Increased Atmospheric SO(2) Detected from Changes in Leaf Physiognomy across the Triassic–Jurassic Boundary Interval of East Greenland

The Triassic–Jurassic boundary (Tr–J; ∼201 Ma) is marked by a doubling in the concentration of atmospheric CO(2), rising temperatures, and ecosystem instability. This appears to have been driven by a major perturbation in the global carbon cycle due to massive volcanism in the Central Atlantic Magma...

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Detalles Bibliográficos
Autores principales: Bacon, Karen L., Belcher, Claire M., Haworth, Matthew, McElwain, Jennifer C.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2013
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3622679/
https://www.ncbi.nlm.nih.gov/pubmed/23593262
http://dx.doi.org/10.1371/journal.pone.0060614

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3622679/
https://www.ncbi.nlm.nih.gov/pubmed/23593262
http://dx.doi.org/10.1371/journal.pone.0060614

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