Phanerozoic paleotemperatures: The earth's changing climate during the last 540 million years
This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …
have changed during the last 540 million years. It combines paleotemperature …
Coupling of paleoenvironment and biogeochemistry of deep-time alkaline lakes: A lipid biomarker perspective
L Xia, J Cao, W Hu, D Zhi, Y Tang, E Li, W He - Earth-Science Reviews, 2021 - Elsevier
Studies of alkaline lakes have critical biological–environmental–economic properties, but
deep-time alkaline lakes are challenging to investigate. Lipid biomarkers can provide …
deep-time alkaline lakes are challenging to investigate. Lipid biomarkers can provide …
How Large Igneous Provinces affect global climate, sometimes cause mass extinctions, and represent natural markers in the geological record
Abstract Large Igneous Provinces (LIPs) can have a significant global climatic effect as
monitored by sedimentary trace and isotopic compositions that record paleo …
monitored by sedimentary trace and isotopic compositions that record paleo …
Recurrent photic zone euxinia limited ocean oxygenation and animal evolution during the Ediacaran
Abstract The Ediacaran Period (~ 635–539 Ma) is marked by the emergence and
diversification of complex metazoans linked to ocean redox changes, but the processes and …
diversification of complex metazoans linked to ocean redox changes, but the processes and …
Mercury isotope evidence for recurrent photic-zone euxinia triggered by enhanced terrestrial nutrient inputs during the Late Devonian mass extinction
Widespread oceanic anoxia marked by globally extensive deposition of organic-rich black
shale during the Late Devonian was a major factor in the mass extinctions at the Frasnian …
shale during the Late Devonian was a major factor in the mass extinctions at the Frasnian …
Mercury isotope evidence for marine photic zone euxinia across the end-Permian mass extinction
The driving forces, kill and recovery mechanisms for the end-Permian mass extinction
(EPME), the largest Phanerozoic biological crisis, are under debate. Sedimentary records of …
(EPME), the largest Phanerozoic biological crisis, are under debate. Sedimentary records of …
Evidence for the Carnian Pluvial Episode in Gondwana: New multiproxy climate records and their bearing on early dinosaur diversification
The Triassic hothouse world experienced dynamic changes in climate and ecosystems that
set the Earth's climate and biotic states for much of the Mesozoic Era. A critical time interval …
set the Earth's climate and biotic states for much of the Mesozoic Era. A critical time interval …
Zinc isotope evidence for intensive magmatism immediately before the end-Permian mass extinction
The end-Permian extinction is typically ascribed to massive volcanic eruptions, but direct
geochemical evidence linking the two independent events is generally lacking. Zinc is an …
geochemical evidence linking the two independent events is generally lacking. Zinc is an …
End-Permian burnout: The role of Permian–Triassic wildfires in extinction, carbon cycling, and environmental change in eastern Gondwana
C Mays, S McLoughlin - Palaios, 2022 - pubs.geoscienceworld.org
Wildfire has been implicated as a potential driver of deforestation and continental
biodiversity loss during the end-Permian extinction event (EPE;∼ 252 Ma). However, it …
biodiversity loss during the end-Permian extinction event (EPE;∼ 252 Ma). However, it …
[HTML][HTML] Phanerozoic variation in dolomite abundance linked to oceanic anoxia
The abundance of dolomitic strata in the geological record contrasts with the general rarity of
locations where dolomite forms today, a discrepancy that has long posed a problem for their …
locations where dolomite forms today, a discrepancy that has long posed a problem for their …