Erimyzon oblongus
creek chubsucker
Type Locality
New York (Mitchill 1815).
Etymology/Derivation of Scientific Name
Erimyzon, Greek,
meaning “to suck”; oblongus, Latin, meaning “oblong” (Pflieger 1975).
Synonymy
Cyprinus oblongus
Mitchell1815:459
Erimyzon oblongus
claviformis Cook 1959:85.
Characters
Maximum size: The
maximum size reported length is 419mm (16.5 in) TL for the larger Atlantic
Slope subspecies (Carlander 1969). The Mississippi River and Gulf Slope
subspecies is smaller with a maximum reported size of 376mm (14.8 in) TL (Boschung
and Mayden 2004); however most adult fish are smaller (Ross 2001).
Coloration: Color
pattern (except in young with two dark stripes) consists of narrow vertical
bars (Hubbs et al. 1991). The back and upper sides are bluish green to
brown, becoming more yellow or gold on the sides. The undersides are white
to yellow. Scale margins are dark giving the upper sides a cross-hatched
appearance. There are five to eight dark blotches on the sides, which are
connected by dorsal saddles. The blotches vary from being very distinct
vertical bars (especially in young fish) to indistinct or coalesced into a
lateral band (in adults). Paired and median fins are yellow orange to gray,
and median fins tend to be darker then paired fins. Young fish have a broad
black lateral stripe with a yellow stripe above it that runs from the snout
to the tip of the caudal fin base. Breeding males are dark brown above,
pink-yellow, below, with orange paired fins and yellow median fins (Ross
2001).
Counts: 56-76
pharyngeal teeth (Eastman 1977); 39-43 (usually 39-41) longitudinal scale
rows; 4-18 dorsal fin rays (Hubbs et al. 1991); 7 anal rays; 13-16 pectoral
rays; 9 (8-9) pelvic rays (Ross 2001).
Body shape:
Cylindrical (Ross 2001); eye smaller (eye length contained more then two
times snout length; Hubbs et al. 1991).
Mouth position:
Subterminal and oblique (Hubbs et al. 1991).
External morphology:
Air bladder with two chambers; dorsal fin base less than one-fourth standard
length; lateral line absent (Hubbs et al. 1991). Breeding males have three
large tubercles on each side of head and a bilobed anal fin (Ross 2001).
Distribution (Native and Introduced)
U.S. distribution:
Atlantic slope streams from Maine to Altamaha drainage of Georgia; Gulf
slope streams east to Escambia River drainage, Alabama (single population)
and west to San Jacinto system Texas. Mississippi Valley in Louisiana,
Arkansas, southeast Oklahoma, upland Missouri, Mississippi, west Tennessee,
West Kentucky, south Great Lakes drainage in southern tributaries to lakes
Michigan, Erie, and Ontario (Wall and Gilbert 1980).
Texas distribution:
Occurs in eastern Texas streams from the Red River southward to the San
Jacinto Drainage; an early record exists from the Devils River (Hubbs et al.
1991).
Abundance/Conservation status (Federal, State, NGO)
Not listed as threatened or
endangered by Texas Parks and Wildlife Department
(2006). Populations in the
southern Unites States are currently stable (Warren et al. 2000). Hubbs et
al. (1991) listed Erimyzon oblongus as a species of special concern,
in Texas.
Habitat Associations
Macrohabitat: Occupies
small rivers and creeks often highly vegetated (Wall and Gilbert 1980), also
less often in ponds (Wagner and Cooper 1963).
Mesohabitat: Wide
variety of gradients, bottom types, and vegetation depending somewhat on age
and stage of reproductive cycle. Seldom if ever occupies impoundments or
springs, but may be taken in spring fed creeks. Young typically in head
water rivulets. Adults usually not taken in large series. Populations
apparently declining in streams subject to siltation (Wall and Gilbert
1980).
Biology
Spawning season: March
to May, when the water temperature reaches about 17 degrees C (Richardson
1913; Breder and Rosen 1966; Boschung and Mayden 2004). Carnes (1958) notes
the eastern subspecies spawns at water temperature of 11 degrees C, with
most activity at night. The western subspecies spawns at water temperatures
of 12-24 degrees C, spawning in the afternoon (Curry and Spacie 1984; Page
and Johnston 1990).
Spawning habitat:
Usually in small creeks, also in ponds or lakes that lack tributary streams
(Carnes 1958). In Indiana, small cleared depressions on the sand bottom of
pools just above riffles (Curry and Spacie 1984). Lithopelagophils;
rock and gravel spawners with benthic larvae that hide beneath stones
(Hankinson 1920; Page and Johnston 1990; Simon 1999).
Reproductive strategy:
Males guard spawning location (Curry and Spacie 1984). Hankinson (1920)
observed stone pulling by males and apparent acts of spawning. Prior to
spawning males defend territories in moderately swift water over beds of
gravel or near pits constructed by stonerollers or creek chubs. Males
apparently do not initiate the digging of nest pits, but will modify
existing pits by pushing stones around with their snouts. Females congregate
upstream of males in quiet water, periodically drifting tail first into male
territories. Once in a male’s territory, the female digs in the gravel with
her snout, apparently signaling to the male that she is ready to spawn. In
contrast to most species of suckers, pair spawning is much more common than
group spawning, perhaps due to the shallowness of the usual spawning
habitat. Actual spawning lasts three to five seconds as the male presses
against female. Both release gametes while quivering and stirring the
substratum with their caudal and anal fins (Page and Johnson 1990).
Fecundity: Fertilized
eggs of the eastern subspecies E. o. oblongus are demersal and
semiadhesive, with an average diameter of 1.8 mm; color varies from light to
deep golden yellow and yolk occupies most of egg; no oil drops in the yolk
mass; hatching occurs in 96 hours at a temperature of 20 degrees C (Kay et
al. 1994). Egg production varies from 8,694-83,013 in fish 111-1110 g
(Carnes 1958). Regardless of high fecundity this species is not found in
high numbers (Boschung and Mayden 2004).
Age at maturation:
Migration: An upstream
migration often precedes spawning (Breder and Rosen 1966).
Growth and population
structure: For the western subspecies E. o. claviformis TL
averages 48-51 mm after one year and 104-107mm at end of the second year
(Lewis and Elder 1953; Carlander 1969). There is no sexual dimorphism in
size (Ross 2001). Newly hatched protolarvae are 4.8-6.6 mm TL (Kay et al.
1994).
Longevity: Females may
live for 6 or 7 years, though males only live for 5 years (Carnes 1958;
Wagner and Cooper 1963; Carlander 1969).
Food habits:
Invertivore; major food items include copepods, cladocerans, chironomid
larvae and other bottom organisms (Goldstein and Simon 1999). Diet includes
organic detritus (including plant fragments), algae, diatoms, midge larvae
(Diptera), small clams, and zooplankton (primarily copepods). Food habits
are similar to E. sucetta, the lake chubsucker (Flemmer and Woolcott
1966; Gatz 1979; Sheldon and Meffe 1993). Feeding begins 7.4 days after
hatching at a length of 7.7 mm TL (Kay et al. 1994).
Phylogeny and morphologically similar fishes:
Two subspecies recognized,
E. o. claviformis, which occurs in the Gulf of Mexico and Mississippi
River Basins, and the Atlantic Slope subspecies E. o. oblongus (Wall
and Gilbert 1980). E. oblongus is most closely related to E.
sucetta, and two species are known to hybridize (Hanley 1977). The genus
Erimyzon is most closely related to Minytrema, and both genera
are placed within the tribe Moxostomatini (Smith 1992).
Erimyzon oblongus is
most similar to the lake chubsucker. It differs from the lake chubsucker in
its higher lateral scale count (usually 39-40 or more versus 37 or fewer)
and its lower dorsal ray count (10-11 versus 11-12). (Gilbert and Wall
1985). Compared to lake chubsuckers, creek chubsuckers have more cylindrical
bodies, lighter colored fins and less deeply emarginated caudal fins (Ross
2001).
Host Records:
Cestoda: Monobothrium sp.
Biacetabulum sp. (Arnold et. al 1967); Acanthocephala:
Neoechinorhynchus prolixoides, Crustacea: Lernaea cyprinacea
(Hoffman 1967).
Commercial or Environmental Importance
References
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