The importance of wetlands in the global C budget has been recognized in recent years, and the high biomass productivity of riverine fioodplains is widely acknowledged. However, soil C dynamics in these ecosystems are still poorly understood and rarely quantified. In this study, we quantify organic C accretion and examine changes of organic matter pools across an age gradient of riverine fioodplain soils under different land uses in a warm temperate climate. We find rapid C accumulation during the initial 100 years of soil formation, with rates exceeding 100 g m-2 a-1. We show that fioodplain land use strongly affects soil C sequestration and organic matter pool allocation and find that the distribution of different soil organic matter pools reaches a steady state within a few decades of soil development. Our results demonstrate that continually rejuvenated soils on riverine fioodplains are strong C sinks but also show that intensive cultivation severely compromises their high C sequestration potential. Copyright 2009 by the American Geophysical Union.
CITATION STYLE
Zehetner, F., Lair, G. J., & Gerzabek, M. H. (2009). Rapid carbon accretion and organic matter pool stabilization in riverine floodplain soils. Global Biogeochemical Cycles, 23(4). https://doi.org/10.1029/2009GB003481
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