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Long-term oceanic changes prior the end-Triassic mass extinction
Marie-Emilie Clemence, Wolfgang Mette,
Nicolas Rudolph Thibault
,
Christoph Korte
Geologi
428
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Keyphrases
End-Triassic Mass Extinction
100%
Rhaetian
100%
Northern Calcareous Alps
50%
Stomatal Density
25%
Carbon Isotope Excursion
25%
Climatic Fluctuations
25%
Tethys
25%
End-Triassic
25%
Black Shale
25%
Shale
25%
Ocean Basins
12%
Marl
12%
Terrestrial Biota
12%
Atmospheric CO2 Concentration
12%
Direct Connection
12%
Carbon Cycle Perturbation
12%
Fossil Leaves
12%
Climatic Events
12%
Volcanism
12%
Stratigraphy
12%
Tethyan
12%
Ocean Acidification
12%
Environmental Perturbations
12%
Sea Level Variations
12%
Marine Biota
12%
Triassic-Jurassic Boundary
12%
Coral Reefs
12%
Stable Isotopes
12%
Carbonate
12%
Limestone-marl Alternations
12%
Rising CO2
12%
Trace Element Analysis
12%
Organic-rich
12%
Triassic-Jurassic
12%
Organic Matter
12%
Oxygen Isotopes
12%
Earth and Planetary Sciences
Rhaetian
100%
Mass Extinction
100%
Tethys
25%
Black Shale
25%
Marine Biota
12%
Organic Matter
12%
Purity
12%
Ocean Acidification
12%
Stable Isotope
12%
Volcanism
12%
Trace Element
12%
Atmospherics
12%
Reef
12%
Stratigraphy
12%
Carbon Cycle
12%
Sea Level
12%
Carbon Dioxide
12%
Coral Reef
12%
Sedimentology
12%