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Rapid biotic molecular transformation of fulvic acids in a karst aquifer.
Geochim. Cosmochim. Acta 71, 5474-5482 (2007)
The study of molecular transformation processes of dissolved organic carbon (DOC) in the environment significantly contributes to a better understanding of the global biogeochemical organic matter cycle. In an oxic karst groundwater system, in which the most powerful abiotic DOC degradative reactions, photodegradation and metal-mediated redox chemistry, are at best marginal contributors, a near complete turnover of fulvic acids (FAs) has been observed within decades (not, vert, similar60 years). Depletion of oxygen for a very extensive range of aliphatic and aromatic carbon chemical environments has been confirmed as well as the formation of novel classes of compounds, suggesting a major contribution from biotic processes. From these results we infer that FAs must be perceived as a rather active participant in the global carbon cycle. Molecular-level alterations of such magnitude and rapidity on such short-time scales ought to be considered as widespread in the processing of “refractory” DOC in the environment.
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Publikationstyp
Artikel: Journalartikel
Dokumenttyp
Wissenschaftlicher Artikel
ISSN (print) / ISBN
0016-7037
e-ISSN
1872-9533
Zeitschrift
Geochimica et Cosmochimica Acta
Quellenangaben
Band: 71,
Heft: 22,
Seiten: 5474-5482
Verlag
Elsevier
Begutachtungsstatus
Peer reviewed
Institut(e)
Institute of Groundwater Ecology (IGOE)
Institute of Ecological Chemistry (IOEC)
Institute of Ecological Chemistry (IOEC)