Swarms of Dioithona oculata, shoals of Mysidium columbiae, and schools
of planktivorous fish were observed among mangrove prop roots on a la
goonal island. Detritus covering epiphytic and benthic macroalgae and
invertebrates was a probable food source for pelagic mysids, and copep
ods, as well as benthic oysters and sponges. Open water blooms of dino
flagellate Amphidinium klebsii were probably only accessible to the sw
arming dioithonans which spend the night away from the mangrove prop r
oots. Dominant species were analyzed for stable carbon isotopic compos
ition (expressed as deltaC-13 parts per thousand) to elucidate the ori
gin and fate of detritus. Detrital components (-23.6 to -19.1 parts pe
r thousand), which included floating detritus, marine snow, prop root
detritus, and detritus below prop roots, probably originated from the
dominant subtidal macroalgal species (-24.2 to -14.6 parts per thousan
d) and A. klebsii (-25.8 to -21.2 parts per thousand), although other
sources which are end-members could theoretically contribute since det
rital isotopic ratios are half way between end-members. These other so
urces include the intertidal red algal Bostrychia spp. (-30.9 to -29.6
parts per thousand), red mangrove Rhizophora mangle leaves (-28.2 to
-27.0 parts per thousand), and turtle grass Thalassia testudinum (-12.
3 to -11.1 parts per thousand). Particle feeders such as mangrove oyst
ers, sponges, mysids, and dioithonans were usually enriched with C-13(
-21.0 to -16.2 parts per thousand) compared to their probable food sou
rces, detritus and A. klebsii. At Anchovy Bay, adult mysids and plankt
ivorous fish were more C-13 enriched (1-3 parts per thousand) than the
ir probable prey, the dioithonans. Turtle grass may have a minor role
in food webs, since dioithonans and mysids from Outer Twin and Anchovy
Bays where turtle grass beds were abundant were consistently more C-1
3 enriched (2-7 parts per thousand) than in the Lair Channel where tur
tle grass beds were sparse.