Humic substances, which are randomly cross-linked heterogeneous organic
materials of high
molecular weight, comprise a major fraction of the organic matter in
soils and sediments. Because
humic substances have a variety of functional groups, they play a major
role in controlling the
physical and chemical characteristics of natural waters, soils, and
sediments. Sedimentary humic
substances are considered to be the precursors of petroleum-forming
kerogens. Sulfur is thought
to play a major role in forming humic substances in anoxic marine
sediments. Because of their
structural heterogeneity, humic substances are not easily amenable to
biochemical degradation
and, thus, are generally considered to be biologically refractory.
The complexity and heterogeneity
of humic substances render the elucidation of their chemical structure
a major analytical
challenge. Degradative techniques, such as pyrolysis GC−MS, can
change a sample's structure
during preparation and analysis and, thus, may give inaccurate
information. In this study, we
investigated the sulfur-containing functional groups in humic acids
from various marine sediments
using XANES spectroscopy which has proved to be an important,
nondestructive tool for analyzing
sulfur forms. Humic acids were isolated from near-surface
sediments from three locations: a
salt marsh in Shelter Island, NY; the Peru Margin; and Florida Bay.
We found that organic
sulfides, di- and polysulfides, sulfonates, and organic sulfates are
the major forms of sulfur in
these sedimentary humics. The reduced-sulfur structures, organic
sulfides, and di- and
polysulfides, are essentially intramolecular as opposed to the highly
oxidized forms of sulfur,
sulfonates, and ester-bonded sulfates, which can only be present as end
groups. The abundance
of the reduced-sulfur structures reflects the extent to which sulfur is
involved in forming
intramolecular cross-links which are crucial for building up the
macromolecular structures of
humic substances. The significance of the presence of the
different sulfur functionalities in humic
substances is discussed in relation to early diagenesis and
preservation of organic matter in marine
sediments.