Synonymy:
None
Other Taxonomic Groupings:
Suborder: Anasca
Potentially Misidentified Species:
C. seurati
could be mistaken for C. tenuissimum. However, the budding pattern in C.
tenuissimum is slightly more regular than in C. seurati due to C.
tenuissimum's somewhat larger zooid size and distal-proximal budding
pattern. Additionally, lateral walls in individual zooids are more calcified in C.
seurati, and its distal spines are longer and more pointed. C. seurati
has fewer lateral spines than C. tenuissimum in water of the same
salinity: 1 - 3 for C. seurati vs. 5 for C. tenuissimum.
II. HABITAT AND
DISTRIBUTION
Regional Occurrence:
C. seurati typically
occurs in Northern Europe and the Mediterranean. Prior to Winston's 1982 study,
this species had not been reported in the western hemisphere. Its range now
includes estuarine habitats on Florida's east coast.
IRL Distribution:
C. seurati is likely to be widespread in the
IRL, but it has been primarily collected from Link Port (Winston 1982).
III. LIFE HISTORY AND POPULATION BIOLOGY
Age, Size, Lifespan:
Individual zooids measure an average of 0.55 X 0.33
mm in size. Lophophore diameter measures 0.621 on average.
Abundance:
C. seurati is
among the most abundant bryozoan species in the IRL. It is most common from
December through May (Winston 1982). In the IRL, it is considered a fouling
organism (Winston 1995).
Locomotion:
Sessile
Reproduction:
No ovicells are present in this species and eggs
are not brooded. Reproduction is accomplished by releasing eggs into the water
column for fertilization. Peak reproductive season occurs from late winter to
early spring.
C. seurati and C.
tenuissimum co-occur in estuarine habitats, but their reproductive seasons
are apparently offset. During December, when C. tenuissimum larvae are
settling in their greatest numbers, they can outnumber C. seurati by
a ratio of 99:1. However, throughout January, settlement rates between both
species tend to equalize, and by May, only C. seurati is still settling.
Embryology:
After fertilization, embryos develop into
planktonic larvae.
IV. PHYSICAL TOLERANCES
Temperature:
C. seurati is
considered a winter species in the IRL, being most common from December through
May (Winston 1982, 1995).
Salinity:
C. seurati is
one of 3 truly estuarine bryozoan species in the Indian River Lagoon. It was not
collected from coastal stations, but was routinely collected in the IRL in
waters where salinity ranged between 18 - 40 ‰ (Winston 1982, 1995). In
Europe, it has been collected in estuaries where salinity is less than 1 ‰
(Winston 1982).
V. COMMUNITY ECOLOGY
Trophic Mode:
C. seurati,
like all bryozoans, is a suspension feeder. Each individual zooid in a colony
has an average of 15 ciliated tentacles that are extended to filter
phytoplankton less than 0.045 mm in size (about 1/1800 of an inch) from the
water column. Bullivant ( 1967; 1968) showed that the average individual zooid
in a colony can clear 8.8 ml of water per day.
Competitors:
Winston (1982) reported that C. seurati may
be a better space competitor than C. tenuissimum, because its colonies
were often observed to overgrow C. tenuissimum.
Habitats:
Typical habitat for ectoprocts in the Indian River
Lagoon include seagrasses, drift algae, oyster reef, dock, pilings, breakwaters,
and man-made debris (Winston 1995).
Associated Species:
Seagrasses as well as floating macroalgae, provide
support for bryozoan colonies. In turn, bryozoans provide habitat for many
species of juvenile fishes and their invertebrate prey such as polychaete worms,
amphipods and copepods (Winston 1995). Bryozoans are also found in association
with other species that act as support structures: mangrove roots, oyster beds,
mussels, etc.
VI. SPECIAL STATUS
Special Status:
None.
Benefit in IRL:
Bryozoans are ecologically important in the Indian
River Lagoon due to their feeding method. As suspension feeders, they act as
living filters in the marine environment. For example, Winston (1995) reported
that bryozoan colonies located in 1 square meter of seagrass bed could
potentially filter and recirculate
an average of 48,000 gallons of seawater per day.
Economic Importance:
None
Report by: K. Hill,
Smithsonian Marine Station
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Page last updated: July 25, 2001
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