Am. Compiano et al., MONOSACCHARIDE COMPOSITION OF SUSPENDED ORGANIC PARTICULATE MATTER INRELATION TO ITS ORIGIN, Oceanologica acta, 16(2), 1993, pp. 135-144
Samples of phytoplankton cultures and of suspended particulate matter
from continental, brackish and marine waters were examined by HPLC for
the monosaccharide content of their hydrolysable sugar fraction. Eigh
t monosaccharides were currently assayed and their weight compared to
HPLC-assayed chlorophyll a concentrations. With the exception of oligo
trophic waters, these two variables are well correlated in the various
prospected environments. Glucose was always the strongly dominant for
m, not only in fresh and brackish waters but also in marine samples wi
th high phytoplanktonic biomass. If samples are compared on a salinity
basis, only four monosaccharides showed significant differences in th
eir relative concentrations, as a consequence of sampling location: ri
bose, galactose and mannose contents were higher in marine waters (sal
inity > 35) and arabinose in brackish or fresh waters (salinity < 25).
On the other hand, no significant difference appears between the two
respective average glucose relative concentrations. No direct relation
ship could be established between the origin of organic matter (marine
or continental) and monosaccharide ratios or an order of monosacchari
de predominance in hydrolysable sugar fraction. But the occurrence of
phytoplanktonic bloom was frequently associated with an enhancement of
glucose relative concentrations as compared to other monosaccharide f
orms. Moreover, ribose and galactose relative values can provide valua
ble information and appear to be linked to phytoplanktonic biomass in
marine waters.