Effect of end-Triassic CO2 maximum on carbonate sedimentation and marine mass extinction

2004/07/27 by Michael Hautmann · 8 citations
Earth and Planetary Sciences · #Geological and Geophysical Studies #Geology and Paleoclimatology Research #Paleontology and Stratigraphy of Fossils

paper · doi:10.1007/s10347-004-0020-y

openalex publication_date 2004/07/27 · crossref created 2004/07/27 · crossref issued 2004/07/28 · crossref published 2004/07/28 · crossref published-online 2004/07/28 · crossref published-print 2004/09/01 · openalex created_date 2016/06/24 · crossref deposited 2019/05/31 · crossref indexed 2026/06/02 · openalex updated_date 2026/07/29

Citations

• Facies and geochemical evidence bearing on the end‐triassic disappearance of the alpine reef ecosystem
• Secular oscillations in the carbonate mineralogy of reef-building and sediment-producing organisms driven by tectonically forced shifts in seawater chemistry

Cited by

• A new correlation of Triassic–Jurassic boundary successions in NW Europe, Nevada and Peru, and the Central Atlantic Magmatic Province: A time-line for the end-Triassic mass extinction
• Extinction: End‐Triassic Mass Extinction
• Recognising ocean acidification in deep time: An evaluation of the evidence for acidification across the Triassic-Jurassic boundary
• Extinction-Recovery Pattern of Level-Bottom Faunas Across the Triassic-Jurassic Boundary in Tibet: Implications for Potential Killing Mechanisms
• Gastropods underwent a major taxonomic turnover during the end-Triassic marine mass extinction event
• Is the relative thickness of ammonoid septa influenced by ocean acidification, phylogenetic relationships and palaeogeographic position?
• Latest Triassic (Sevatian–Rhaetian) reef carbonates from the Northern Calcareous Alps (Austria), their mollusc dwellers, and their fate at the end-Triassic extinction event
• Ocean acidification [wikipedia]