On impact and volcanism across the Cretaceous-Paleogene boundary
The cause of the end-Cretaceous mass extinction is vigorously debated, owing to the
occurrence of a very large bolide impact and flood basalt volcanism near the boundary …
occurrence of a very large bolide impact and flood basalt volcanism near the boundary …
Halogens in mafic and intermediate-silica content magmas
As volatile and variably mobile components, halogens play key roles in magmatic,
metasomatic, mineralizing, and volcanic processes by influencing the physical and chemical …
metasomatic, mineralizing, and volcanic processes by influencing the physical and chemical …
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 …
Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
E Font, T Adatte, AN Sial, LD de Lacerda… - …, 2016 - pubs.geoscienceworld.org
The contribution of the Deccan Traps (west-central India) volcanism in the Cretaceous-
Paleogene (KPg) crisis is still a matter of debate. Recent U-Pb dating of zircons interbedded …
Paleogene (KPg) crisis is still a matter of debate. Recent U-Pb dating of zircons interbedded …
Reconciling early Deccan Traps CO2 outgassing and pre-KPB global climate
A Hernandez Nava, BA Black… - Proceedings of the …, 2021 - National Acad Sciences
A 2 to 4° C warming episode, known as the Latest Maastrichtian warming event (LMWE),
preceded the Cretaceous–Paleogene boundary (KPB) mass extinction at 66.05±0.08 Ma …
preceded the Cretaceous–Paleogene boundary (KPB) mass extinction at 66.05±0.08 Ma …
Environmental changes during the Cretaceous-Paleogene mass extinction and Paleocene-Eocene thermal maximum: implications for the Anthropocene
Abstract The Cretaceous-Paleogene boundary (KPB) mass extinction (~ 66.02 Ma) and the
Paleocene-Eocene Thermal Maximum (PETM)(~ 55.8 Ma) are two remarkable climatic and …
Paleocene-Eocene Thermal Maximum (PETM)(~ 55.8 Ma) are two remarkable climatic and …
Mercury enrichment and Hg isotopes in Cretaceous–Paleogene boundary successions: Links to volcanism and palaeoenvironmental impacts
We investigate the use of Hg as a proxy for volcanism by studying four distal and two
proximal sections in relation to the Deccan volcanic center, straddling the Cretaceous …
proximal sections in relation to the Deccan volcanic center, straddling the Cretaceous …
Upheavals during the late Maastrichtian: Volcanism, climate and faunal events preceding the end-Cretaceous mass extinction
The late Maastrichtian was a time of major climate, evolution and extinction extremes. Rapid
climate warming of 2–3° C in intermediate waters between 69.5 and 68 Ma (top C31r to …
climate warming of 2–3° C in intermediate waters between 69.5 and 68 Ma (top C31r to …
Effects of Deccan volcanism on paleoenvironment and planktic foraminifera: A global survey
Deccan volcanism, one of Earth's largest flood basalt provinces, erupted~ 80% of its total
volume (phase 2) during a relatively short time in the uppermost Maastrichtian …
volume (phase 2) during a relatively short time in the uppermost Maastrichtian …
Imprints of modal metasomatism in the post-Deccan subcontinental lithospheric mantle: petrological evidence from an ultramafic xenolith in an Eocene lamprophyre …
We report here on the occurrence of an interesting mantle-derived ultramafic xenolith
entrained in an Eocene (c. 55 Ma) lamprophyre dyke from the Dongargaon area of the …
entrained in an Eocene (c. 55 Ma) lamprophyre dyke from the Dongargaon area of the …