The ophiuroid Amphiodia urtica LYMAN is presently under study as a pot
ential wastewater discharge indicator species from ocean outfalls in t
he Southern California Eight. On the San Pedro Shelf, the maximum abun
dance of A. urtica was found at depths from 30 to 100 m, and in sedime
nt with a median grain size of 0.085 mm, 60-80% sand, 15-30% silt, 0-3
7% clay, and 0.2-0.5% TOC. The mean abundance of A. urtica fluctuated
annually with a slight increase from 1977 through 1993. The hypothesis
was posed that the distribution and abundance of A. urtica is not inf
luenced by an ocean outfall and its operation on the San Pedro Shelf B
ased on long-term (1977-1994) and intensive (2860 samples) sampling, t
he hypothesis was rejected. However, the effect of the outfall is not
clear because sediment bioassays from test stations and controls produ
ced no significant differences in survivorship and growth of juveniles
. Amphiodia presently occupies areas within the Zone of Initial Diluti
on (ZID) where it was not found during the mid-1970s and early 1980s.
While recognizing that A. urtica abundance responds to proximity to th
e outfall, the mechanism for this response is still unclear. The appli
cation of a single species as a bioindicator is not recommended, and m
ost certainly not without fully assessing its role in community struct
ure and function.