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Nutrient acquisition by symbiotic fungi governs Palaeozoic climate transition
Fossil evidence from the Rhynie chert indicates that early land plants, which evolved in a high-CO(2) atmosphere during the Palaeozoic Era, hosted diverse fungal symbionts. It is hypothesized that the rise of early non-vascular land plants, and the later evolution of roots and vasculature, drove the...
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| Publicat a: | Philos Trans R Soc Lond B Biol Sci |
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| Autors principals: | , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
The Royal Society
2018
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5745338/ https://ncbi.nlm.nih.gov/pubmed/29254967 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rstb.2016.0503 |
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