Two box-core sediments off the northeastern Taiwan coast have been col
lected and examined for the relationship between bound lipids and grai
n size in the mud fraction (< 63 mu m). No grain size effect was found
for the concentrations of Sigma n-alkanes, Sigma n-fatty acids and Si
gma n-alcohols. The ratios of branched-chain to normal fatty acids inc
reased progressively with decreasing particle size and correlated high
ly with BOC (bound organic carbon), suggesting an increasing bacterial
input. Moreover, we observed an increase in the ratios of monounsatur
ated to saturated fatty acids with decreasing grain size, pointing to
an increasing microbial contribution. Particularly interesting is phyt
ol, which demonstrated a remarkable grain size effect; the phytol to B
OC ratio increased sharply with decreasing particle size. Major sterol
s normalized to BOC increased progressively with a decrease in grain s
ize and correlated highly with BOC. The results indicate that a plankt
on contribution to phytol and sterols increased as particle size decre
ased. The grain size effect is stronger for phytol than for sterols an
d branched-chain fatty acids in the sediments.