N(2)-fixing tropical legume evolution: a contributor to enhanced weathering through the Cenozoic?

Fossil and phylogenetic evidence indicates legume-rich modern tropical forests replaced Late Cretaceous palm-dominated tropical forests across four continents during the early Cenozoic (58–42 Ma). Tropical legume trees can transform ecosystems via their ability to fix dinitrogen (N(2)) and higher le...

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Detalles Bibliográficos
Autores principales: Epihov, Dimitar Z., Batterman, Sarah A., Hedin, Lars O., Leake, Jonathan R., Smith, Lisa M., Beerling, David J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society 2017
Materias:
Palaeobiology
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5563791/
https://www.ncbi.nlm.nih.gov/pubmed/28814651
http://dx.doi.org/10.1098/rspb.2017.0370

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5563791/
https://www.ncbi.nlm.nih.gov/pubmed/28814651
http://dx.doi.org/10.1098/rspb.2017.0370

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