Cargando…
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...
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: | |
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 |
Ejemplares similares
-
CO(2)
‐induced biochemical changes in leaf volatiles decreased fire‐intensity in the run‐up to the Triassic–Jurassic boundary
por: Baker, Sarah J., et al.
Publicado: (2022) -
Differences in the photosynthetic plasticity of ferns and Ginkgo grown in experimentally controlled low [O(2)]:[CO(2)] atmospheres may explain their contrasting ecological fate across the Triassic–Jurassic mass extinction boundary
por: Yiotis, C., et al.
Publicado: (2017) -
Tracking Taphonomic Regimes Using Chemical and Mechanical Damage of Pollen and Spores: An Example from the Triassic–Jurassic Mass Extinction
por: Mander, Luke, et al.
Publicado: (2012) -
Synchronous Wildfire Activity Rise and Mire Deforestation at the Triassic–Jurassic Boundary
por: Petersen, Henrik I., et al.
Publicado: (2012) -
Sauropodomorph evolution across the Triassic–Jurassic boundary: body size, locomotion, and their influence on morphological disparity
por: Apaldetti, Cecilia, et al.
Publicado: (2021)