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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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The Royal Society
2018
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5745338/ https://www.ncbi.nlm.nih.gov/pubmed/29254967 http://dx.doi.org/10.1098/rstb.2016.0503 |