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Monograph 22
4290206 Notes of the NorNthOeRNTaHosrEtthAeeSraTnsEte RNrnN aNNatAtuuTrUraaRliAsltiLsIStT, Issue 14/3, 2V10o3l0.( 1174):,3 N9–o4. 23
First Record of Central Stoneroller (Campostoma anomalum) in
the Tidal Hudson River
Robert E. Schmidt1,*, Richard Morse2, and Bryan Weatherwax2
Abstract - We document the discovery of Campostoma anomalum (Central Stoneroller) in the
tidal mouth of the Poestenkill, a Hudson River tributary in Troy, NY. This is the first record of
the species from a tidal habitat and is a range extension of approximately 68 km downstream
from the Mohawk River.
Campostoma anomalum (Rafinesque) (Central Stoneroller) is a small minnow
(Cyprinidae) native to the Mississippi Valley and adjacent drainages (Lee et al. 1980
et seq.). This species is known from the Mohawk River (Smith 1985), the largest
Hudson River tributary, but there is consensus that the Mohawk River populations
are not native (Carlson and Daniels 2004, Schmidt 1986, Smith and Lake 1990).
Central stoneroller was not present in the Mohawk River in the 1930s (Smith and
Lake 1990) and probably moved through the renovated Barge Canal within the last
40 years (Carlson and Daniels 2004, Daniels 2001). Labidesthes sicculus Cope
(Brook Silverside) followed the same route (Marsden et al. 2000) and is now
established in the tidal Hudson River (Daniels et al. 2005). The purpose of this paper
is to document range expansion of Central Stoneroller to the tidal Hudson River.
We collected a single specimen of Central Stoneroller from the Poestenkill in
Troy, NY on May 25, 2005 in shallow water (less than 1 m deep) over cobble substrate with
a backpack electroshocker. The specimen was measured with a digital calipar to be
46.0 mm SL (NYSM 58486; Fig. 1.) The Poestenkill is the northernmost tributary to
the tidal Hudson River. Its mouth is 1.9 km south of the Federal Dam at Troy, the
upstream limit of tidal influence. The Central Stoneroller was collected about 20 m
downstream (west) of the First Street Bridge in a tidally influenced riffle.
Smith (1985) did not list Central Stoneroller from tributaries to the tidal Hudson
River, although Carlson and Daniels (2004) indicated that there were records of this
species in the area. We sampled the two tributaries (Mill Creek and Moordener Kill,
Rensselaer County) where Central Stoneroller was recorded in the 1960s (D.
Carlson, NY Department of Environmental Conservation, Waterown, NY, pers.
comm.) and found no stoneroller in June 2005. We conclude that these early records
were identification errors.
This is the first report of this species in tidal water. The tidal Hudson River is
completely freshwater in the vicinity of Troy, and brackish water is rarely detected
within 145 km of the mouth of the Poestenkill (Cooper et al. 1988). This record is
Figure 1. Photograph of a preserved Campostoma anomalum (Central Stoneroller) collected in
tidal riffles of the Poestenkill, Troy, NY (NYSM 58486).
492
2007 Notes 493
approximately 42 km downstream of the closest recorded population of Central
Stoneroller in the Mohawk River (Smith 1985).
Central stoneroller feeds by scraping algae and other organisms from the surface
of rocks, usually in flowing water (Smith 1985). There may not be very much habitat
for this species in the main Hudson River estuary, but many of the tributary streams
would have suitable habitat. Central stoneroller, therefore, has the potential to spread
throughout the upper tidal Hudson River system, as it has in the Mohawk River.
Smith (1985) said, “The stoneroller is a rather undistinguished minnow….”
The best field character is the presence of a hard cartilaginous ridge protruding
beyond the lower lip. We urge anyone sampling small fishes in the Hudson River
estuary and the upper Hudson watershed to look for this character on otherwise
ordinary-looking minnows, perhaps most closely resembling Rhinichthys spp.
(Blacknose or Longnose Dace).
Central stoneroller joins several species that have invaded the tidal Hudson River
from the Mohawk River, probably in this century. Brook Silverside, Moxostoma
macrolepidotum (Lesueur) (Shorthead Redhorse), and Aplodinotus grunniens
Rafinesque (Freshwater Drum) are now established in the Hudson estuary, although
redhorse spawning has not been documented (Schmidt and Lake 2006).
Other Mohawk River species may be moving into the Hudson River in the future.
Nocomis biguttatus (Kirtland) (Hornyhead Chub), Noturus flavus Rafinesque
(Stonecat), Etheostoma flabellare Rafinesque (Fantail Darter), and Etheostoma
blennioides Rafinesque (Greenside Darter) are each common in some areas of the
Mohawk River, and Noturus miurus (Richardson) (Brindled Madtom) has been
collected between the locks in the Barge canal in Waterford (NYSM 51208) and
could easily reach the tidal Hudson River.
This individual was probably starting its second summer according to sizes
reported by Trautman (1957). Since we only caught one specimen, we have little
evidence that the species is established. We view this record as a dispersal event
and an instance of further homogenization of the Hudson River fish fauna which
mimics the larger scale homogenization of fishes in New York (Carlson and
Daniels 2004) and North America in general (Rahel 2000). This local homogenization
of the fauna is due to human alterations to the watershed and is occurring
over the span of decades.
It is interesting to note the dispersal of small fishes like the Central
Stoneroller. The spread of a small species through a large watershed on a decadal
scale has implications for the rapidity of dispersal among watersheds on much
longer time scales.
Acknowledgments. We thank Gay Malin for helping us with photography.
Literature Cited
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1Bard College at Simons Rock, 84 Alford Road, Great Barrington, MA 01230-1978. 2Biological
Survey Laboratory 145 Jorddan Road, Troy, NY 12180. *Corresponding author -
schmidt@simons-rock.edu.