Articles | Volume 16, issue 5
https://doi.org/10.5194/cp-16-1759-2020
https://doi.org/10.5194/cp-16-1759-2020
Research article
 | 
22 Sep 2020
Research article |  | 22 Sep 2020

Influence of temporally varying weatherability on CO2-climate coupling and ecosystem change in the late Paleozoic

Jon D. Richey, Isabel P. Montañez, Yves Goddéris, Cindy V. Looy, Neil P. Griffis, and William A. DiMichele

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Cited articles

Balseiro, D. and Powell, M. G.: Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis, Geology, 48, 118–122, https://doi.org/10.1130/G46858.1, 2019. 
Beerling, D. J. and Berner, R. A.: Impact of a Permo-Carboniferous high O2 event on the terrestrial carbon cycle, P. Natl. Acad. Sci. USA, 97, 12428–12432, https://doi.org/10.1073/pnas.220280097, 2000. 
Beerling, D. J., Woodward, F. I., Lomas, M. R., Wills, M. A., Quick, W. P., and Valdes, P. J.: The influence of Carboniferous palaeoatmospheres on plant function: an experimental and modelling assessment, Philos. T. R. Soc. Lon. B, 353, 131–140, https://doi.org/10.1098/rstb.1998.0196, 1998. 
Belt, E. S., Heckel, P. H., Lentz, L. J., Bragonier, W. A., and Lyons, T. W.: Record of glacial–eustatic sea-level fluctuations in complex middle to late Pennsylvanian facies in the Northern Appalachian Basin and relation to similar events in the Midcontinent basin, Sediment. Geol., 238, 79–100, https://doi.org/10.1016/j.sedgeo.2011.04.004, 2011. 
Benton, M. J.: No gap in the Middle Permian record of terrestrial vertebrates, Geology, 40, 339–342, https://doi.org/10.1130/G32669.1, 2012. 
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Short summary
Our 40 Myr CO2 reconstruction substantially refines existing late Paleozoic CO2 estimates, provides the best resolved pre-Cenozoic CO2 record, and indicates a close temporal relationship to changes in marine and terrestrial ecosystems. The GEOCLIM model used in our study allows for insight into the relative influences of uplift of the Central Pangean Mountains, intensifying aridity, and increasing mafic-to-granite ratio of outcropping rocks on changes in pCO2 through the late Paleozoic.