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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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| Hlavní autoři: | , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Public Library of Science
2013
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| Témata: | |
| On-line přístup: | 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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