Compound-specific carbon isotopes from Earth's largest flood basalt eruptions directly linked to the end-Triassic mass extinction
about
Integration of molecules and new fossils supports a Triassic origin for Lepidosauria (lizards, snakes, and tuatara)Tracking taphonomic regimes using chemical and mechanical damage of pollen and spores: an example from the Triassic-Jurassic mass extinctionBolide impact triggered the Late Triassic extinction event in equatorial PanthalassaIncreased atmospheric SO₂ detected from changes in leaf physiognomy across the Triassic-Jurassic boundary interval of East GreenlandAn analytical approach for estimating fossil record and diversification events in sharks, skates and raysAn explanation for conflicting records of Triassic-Jurassic plant diversityMass extinctions of life and catastrophic flood basalt volcanismIchthyosaurs from the French Rhaetian indicate a severe turnover across the Triassic–Jurassic boundaryZircon U-Pb geochronology links the end-Triassic extinction with the Central Atlantic Magmatic Province.End-Triassic mass extinction started by intrusive CAMP activity.Atmospheric carbon injection linked to end-Triassic mass extinction.Triassic-Jurassic climate in continental high-latitude Asia was dominated by obliquity-paced variations (Junggar Basin, Ürümqi, China)Geographic range did not confer resilience to extinction in terrestrial vertebrates at the end-Triassic crisis.Mercury evidence for pulsed volcanism during the end-Triassic mass extinction.Atmospheric PCO₂ perturbations associated with the Central Atlantic Magmatic Province.Mercury, volcanism, and mass extinctions.Large-scale sill emplacement in Brazil as a trigger for the end-Triassic crisis.Impact of the Late Triassic mass extinction on functional diversity and composition of marine ecosystemsA tale of two extinctions: converging end-Permian and end-Triassic scenariosArctic Deltaic Lake Sediments As Recorders of Fluvial Organic Matter DepositionPlacing our current 'hyperthermal' in the context of rapid climate change in our geological pastModelling the impact of pulsed CAMP volcanism on pCO2 and δ13C across the Triassic–Jurassic transitionCuticle surfaces of fossil plants as a potential proxy for volcanic SO2 emissions: observations from the Triassic–Jurassic transition of East GreenlandCould a potential Anthropocene mass extinction define a new geological period?Aspects of the Archean-Proterozoic transition: How the great Huronian Glacial Event was initiated by rift-related uplift and terminated at the rift-drift transition during break-up of Lauroscandia
P2860
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P2860
Compound-specific carbon isotopes from Earth's largest flood basalt eruptions directly linked to the end-Triassic mass extinction
description
2010 nî lūn-bûn
@nan
2010 թուականի Ապրիլին հրատարակուած գիտական յօդուած
@hyw
2010 թվականի ապրիլին հրատարակված գիտական հոդված
@hy
2010年の論文
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2010年学术文章
@wuu
2010年学术文章
@zh-cn
2010年学术文章
@zh-hans
2010年学术文章
@zh-my
2010年学术文章
@zh-sg
2010年學術文章
@yue
name
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@ast
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@en
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@nl
type
label
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@ast
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@en
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@nl
prefLabel
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@ast
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@en
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@nl
P2093
P2860
P3181
P356
P1476
Compound-specific carbon isoto ...... e end-Triassic mass extinction
@en
P2093
Jessica H Whiteside
Michael E Brookfield
Paul E Olsen
Raymond N Sambrotto
Timothy Eglinton
P2860
P304
P3181
P356
10.1073/PNAS.1001706107
P407
P577
2010-04-13T00:00:00Z
P5875
P698
P819
2010PNAS..107.6721W