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High potential for weathering and climate effects of non-vascular vegetation in the Late Ordovician

It has been hypothesized that predecessors of today's bryophytes significantly increased global chemical weathering in the Late Ordovician, thus reducing atmospheric CO(2) concentration and contributing to climate cooling and an interval of glaciations. Studies that try to quantify the enhancem...

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Detalles Bibliográficos
Autores principales: Porada, P., Lenton, T. M., Pohl, A., Weber, B., Mander, L., Donnadieu, Y., Beer, C., Pöschl, U., Kleidon, A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4941054/
https://www.ncbi.nlm.nih.gov/pubmed/27385026
http://dx.doi.org/10.1038/ncomms12113