An important contributor to atmospheric Carbon is the decomposition of organics in the soil by free living microbes. One of the key resources for these microbes is the availability of Nitrogen, which plants via their mycorrhizal marriages, compete actively for. This would mean that the more active and successful the fungi are at gathering Nitrogen, the less active and successful the free decomposers would be at breaking up organic matter. That, in turn, would lead to an increased storage of Carbon in the Soil.
Amanita phalloides (an Ectomycorrhizal fungi) |
To study the importance that the mycorrhizal relationship had on Carbon stored in the soil (and thus not in the atmosphere), this group of scientists compared the not only the two above mentioned groups, but also the difference in annual temperature, precipitation, net primary production and clay content, of multiple ecosystems based on global data product measurements.
Their results showed that the EEM ecosystems had a significantly higher storage of Carbon than the AM ecosystems. When contrasting to the other data measurements, it was determined that the mycorrhizal type was a far more important controller of soil Carbon than the rest.
This means that the Carbon cycle (exchange of carbon throughout the environment) is in part managed by the mycorrhizal control exerted on decomposition in the soil. And as such, the broad implications that could be derived from this study are that changes altering the competition for Nitrogen will also greatly alter the global levels of Carbon in the Atmosphere.
Colin Averill, Benjamin L. Turner, & Adrien C. Finzi (2014). Mycorrhiza-mediated competition between plants and decomposers drives soil carbon storage Nature DOI: 10.1038/nature12901
Photo by Aleksey Gnilenkov (http://www.flickr.com/photos/gnilenkov/5083008614/) [CC-BY-2.0 (http://creativecommons.org/licenses/by/2.0)], via Wikimedia Commons
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