Molecular characterization of microgram amounts of oceanic colloidal organic matter by direct temperature-resolved ammonia chemical ionization mass spectrometry
Jj. Boon et al., Molecular characterization of microgram amounts of oceanic colloidal organic matter by direct temperature-resolved ammonia chemical ionization mass spectrometry, ORG GEOCHEM, 29(5-7), 1998, pp. 1051-1061
Marine colloidal organic matter in coastal waters off the coast of the east
ern United States (from Georges Bank and the Mid-Atlantic Eight) is charact
erized by means of direct temperature-resolved mass spectrometry (DT-MS). C
hemical ionization (NH3) appears to be a very appropriate ionization method
for this material. The analytical data confirm the presence of a significa
nt polysaccharide fraction consisting of neutral sugars (normal-, deoxy- an
d methylated aldoses), N-acetyl aminosugars and, possibly, acidic sugars. T
he methylated and N-acetyl aminosugars are considered as markers for a bact
erial contribution. No evidence is found for polysaccharides with large hom
opolymeric domains, suggesting an origin distinct from the common structura
l polysaccharides that comprise major polymers in algae and higher plants.
The TIC profiles, which express the number of ions produced as a function o
f the temperature, often show a bimodal distribution. This indicates that t
he colloidal matter consists of two fractions with different thermal stabil
ities and probably also different chemical stabilities. Multivariate "mappi
ng" of the DT-MS spectra reveals that the chemical differences between thes
e two fractions show remarkable conformity amongst samples collected at wid
espread locations. The relative abundance of the two fractions appears to d
epend on both depth and location. The more thermally stable fraction is rel
atively abundant in deep water samples and some surface waters of the Mid-A
tlantic Eight. (C) 1998 Elsevier Science Ltd. All rights reserved.