Novel esters of carotenols and chlorins (carotenol chlorin esters, CCEs) we
re found in recent sediments from the California Borderlands, Monterey Bay,
and the Peru and Oman margins. The chlorins associated with CCEs were pheo
phorbide a and pyropheophorbide a, degradation products of chlorophyll a. I
sofucoxanthin-dehydrate and isofucoxanthinol-dehydrate and possibly their i
somers, degradation products of fucoxanthin, were the only carotenols assoc
iated with CCEs. This result is surprising, considering that at least 8 maj
or degradation products of fucoxanthin are present in organic-rich marine s
ediments. The carotenols of CCEs are likely derived from diatoms as these a
re the primary source for fucoxanthin in the marine environment. In sedimen
ts studied by us, CCEs contributed approximately 10% to total solvent extra
ctable chlorins. The high relative concentrations of CCEs in these sediment
s suggest that CCEs are an important degradation product of chlorophyll a i
n some marine environments; a pathway hitherto unrecognized. Off Oman and S
outhern California we found CCEs in water column suspended particulate matt
er when diatoms dominated the phytoplankton community. By analogy with ster
ol chlorin esters, we suggest that CCEs are primarily produced by enzymatic
ally mediated transesterifications in crustaceans grazing on diatoms. We ar
e currently studying if CCEs are biomarkers for the grazing of crustaceans
on diatoms, an important pathway of carbon remineralization in the marine e
nvironment. (C) 1999 Elsevier Science Ltd.