Artigo Revisado por pares

Characterization of a major refractory component of marine dissolved organic matter

2006; Elsevier BV; Volume: 70; Issue: 12 Linguagem: Inglês

10.1016/j.gca.2006.03.021

ISSN

1872-9533

Autores

Norbert Hertkorn, Ronald Benner, Moritz Frommberger, Philippe Schmitt‐Kopplin, Matthias Witt, Karl Kaiser, A. Kettrup, John I. Hedges,

Tópico(s)

Atmospheric and Environmental Gas Dynamics

Resumo

Refractory carboxyl-rich alicyclic molecules (CRAM) are characterized in marine dissolved organic matter (DOM) using nuclear magnetic resonance spectroscopy and ultrahigh resolution mass spectrometry. CRAM are distributed throughout the water column and are the most abundant components of deep ocean DOM ever characterized. CRAM are comprised of a complex mixture of carboxylated and fused alicyclic structures with a carboxyl-C:aliphatic-C ratio of 1:2 to 1:7. CRAM are expected to constitute a strong ligand for metal binding, and multiple coordination across cations could promote aggregation and marine gel formation thereby affecting CRAM reactivity and the bioavailability of nutrients and trace metals. It appears CRAM are ultimately derived from biomolecules with structural similarities to sterols and hopanoids. The occurrence of CRAM in freshwater and terrestrial environments seems likely, considering the global distribution of biomolecules and the similarities of biogeochemical processes among environments.

Referência(s)
Altmetric
PlumX