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      Influence of hydrological, biogeochemical and temperature transients on subsurface carbon fluxes in a flood plain environment

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          Most cited references 105

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          Plumbing the Global Carbon Cycle: Integrating Inland Waters into the Terrestrial Carbon Budget

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            Persistence of soil organic matter as an ecosystem property.

            Globally, soil organic matter (SOM) contains more than three times as much carbon as either the atmosphere or terrestrial vegetation. Yet it remains largely unknown why some SOM persists for millennia whereas other SOM decomposes readily--and this limits our ability to predict how soils will respond to climate change. Recent analytical and experimental advances have demonstrated that molecular structure alone does not control SOM stability: in fact, environmental and biological controls predominate. Here we propose ways to include this understanding in a new generation of experiments and soil carbon models, thereby improving predictions of the SOM response to global warming.
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              Analysis of Factors Controlling Soil Organic Matter Levels in Great Plains Grasslands1

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                Author and article information

                Journal
                Biogeochemistry
                Biogeochemistry
                Springer Nature
                0168-2563
                1573-515X
                February 2016
                February 12 2016
                February 2016
                : 127
                : 2-3
                : 367-396
                Article
                10.1007/s10533-016-0186-8
                © 2016

                http://www.springer.com/tdm

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