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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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| Hoofdauteurs: | , , , |
|---|---|
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Public Library of Science
2013
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3622679/ https://ncbi.nlm.nih.gov/pubmed/23593262 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1371/journal.pone.0060614 |
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