Heterogeneity of soil organic matter composition and its fate across ecosystem boundaries, or does it all come out in the wash?

Abstract:

A grand challenge in our understanding of the global carbon cycle is the vulnerability of large organic carbon pools at the land–water interface to changes in climate and to landscape disturbance. The expectation that terrestrial organic matter (OM) should be dominated by lignified (aromatic) plant-derived material or nitrogen-poor, complex soil OM with old radiocarbon ages has contributed to predictions of low bioavailability or chemical recalcitrance for terrigenous OM. Recent shifts in our understanding of the source of OM in soils and the mechanisms contributing to its persistence or loss have refocused attention on environmental parameters influencing the fate of OM and its role as a source of C to the atmosphere. On land, climate, soil mineralogy, topography, drainage, vegetation, disturbance (e.g., fire) and human land use influence the quantity and biochemical composition of organic matter accumulating in soils and available for lateral transfer to aquatic systems in dissolved or particulate form. Growing research indicates that local site conditions and disturbance history are important for predicting the response of soil OM to environmental change, often more so than OM chemical composition, contradicting traditional models that tie reactivity to structure. Soils are a large source of C entering waterways, yet how much landscape heterogeneity within the watershed matters for understanding the fate of C downstream is unknown: does all this heterogeneity come out in the wash? Here we follow up on recent discussions about environmental controls on the composition and age of OM in soil, what type and age of C is mobilized during landscape disturbance, and how its source on land can help predict its fate downstream. To further improve understanding of how landscape alterations affect transfers from land to water and fill some of the gaps in the global C cycle, we identify areas of research where collaborations between aquatic and terrestrial scientists would be especially fruitful.