dramatic global temperature and humidity increases, which in many terrestrial settings was …