Biological diagenesis: dicarboxylic acids in recent sediments

Details Biological diagenesis: dicarboxylic acids in recent sediments Biological diagenesis: dicarboxylic acids in recent sediments

Feb 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975gecoa..39..129j&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 39, Issue 2, pp.129-136

Physics

2

Scientific paper

A series of even carbon numbered , -dicarboxylic acids ranging from C 16 to C 24 has been identified in recent sediments from various environments and sampling localities. A lacustrine sediment did not show detectable quantities of diacids. Consideration of quantitative relationships involving the diacids leads us to propose a dual origin for these diacids: deposition by mangroves is their main source in mangal areas while in situ production by sedimentary organisms is the only important source of diacids in a non-mangal marine environment. A fresh water lagoon shows an intermediate situation between these extremes.

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