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• W2144857900 abstract "and 14 C dating of dissolved inorganic carbon revealed that ancient SOC mineralization was common, and that it constituted 31–100% of C mineralization 2.6 m deep at one site, at rates sufficient to influence landscape N budgets. Our data failed to reveal consistent spatial patterns of microbially available ancient C. Although mineralized C age increased with depth at one alluvial site, we observed ancient C metabolism 150 cm deep at a glaciofluvial site, suggesting that subsurface microbial activity in riparian zones does not vary systematically between alluvial and glaciofluvial hydrogeologic settings. These findings underscore the relevance of ancient C to contemporary ecosystem processes and the challenge of using mappable surface features to identify subsurface ecosystem characteristics or riparian zone N-sink strength." @default.
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• W2144857900 date "2008-05-10" @default.
• W2144857900 modified "2023-10-18" @default.
• W2144857900 title "Mineralization of ancient carbon in the subsurface of riparian forests" @default.
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• W2144857900 doi "https://doi.org/10.1029/2007jg000482" @default.
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