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+The Project Gutenberg EBook of Geographic Variation in the North American
+Cyprinid Fish, Hybopsis gracilis, by Leonard J. Olund and Frank B. Cross
+
+This eBook is for the use of anyone anywhere at no cost and with
+almost no restrictions whatsoever. You may copy it, give it away or
+re-use it under the terms of the Project Gutenberg License included
+with this eBook or online at www.gutenberg.org
+
+
+Title: Geographic Variation in the North American Cyprinid Fish, Hybopsis gracilis
+
+Author: Leonard J. Olund
+ Frank B. Cross
+
+Release Date: December 27, 2011 [EBook #38425]
+
+Language: English
+
+Character set encoding: ASCII
+
+*** START OF THIS PROJECT GUTENBERG EBOOK GEOGRAPHIC VARIATION ***
+
+
+
+
+Produced by Chris Curnow, Joseph Cooper, Erica
+Pfister-Altschul and the Online Distributed Proofreading
+Team at http://www.pgdp.net
+
+
+
+
+
+
+
+ UNIVERSITY OF KANSAS PUBLICATIONS
+ MUSEUM OF NATURAL HISTORY
+
+ Volume 13, No. 7, pp. 323-348, pls. 21-24, 2 figs.
+
+ February 10, 1961
+
+
+
+
+ Geographic Variation
+ In the North American Cyprinid Fish,
+ Hybopsis gracilis
+
+ BY
+
+ LEONARD J. OLUND AND FRANK B. CROSS
+
+
+ UNIVERSITY OF KANSAS
+ LAWRENCE
+ 1961
+
+
+ UNIVERSITY OF KANSAS PUBLICATIONS, MUSEUM OF NATURAL HISTORY
+
+ Editors: E. Raymond Hall, Chairman, Henry S. Fitch,
+ Robert W. Wilson
+
+
+ Volume 13, No. 7, pp. 323-348, pls. 21-24, 2 figs.
+ Published February 10, 1961
+
+
+ UNIVERSITY OF KANSAS
+ Lawrence, Kansas
+
+
+ PRINTED IN
+ THE STATE PRINTING PLANT
+ TOPEKA, KANSAS
+ 1961
+
+ [Illustration]
+
+ 28-5871
+
+
+
+
+Geographic Variation
+In the North American Cyprinid Fish,
+Hybopsis gracilis
+
+BY
+
+LEONARD J. OLUND AND FRANK B. CROSS
+
+
+
+
+CONTENTS
+
+
+ PAGE
+
+ INTRODUCTION 325
+
+ METHODS, MATERIALS, AND ACKNOWLEDGMENTS 326
+
+ DESCRIPTION OF THE SPECIES HYBOPSIS GRACILIS 327
+ _Hybopsis gracilis gracilis_ 328
+ _Hybopsis gracilis gulonella_ 330
+
+ INTRASPECIFIC VARIATION 333
+
+ NATURAL HISTORY 334
+ _Habitat_ 334
+ _Associated Species_ 336
+ _Food_ 338
+ _Spawning Season_ 338
+
+ DISCUSSION 340
+
+ LITERATURE CITED 343
+
+
+
+
+INTRODUCTION
+
+
+The flathead chub, _Hybopsis gracilis_ (Richardson), occurs in the
+Plains Region of Canada and the United States, in four major drainage
+systems: Mackenzie River, which discharges into the Arctic Ocean;
+Saskatchewan River, which discharges into Hudson Bay via Nelson River;
+and Missouri-Mississippi System and Rio Grande, both draining into the
+Gulf of Mexico. Each of these systems is occupied in part only. In the
+Mackenzie Basin, _H. gracilis_ has been reported as far north as Fort
+Good Hope (Walters, 1955:347). Flathead chubs occur in the Saskatchewan
+Basin from Alberta eastward to Lake Winnipeg, Manitoba, but have not
+been found in other streams that flow into Lake Winnipeg (Red River,
+Brokenhead River and Whitemouth River) nor in Nelson River downstream
+from Lake Winnipeg. In the Missouri Basin the species occurs more or
+less continuously from the high plains adjacent to the Rocky Mountains
+in Montana and Wyoming down the mainstream of the Missouri River to its
+mouth, and down the mainstream of the Mississippi River as far as
+Barfield, Arkansas, but not to the Gulf. The species probably attains
+its greatest abundance in the Missouri Basin, but it is scarce or absent
+in tributaries north and east of the Missouri mainstream, in the South
+Platte Basin, and in the central part of the Platte River in Nebraska.
+The flathead chub is unknown in the Mississippi Basin above the mouth of
+the Missouri River, and in the Ohio River Basin above its mouth. In the
+Arkansas River Basin, records are restricted to (1) the headwaters and
+tributaries of the Arkansas River from eastern Colorado downstream as
+far as Garden City, Kansas, (2) the Cimarron River at Kenton, Cimarron
+County, Oklahoma, and (3) the South Canadian River and tributaries from
+northeastern New Mexico eastward as far as Norman, McClain County,
+Oklahoma, but rarely there. Thus, the range in the Arkansas Basin seems
+to consist of three isolated segments. Likewise, isolated populations
+exist in the Rio Grande System, where flathead chubs are confined to the
+upper parts of the Rio Grande and Pecos basins, above the confluence of
+the Rio Grande and Pecos Rivers. Records resulting from introductions
+have been reported for the Gila River by Koster (1957:62) and from the
+Snake River, Wyoming, by Simon (1946:72).
+
+Six names apply to the flathead chub, the earliest of which is _Cyprinus
+gracilis_ Richardson (1836:120). Other names have sometimes been
+accepted as applicable to valid species and/or subspecies, but usage,
+diagnoses, and stated ranges have been confusingly inconsistent. For
+most of the past 100 years, _Platygobio_ Gill has been recognized as the
+appropriate generic name for the flathead chub, but Bailey (1951:192)
+places _Platygobio_ and other nominal genera of barbeled minnows having
+short guts, protractile premaxillae, and four teeth (primary row) in the
+single genus _Hybopsis_ (Agassiz, 1854). Strangely, the orthotype of
+_Hybopsis_, _H. gracilis_ Agassiz, is a junior synonym of _H. amblops_
+(Rafinesque) (Hubbs and Ortenburger, 1929b:66) and is a younger name
+than _C. gracilis_ Richardson.
+
+The purpose of this paper is to redescribe the species and to make known
+its pattern of geographic variation. Natural history will also be
+considered, as will habitat, food habits, and breeding season.
+
+
+
+
+METHODS, MATERIALS AND ACKNOWLEDGMENTS
+
+
+Ten meristic characters and seventeen measurements of body-parts (the
+latter expressed as proportions of standard length) have been analyzed.
+They are: number of rays in the dorsal, anal, caudal, pectoral and
+pelvic fins; number of scales in the lateral line, before the dorsal
+fin, around the body and around the caudal peduncle; number of
+vertebrae; body-depth, depth of caudal peduncle, length of caudal
+peduncle, predorsal length, length of depressed anal and dorsal fins,
+length of pectoral and pelvic fins, head-length, head-depth,
+head-width, snout-length, postorbital length of head, length of orbit,
+interorbital width, length of upper jaw and width of gape.
+
+Counts and measurements were made as described by Hubbs and Lagler
+(1958), with the exception of scales before the dorsal fin, which were
+counted as the number of vertical scale-rows between the upper margin of
+the opercular cleft and the origin of the dorsal fin. Vertebral counts,
+made from roentgenograms, excluded vertebrae in the Weberian complex
+(presumably always four) but included the hypural vertebra.
+
+Counts and measurements were made on series (usually ten fish) from
+localities throughout the range. To minimize effects of allometric
+growth, the fish were divided into several length-groups prior to
+analysis of proportional measurements: 30-50mm, 50-70mm, 70-100mm,
+100-150mm, 150-200mm and 200mm standard length and over. The majority of
+specimens examined were 70-100mm in standard length.
+
+Specimens were obtained from the following institutions: University of
+Alberta (abbreviated UA in the text); Museum of Zoology, University of
+Michigan (UMMZ); University of Missouri (UM); Montana State College
+(MSC); University of Oklahoma Museum of Zoology (UOMZ); University of
+Saskatchewan; Royal Ontario Museum, Division of Zoology, Toronto (ROMZ);
+University of Wyoming (WU); Museum of Natural History, University of
+Kansas (KU). Specimens examined are listed in the accounts of the
+subspecies.
+
+We are grateful to D. A. Boag, Reeve M. Bailey, Arthur L. Witt, C. J. D.
+Brown, Carl Riggs, F. M. Atton, W. B. Scott, and George Baxter, all
+staff-members of the institutions listed in the immediately preceding
+paragraph, for placing specimens at our disposal. Mr. William Peters
+analyzed the contents of stomachs of specimens that were used for study
+of the food habits. Mr. Artie L. Metcalf assisted in collecting
+specimens. Drs. Kenneth B. Armitage and E. Raymond Hall offered valued
+suggestions in connection with the preparation of the manuscript.
+
+
+
+
+DESCRIPTION OF THE SPECIES
+
+
+=Hybopsis gracilis= (Richardson)
+
+Flathead Chub
+
+(Synonymy under accounts of subspecies)
+
+_Description._--Pharyngeal teeth 2,4-4,2, hooked; dorsal fin of
+moderate size, falcate, first principal ray longest, extending beyond
+posterior rays in depressed fin, its origin usually slightly in front
+of insertion of pelvic fin, approximately equidistant from tip of snout
+and base of caudal fin, rays 8, rarely 9; pectoral fin strongly
+falcate, rays 14-20, usually 16-18; pelvic rays 8, rarely 9; anal fin
+falcate, rays 8, rarely 9; caudal rays 19, rarely 20.
+
+Body slightly compressed, nearly terete; head-length 23.1-28.8 per cent
+of standard length; head broad and flattened, snout subconical,
+premaxillae protractile, upper lip not medially expanded; mouth
+subterminal, nearly horizontal, large; a single pair of terminal
+maxillary barbels; orbit usually 5-7 per cent of standard length;
+lateral line slightly decurved; intestine short, peritoneum silvery.
+
+Color brown or olivaceous dorsally, silver or creamy white ventrally,
+without distinctive markings; dusky lateral band evident in preserved
+specimens.
+
+Taste-buds present on membrane between first and second principal rays
+of all fins, and on first to sixth interradial membranes of pectoral
+fin. On the caudal fin, taste buds between first and second principal
+rays of upper and lower lobes, though present, are less well developed
+than on other fins. Moore (1950:88) states that taste buds are numerous
+on the barbels, cheeks, lips, chin, snout, opercles and branchial
+membranes, and are present in decreasing numbers over the body.
+
+Nuptial tubercles of male minute and densely scattered over top of head
+and snout; usually present on pectoral rays 1-8, weak when present on
+rays beyond the eighth, never found beyond the eleventh ray; minute
+tubercles usually found on dorsal, pelvic and anal fins, rarely on lower
+scales of caudal peduncle; predorsal scales have a fine peripheral row
+of tubercles.
+
+
+=Hybopsis gracilis gracilis= (Richardson)
+
+(Plate 22)
+
+ _Cyprinus (Leuciscus) gracilis_ Richardson, 1836:120 and Pl. 78
+ (original description; Saskatchewan R. at Carlton House).
+
+ _Coregonus angusticeps_ Cuvier and Valenciennes, 1848:534
+ (original description; Saskatchewan R.).
+
+ _Pogonichthys communis_ Girard, 1856:188 (in part; original
+ description); Girard, 1858:247 and plate 55 (in part;
+ characters; synonymy); Suckley, 1860:361 (Milk R.); Cope,
+ 1879:440 (Fort Benton, Mo. R.; Judith R.).
+
+ _Platygobio gracilis_, Jordan and Gilbert, 1882:219 (in part;
+ characters; synonymy); Graham, 1885:74 (Kansas R.; synonymy);
+ Jordan, 1885:29 (records); Jordan and Meek, 1886:13 (Mo. R., St.
+ Joseph, Mo.); Meek, 1892:245 (characters; Mo. R., Sioux City,
+ Iowa); Eigenmann, 1895:111 (Craig; Poplar; Brandon; Medicine
+ Hat); Meek, 1895:137 (Platte R., Fremont, Neb.); Evermann and
+ Cox, 1896:412 (in part; habitat; synonymy); Jordan and Evermann,
+ 1896:326 (in part; characters; synonymy); Thompson, 1898:214
+ (Brandon; Saskatchewan R.); Evermann and Goldsborough, 1907:98
+ (records from Canada); Forbes and Richardson, 1920:170
+ (characters; habitat; synonymy; records from Illinois; but Fig.
+ 45 is _Hybopsis meeki_ Jordan and Evermann, not _H. gracilis_);
+ Hankinson, 1929:446 (records from North Dakota); Jordan, 1929:76
+ (in part; characters); Jordan, Evermann and Clark, 1930:136 (in
+ part; synonymy); Churchill and Over, 1933:45 (characters; food;
+ habitat; spawning; records from South Dakota); O'Donnel,
+ 1935:481 (Ohio R., Cairo, Ill.; Miss. R., Chester, Ill.); Hinks,
+ 1943:57 (records from Canada); Clemens, _et al._, 1947:17
+ (records from Saskatchewan); Dymond, 1947:19 (distribution in
+ Canada); Rawson, 1951:208 (Great Slave Lake; Mackenzie R.);
+ Shoemaker, Pickering and Durham, 1951:84 (Miss. R., Cates, Tenn.;
+ Miss. R., between Hickman and Barfield, Ark.); Wynne-Edwards,
+ 1952:18 (distribution in Canada); Miller and Paetz, 1953:47
+ (Peace R. at town of Peace River); Walters, 1955:347
+ (distribution in Canada; dispersal into Canada); Keleher,
+ 1956:265 (Saskatchewan R., Manitoba); Lindsey, 1956:771
+ (distribution in Canada); Keleher and Kooyman, 1957:110 (Kelsey
+ Lake, Manitoba); Lindsey, 1957:657 (Laird and Peace drainages,
+ British Columbia); Scott, 1958:16 (distribution in Canada);
+ Slastenenko, 1958:7 (distribution in Canada).
+
+ _Platygobio pallidus_ Jordan and Gilbert, 1882:220 (original
+ description; Ohio R., Cairo, Ill.); Jordan and Evermann,
+ 1896:326 (characters; synonymy; Ohio R., Cairo, Ill.); Jordan,
+ Evermann and Clark, 1930:136 (Ohio R., Cairo, Ill.; synonymy).
+
+ _Platygobio gracilis communis_, Simon, 1946:71 (in part;
+ characters; food; habitat; spawning); Moore, 1950:87 (habitat;
+ sense organs).
+
+ _Hybopsis gracilis communis_, Bailey, 1951:192 (record from Iowa;
+ key); Harlan and Speaker, 1951:75 (characters; distribution in
+ Iowa); Hubbs, 1951:9 (habitat; Miss. R.); Harrison and Speaker,
+ 1954:516 (habitat); Personius and Eddy, 1955:42 (habitat; Little
+ Mo. R.).
+
+ _Hybopsis gracilis_, Cleary, 1956:271 (record from Iowa;
+ distributional map); Bailey, 1956:332 (record from Iowa; key);
+ Harlan and Speaker, 1956:90 (characters; distribution in Iowa);
+ Eddy, 1957:111 (in part; characters; key); Moore, 1957:110 (in
+ part; key); Underhill, 1959:100 (Vermillion R., South Dakota).
+
+_Diagnosis._--Post-Weberian vertebrae 40-42, usually 41-42; lateral
+line scales 50-56; pectoral rays 15-20, usually 17 or more; head-depth
+12.3-15.1 per cent of standard length, usually 14.7 per cent or less.
+See Figs. 1 and 2.
+
+_Other characters._--Circumference scale-rows 31-42; predorsal
+scale-rows 20-29; size large, as much as 246 mm standard length (see
+Fig. 1 of Pl. 24); head-length 23.4-27.4 per cent of standard length,
+usually 25.5 per cent or less; postorbital length of head 10.9-13.9 per
+cent of standard length, usually 12.5 per cent or less; predorsal length
+46.0-51.7 per cent of standard length; orbit 5.1-6.8 per cent of
+standard length; prepelvic length 46.6-52.2 per cent of standard length;
+caudal peduncle length 17.2-22.1 per cent of standard length.
+
+_Range_ (Plate 21).--Mackenzie Basin south from Fort Good Hope;
+Saskatchewan Basin east to Lake Winnipeg; mainstream of Missouri River
+and Mississippi River south to Barfield, Arkansas; intergrading with _H.
+g. gulonella_ in upper Missouri Basin and lower parts of major
+tributaries to Missouri River in Nebraska and Kansas.
+
+_Specimens examined._--Below are listed museum numbers, number of
+specimens (in parentheses), localities, and year of collection.
+Collections marked with asterisk (*) are intergrades more closely
+resembling _H. g. gracilis_ than _H. g. gulonella_. Records from
+literature are cited in the synonymy.
+
+ALBERTA: UA (6), Milk R. at town of Milk River, 1950; UA (3), Athabasca
+R. at Fort McMurray, 1955; UA (1), Red Deer R. at Steveville, 1952; UA
+(2), Peace R. at town of Peace River, 1952; UA (11), Peace R. at
+Dunvegan, 1956; UA (2), Simonette R. tributary to Smoky R., date
+unknown; ROMZ 17704 (1), Milk R. W town of Milk River, 1955.
+
+ARKANSAS: UMMZ 128573 (5), Mississippi Co., Mississippi R., 1939.
+
+ILLINOIS: UMMZ 134799 (146), Mississippi R. at Grand Tower, 1936; UMMZ
+147045 (8), Mississippi R. at Cairo, 1944.
+
+KANSAS: KU 1234 (173), Leavenworth Co., backwater of Missouri R. near
+Corral Cr., 1940; * KU 1814 (1), Douglas Co., floodpool of Kansas R.,
+below Lakeview, 1951; * KU 1825 (1), Douglas Co., floodpool of Kansas
+R., 1951; * KU 1841 (56), Douglas Co., Kansas R. at Lawrence, 1951; * KU
+1898 (6), Douglas Co., floodpool of Kansas R., 1951; * KU 1911 (5),
+Douglas Co., floodpool of Kansas R., 1951; * KU 1928 (2), Jefferson Co.,
+floodpool of Kansas R., 1951; KU 3850 (30), Atchison Co., Missouri R.,
+1957; * KU 4377 (2), Douglas Co., Kansas R. at Lawrence, 1958; * KU 4655
+(2), Douglas Co., Kansas R. at Lawrence, 1959.
+
+MANITOBA: ROMZ 13834 (1), Kelsey Lake, 25 miles east of the Pas, no
+date; ROMZ 14500 (25), Saskatchewan R. at the Pas, 1947; ROMZ 16325 (1),
+Lake Winnipeg, no date.
+
+MISSOURI: UMMZ 147126 (130), Mississippi R. at Cliff Cave, 1944.
+
+MONTANA: * MSC 1878 (36), Carbon Co., Elbow Cr., 1957; * MSC 1943 (11),
+Phillips Co., Frenchman Cr., 1957; * MSC 2021 (10), Pondora Co., Marias
+R., 1955; * MSC 2022 (4), Lewis and Clark Co., Missouri R. below Holter
+Dam, 1948; * MSC 2052 (6), Gallatin Co., Missouri R. near Trident, 1948;
+* MSC 3074 (3), Custer Co., Hardy Reservoir, 1952; UMMZ 94146 (34), near
+mouth of Powder R., 1926.
+
+NEBRASKA: * KU 4158 (9), Holt Co., Niobrara R. 6 mi. N Midway, 1958; *
+UM (field no. 59-81) (56), Butler Co.-Colfax Co. line, Platte R. 1.5 mi.
+S Schuyler, 1959; * UM (field no. 59-74) (5), Dodge Co., Platte R. 1 mi.
+S North Bend, 1959; UMMZ 134826 (46), Otoe Co., Missouri R. 1.5 mi. E
+Minersville, 1940; UMMZ 134799 (67), Cass Co., Missouri R., 1940; UMMZ
+135341 (43), Knox Co., Missouri R. 2 mi. NE Niobrara, 1940; UMMZ 135818
+(95), Thurston Co., Missouri R. NE Macy, 1941.
+
+NORTHWEST TERRITORY: ROMZ 13627 (1), Great Slave Lake, no date; ROMZ
+13628 (1), Great Slave Lake, no date.
+
+SASKATCHEWAN: * ROMZ 3885 (2), Sucker Cr., trib. Cypress Lake, 1927;
+ROMZ 14368 (2), South Saskatchewan R. at Yorath Island, 1941; ROMZ 16620
+(5), South Saskatchewan R. at Saskatoon, 1953; KU 5126 (5), South
+Saskatchewan R. at Birson Ferry, 1957; KU 5127 (3), South Saskatchewan
+R. at Leader, 1957; KU 5128 (2), North Saskatchewan R. at Cecil Ferry,
+1957; KU 5129 (1), South Saskatchewan R. at Clarkboro Ferry, 1957.
+
+SOUTH DAKOTA: * KU 4961 (9), Haakon Co., Bad R. at Midland, 1959; * KU
+4963 (17), Washabaugh Co., White R. 6 mi. SW Belvidere, 1959; * UMMZ
+120362 (168), White R. 6.5 mi. S Kadoka, 1934; * UMMZ 127484 (11), Todd
+Co., Little White R., 1934; UMMZ 127488 (29), Charles Mix Co., Missouri
+R., 1934; * UMMZ 127678 (32), Cheyenne R., E Wasta, 1939; UMMZ 166762
+(21), Hughes Co., Missouri R. 3 mi. NE Pierre, 1952; * UMMZ 166803 (91),
+Harding Co., Little Missouri R. at Camp Crook, 1952; UMMZ 166845 (121),
+Carson Co.-Walworth Co. line, Missouri R. 2.5 mi. N Mobridge, 1952; UMMZ
+166985 (61), Yankton Co., Missouri R. at Yankton, 1952.
+
+WYOMING: * WU 2073 (6), Washakie Co., Big Horn R. at Worland, 1956.
+
+
+=Hybopsis gracilis gulonella= (Cope)
+
+(Plate 23)
+
+ _Pogonichthys communis_ Girard, 1856:188 (in part; original
+ description); Girard, 1858:247 (in part; characters; synonymy);
+ Cope and Yarrow, 1875:653 (characters; Pueblo, Colo.).
+
+ _Pogonichthys (Platygobio) gulonellus_ Cope, 1864:277 (original
+ description; near Bridger's Pass, Wyo.).
+
+ _Platygobio gulonellus_ Cope, 1865:85 ("Platte R., near Fort
+ Riley" [Fort Riley is on Kansas R., not Platte R.; Cope's
+ specimens probably are from Platte drainage, on basis of known
+ distributions of other species reported]).
+
+ _Ceratichthys physignathus_ Cope and Yarrow, 1875:651 (original
+ description; Arkansas R., Pueblo, Colo.).
+
+ _Platygobio communis_, Gill, 1876:408 (characters; Platte Valley;
+ Green River, Utah [the latter probably erroneous]).
+
+ _Couesius physignathus_, Jordan and Gilbert, 1882:219 (characters;
+ synonymy; Arkansas R., Pueblo, Colo.); Jordan, 1885:29
+ (records).
+
+ _Platygobio gracilis_, Jordan and Gilbert, 1882:219 (in part;
+ characters; synonymy); Cragin, 1885:109 (Garden City, Kans.);
+ Gilbert, 1885:98 (Garden City, Kans.); Jordan, 1885:29
+ (records); Evermann and Cox, 1896:412 (in part; habitat;
+ synonymy); Jordan and Evermann, 1896:326 (in part; characters;
+ synonymy); Ortenburger and Hubbs, 1927:125 (Canadian R., Norman,
+ Okla.); Hubbs, 1927:75 (parasites; teratology; records from New
+ Mexico); Hubbs and Ortenburger, 1929a:28 (S. Canadian R.,
+ Durham, Okla.); Jordan, 1929:76 (in part; characters); Jordan,
+ Evermann and Clark, 1930:136 (in part; synonymy).
+
+ _Platygobio physignathus_, Jordan and Evermann, 1896:325
+ (characters; synonymy; records from upper Arkansas R.); Ellis,
+ 1914:62 (characters; synonymy; records from Colorado);
+ Cockerell, 1927:123 (distribution in Colorado); Jordan, Evermann
+ and Clark, 1930:136 (synonymy; records from upper Arkansas R.).
+
+ _Platygobio gracilis communis_, Simon, 1946:71 (in part;
+ characters; food; habitat; spawning).
+
+ _Platygobio gracilis gulonellus_, Simon, 1946:72 (characters;
+ records from Wyoming; Arkansas R.).
+
+ _Platygobio gracilis:_ _communis_ x _gulonellus_, Simon, 1946:92
+ (North Platte R., Neb.-Wyo. line).
+
+ _Platygobio gracilis physignathus_, Moore, 1950:87 (habitat; sense
+ organs).
+
+ _Hybopsis gracilis communis_, Beckman, 1952:50 (characters; food;
+ habitat); Cross, Dalquest and Lewis, 1955:222 (records from
+ Texas).
+
+ _Hybopsis gracilis physignathus_, Beckman, 1952:50 (characters;
+ habitat).
+
+ _Hybopsis gracilis_, Eddy, 1957:111 (in part; characters; key);
+ Koster, 1957:61 (characters; habitat; spawning; food); Moore,
+ 1957:110 (in part; key); Smith, 1958:177 (fossil record; Doby
+ Springs, Okla.).
+
+_Diagnosis._--Post-Weberian vertebrae 36-38, rarely 39; lateral line
+scales 42-54, usually less than 50; pectoral rays 14-19, usually fewer
+than 17; head-depth 13.5-18.0 per cent of standard length, usually 14.8
+per cent or more. See Figures 1 and 2.
+
+_Other characters._--Circumference scale-rows 30-40, slightly fewer than
+in _H. g. gracilis_; predorsal scale-rows 17-27, somewhat fewer than in
+specimens from Canada, but much the same as specimens from the
+Missouri-Mississippi system; size small, rarely as much as 130 mm
+standard length (Fig. 1 of Pl. 24); head-length 24.0-28.0 per cent of
+standard length, usually more than 25.5 per cent; postorbital length of
+head 11.2-14.4 per cent of standard length, usually more than 12.5 per
+cent (both characters illustrate the larger head of _H. g. gulonella_);
+predorsal length 46.4-52.7 per cent of standard length, longer than in
+the other subspecies; orbit 5.0-6.6 per cent of standard length;
+prepelvic length 47.4-53.7 per cent of standard length, longer than in
+_H. g. gracilis_; caudal peduncle length 17.1-22.7 per cent of standard
+length, essentially the same in both subspecies.
+
+The label on types of this subspecies, in the Academy of Natural
+Sciences of Philadelphia, states merely "near Bridger's Pass, Wyo.,
+Expedition of 1856, Dr. W. A. Hammond" (letter from Dr. James Boehlke to
+Cross, dated Jan. 27, 1960). Dr. Hammond was a surgeon who also
+collected scientific specimens, assigned to an expedition under the
+command of Lt. F. T. Bryant. Bryant's log is recorded in the Proceedings
+of the 35th Congress (1858:455-481). The site at which these specimens
+were taken cannot be ascertained from the log, but study of it is
+helpful in indicating the probable locations.
+
+The expedition left Fort Riley on June 21, 1856, on the following route:
+up Republican River; across to Fort Kearney on Platte River; west along
+Platte River to S. Platte River; up S. Platte River to Pole (Lodgepole)
+Creek; Pine-Bluffs (Neb.-Wyo. line); across East Fork to West Fork of
+Laramie River; Cooper's Creek; West Fork of Medicine Bow; Pass Creek and
+down canyon of Pass Creek; across N. Platte River; up Sage Creek; on
+August 15, camped on Muddy Creek, tributary to Green River (first record
+of fish, trout); back to Sage Creek; August 19-21, camped on island in
+North Platte River; to Pass Creek; Elk Creek; west branch of Medicine
+Bow; Aspen Creek; West Fork of Laramie River; August 29, to East Laramie
+River where a large supply of fish was caught; tributary of Cache la
+Poudre then downstream to mouth of this river; down South Platte River
+past mouth of Crow Creek and Beaver Creek; left South Platte River 14
+miles below mouth of Beaver Creek, toward Republican River; down Rock
+Creek to Arikaree; down Arikaree to Republican River and down the
+Republican to Fort Riley.
+
+Mention is made of fish only twice in the entire log. We doubt that
+Muddy Creek or the East Laramie River is the type locality of _P.
+gulonellus_, because the flathead chub has not since been found in
+either of these streams. The most likely collection site for _P.
+gulonellus_ is the North Platte River near the mouth of Sage Creek, in
+what is now Carbon County, Wyoming, where the expedition was camped for
+three days. This species is known to occur in the North Platte River,
+and since the type locality is reported as "near Bridger's Pass" this is
+the probable location.
+
+_Range_ (Plate 21).--Upper mainstream and tributaries of Rio Grande,
+Pecos, Arkansas and North Platte Rivers; isolated populations in
+tributaries of the upper Missouri River.
+
+_Specimens examined._--Below are listed museum numbers, number of
+specimens (in parentheses), localities and year of collection. Series
+marked by asterisks (*) are intergrades tending toward _H. g.
+gulonella_. Literature reports are cited in the synonymy.
+
+COLORADO: KU 4742 (162), Bent Co., Purgatoire R. at Las Animas, 1959; KU
+4748 (105), Pueblo Co., Arkansas R. at west edge of Pueblo, 1959; KU
+4758 (50), Fremont Co., Arkansas R. at Florence, 1959; KU 4769 (64),
+Fremont Co., Beaver Cr., 1959.
+
+KANSAS: KU 2648 (2), Finney Co., Arkansas R., 1958; KU 2858 (13), Finney
+Co., Arkansas R. at Garden City, 1951; KU 3964 (12), Kearney Co.,
+Arkansas R., 1958; * KU 4041 (2), Cheyenne Co., Republican R., 1958; KU
+4732 (30), Hamilton Co., Arkansas R. at Kendall, 1959; * KU 4868 (1),
+Kansas-Nebraska line, Republican R. 1.5 mi. S. Hardy, 1959.
+
+MONTANA: * MSC 1960 (8), Powder River Co., E. Fork of Powder R., 1957;
+MSC 2010 (64), Dawson Co., Redwater R., 1957.
+
+NEBRASKA: * KU 2140 (2), Dawson Co., Platte R., at Gothenburg, 1931; *
+KU 4863 (20), Furnas Co., Republican R. at Cambridge, 1959; * UM (field
+no. 59-49) (74), Scotts Bluff Co., North Platte R. at Morrill, 1959; *
+UMMZ 133918 (17), Dixon Co., Logan Cr., 1939; * UMMZ 134813 (31), North
+Platte R., Neb.-Wyo. line, 1941; * UMMZ 135084 (14), Harlan Co., Beaver
+Cr. 0.25 mi. S Stamford, 1940; * UMMZ 135200 (41), Scotts Bluff Co.,
+North Platte R. 1 mi. SE Henry, 1940; * UMMZ 135280 (59), Cherry Co.,
+Niobrara R. 3 mi. SE Valentine, 1940; * UMMZ 135700 (25), Buffalo Co.,
+South Loup R. 8 mi. N Miller, 1941; * UMMZ 135778 (54), Thurston Co.,
+Logan Cr. 2.5 mi. W Pender, 1941; * UMMZ 135786 (25), Dixon Co., Logan
+Cr. 0.5 mi. NW Wakefield, 1941.
+
+NEW MEXICO: KU 4219 (50), Colfax Co., Cimarron Cr. at Springer, 1958; KU
+4235 (19), Mora Co., Sapello Cr. near Sapello, 1958; KU 4245 (157),
+Bernalillo Co., Rio Grande 12 mi. S Bernalillo, 1958; KU 4255 (22), Rio
+Arriba Co., Rio Grande at Velarde, 1958; KU 4266 (53), Sandoval Co., Rio
+Grande 2 mi. N Cochiti Pueblo, Marcelino Baca bridge, 1958; KU 4269
+(91), San Miguel Co., Pecos R., 3 mi. S Pecos, 1958; KU 4274 (25),
+Sandoval Co., Jemez R. at Jemez Canyon Dam, 1958; KU 4294 (113),
+Guadalupe Co., Pecos R. 3 mi. N. Dilia, 1958; UMMZ 94897 (146), Pecos R.
+at San Tuan, 1926; UMMZ 94898 (1), Pecos R. at San Juan, 1926; UMMZ
+118209 (68), Sapello Cr. at Sapello, 1937; UMMZ 133131 (7), Pecos R.
+0.5 mi. N Santa Rosa, 1940; UMMZ 133136 (1), Rio Grande at Albuquerque,
+1940.
+
+OKLAHOMA: KU 2329 (1), Cleveland Co.-McClain Co. line, S. Canadian R.,
+1952; UOMZ 26355 (10), Cimarron Co., Cimarron R. 2 mi. N. Kenton, 1957;
+UOMZ 5917 (2), Cleveland Co., S. Canadian R. S Norman, 1925.
+
+TEXAS: KU 3409 (18), Hemphill Co., Canadian R. at town of Canadian,
+1955.
+
+WYOMING: WU 2084 (4), Platte Co., N. Platte R. at Glendo, 1956; WU 2095
+(3), Converse Co., N. Platte R. at Douglas, 1956; UMMZ 104064 (58), N.
+Platte R. below Guernsey Dam, 1937; * UMMZ 114642 (7), drainage ditch in
+Wind R. drainage, 1936; * UMMZ 114644 (20), drainage ditch at Riverton,
+1936; * UMMZ 127518 (63), Weston Co., Beaver Cr., 1934; * UMMZ 127681
+(20), Big Horn Co., Big Horn R. tributary, 1939; * UMMZ 136488 (9),
+Crook Co., Belle Fourche R. 15 mi. N Devil's Tower, 1941; * WU 2122 and
+two uncatalogued series at WU (13), Belle Fourche R., no precise
+locality or date; UMMZ 159969 (14), Natrona Co., N. Platte R. 2 mi. E
+Casper, 1950.
+
+
+
+
+INTRASPECIFIC VARIATION
+
+
+Two subspecies of _H. gracilis_ are recognized by us: one northern and
+eastern, characteristically inhabiting large rivers (_H. g. gracilis_),
+and one southern and western, characteristically inhabiting small
+streams (_H. g. gulonella_). Other scientific names that have been
+applied to this fish in the past are listed in the synonymy.
+
+_H. g. gulonella_ is a chubby, deep-bodied fish, whereas _H. g.
+gracilis_ is long and slender. The head of the creek subspecies is
+deeper and longer than that of _H. g. gracilis_, being rounded
+anteriorly when seen in sideview. The head of the large-river subspecies
+is acutely wedge-shaped in profile. _H. g. gracilis_ has a larger orbit
+than _H. g. gulonella_. Fins of _H. g. gracilis_ are more strongly
+falcate than those of the other subspecies. _H. g. gracilis_ has a
+greater number of lateral line scales, pectoral rays and post-Weberian
+vertebrae than the creek subspecies. The large-river subspecies attains
+much larger size than does the creek subspecies (Plate 24). Except in
+areas of intergradation, complete separation of the two subspecies can
+be made on the basis of lateral line scales, pectoral rays,
+post-Weberian vertebrae and head-depth. The regressions of head-depth on
+standard length in _H. g. gracilis_ from the Saskatchewan River (several
+localities) and in _H. g. gulonella_ from Beaver Creek, Arkansas River
+Drainage (KU 4769) are shown in Plate 24. Although values for the
+largest specimens of _H. g. gracilis_ are omitted from Plate 24, the
+regression remains essentially linear to standard lengths of
+approximately 250 mm. On the basis of head-depth alone, separation of
+the two subspecies is possible in specimens larger than 40 mm. Similar
+results were obtained by using the regression of postorbital length on
+standard length, and could have been obtained by using other
+proportional measurements.
+
+
+
+
+NATURAL HISTORY
+
+
+_Habitat_
+
+The species inhabits alkaline streams with shifting sand bottoms where
+the waterlevel fluctuates considerably with heavy rains and melting
+snow. The flathead chub is found in silty water and often is the
+predominant species in streams that have high turbidity. The remarkable
+ability of this fish to withstand exceedingly high turbidity is
+illustrated by its predominance in the Little Missouri River, which has
+an average concentration of suspended silt two and one-half times that
+of the Missouri River at Kansas City (Personius and Eddy, 1955:42).
+
+[Illustration: FIGURE 1. Graphic analysis of lateral line scales,
+pectoral rays and post-Weberian vertebrae in _Hybopsis gracilis_.
+In each symbol, horizontal line = range, vertical line = mean,
+open rectangle = one standard deviation on each side of mean, black
+rectangle = twice the standard error on each side of mean.
+
+_H. g. gracilis_ is found in large rivers throughout its range,
+occasionally migrating into smaller streams, especially in the spawning
+season. It prefers the main channel of rivers in moderate to strong
+current. All series examined are from elevations lower than 3,000 feet.
+
+Numbers to left of symbols = number of specimens examined from that
+locality; combined collections indicated by brackets. The dash-lines
+represent drainage patterns of rivers in which this species occurs.]
+
+_H. g. gulonella_ occupies small rivers and creeks, preferring pools
+with moderate currents. In fall, dense concentrations of this subspecies
+have been found in small pools, where brush, driftwood or other debris
+deflects the current and prevents filling with drifting sand. Hundreds
+of flathead chubs were collected in such pools in the Purgatoire and
+Arkansas rivers. Specimens were also collected with ease in Beaver
+Creek, Colorado, from pools with murky water and slight flow, over
+bottoms of gravel and bedrock. No brush or other debris was near the
+pools. In each case the streams carried little water, although they
+undoubtedly carry greater volumes of water in spring and early summer
+after rains and spring thaws. The preferred bottom-type for this
+subspecies seems to be gently shifting sand.
+
+_H. g. gulonella_ is found in warm-water streams, whereas _H. g.
+gracilis_ occurs in cooler water. The southwestern subspecies was taken
+in August in the Mora River drainage at Sapello (temperatures above 80 deg.
+F.) but not at Mora (temperatures below 70 deg. F.). In the Purgatoire
+River, a thriving population was found where the water temperature was
+92 deg. F., on September 6, 1959. In the Arkansas and Pecos rivers and the
+Rio Grande this subspecies is most abundant below the mountainous parts
+of the stream-courses, but at elevations higher than 4,000 feet on the
+plains.
+
+
+_Associated Species_
+
+[Illustration: FIGURE 2. Graphic analysis of head-depth, postorbital
+length of head and predorsal length of _Hybopsis gracilis_, expressed
+as thousandths of standard length. Numbers in parenthesis = number
+of specimens examined from each locality. In each symbol, horizontal
+line = range, vertical line = mean, open rectangle = one standard
+deviation on each side of mean, black rectangle = twice the standard
+error on each side of mean. The dash-lines represent drainage patterns
+of rivers in which this species occurs. All measurements are of
+specimens 70 to 100 mm in standard length.]
+
+In the Pecos and Arkansas basins, species commonly taken with _H. g.
+gulonella_ are _Catostomus commersonnii_, _Hybognathus placita_,
+_Notropis lutrensis lutrensis_, _Notropis stramineus missuriensis_,
+_Pimophales promelas_, and _Campostoma anomalum plumbeum_. The only
+spiny-rayed fishes that we have found with _H. g. gulonella_ are
+_Lepomis cyanellus_ and _L. humilis_, both of which are scarce.
+Associates of _H. g. gracilis_ include the same species, plus other
+ostariophysan fishes such as species of _Carpiodes_, _Ictiobus_, and
+silt-adapted species of _Hybopsis_ and _Notropis_.
+
+We failed to find the flathead chub at any of 11 localities in the South
+Platte drainage, where we collected in September, 1959. Dr. George
+Baxter, of the Department of Zoology, University of Wyoming, told
+us that he has never found _H. gracilis_ in that drainage. The fauna
+of the South Platte includes _Catostomus catostomus_, _Semotilus
+atromaculatus_, _Hybopsis biguttata_, _Hybognathus hankinsoni_,
+_Notropis cornutus frontalis_, _Etheostoma nigrum_ and _E.
+exile_--species rarely if ever found with _H. gracilis_.
+
+Ecologically, _H. g. gulonella_ seems to be the counterpart of
+_Semotilus atromaculatus_ in streams where the latter species is absent.
+Observations of _H. g. gulonella_ in the Purgatoire River indicated
+that loosely-organized groups of flathead chubs congregated one to four
+inches above the bottom of pools, and near or under protective cover
+such as roots of vegetation or debris lodged against shore. Individuals
+moved about independently within the group (rather than as schools), and
+occasionally rose to the surface, perhaps for food.
+
+
+_Food_
+
+The flathead chub is chiefly carnivorous, but its food includes some
+aquatic vegetation (Table 1). Most organisms found in specimens (both
+subspecies) were terrestrial insects (Coleoptera, Diptera, Orthoptera);
+all insects were adult stages, except those designated as larvae in
+Table 1. Roundworms probably were parasites, rather than food.
+
+Hubbs (1927:76) states that the food of young flathead chubs that were
+obtained from the Arkansas River System in New Mexico consisted "almost
+entirely of crustaceans (small ostracods and cladocerans to the
+exclusion of all else but an occasional larval or adult insect, etc.)."
+
+
+_Spawning Season_
+
+Specimens of _H. g. gulonella_ that have been examined reach sexual
+maturity at approximately 65 mm standard length. Most specimens of _H.
+g. gracilis_ less than 85 mm in standard length are immature, but larger
+specimens probably are mature.
+
+The spawning season is in late summer, beginning in July and extending
+into September. Specimens from the Peace River, collected on August 10,
+1952, include females that were mostly spent and tuberculate males.
+Males and females in spawning condition were collected in the Milk River
+in August of 1955. A large prespawning female was obtained in Red Deer
+River in June of 1952. A male from Fort McMurray had fairly well
+developed tubercles on August 9, 1955. A prespawning female was taken
+from the Saskatchewan River at Clarkboro Ferry on June 7, 1957.
+Tuberculate males were collected in the Powder River on June 30, 1957.
+Specimens from the White River in South Dakota, collected on July 7,
+1934, include tuberculate males. The specimens discussed above are _H.
+g. gracilis_ or intergrades tending toward that subspecies.
+
+Specimens of _H. g. gulonella_ collected in the Arkansas River at Pueblo
+and Florence, Colorado, on September 7, 1959, include some tuberculate
+males, although most females are spent. On August 8, 1957, a series of
+flathead chubs that includes tuberculate males was collected in the
+Redwater River, Montana. In the Pecos River on August 25, 1958,
+spawning seemingly had been completed, although a few males still bore
+tubercles.
+
+TABLE 1. ORGANISMS FOUND IN STOMACHS OF HYBOPSIS GRACILIS FROM VARIOUS
+LOCATIONS, EXPRESSED AS PERCENTAGE OF TOTAL VOLUME.
+
+ A: S. Saskatchewan R., Clarkboro Ferry, Sask.
+ B: Milk R., Alberta
+ C: Missouri R., S. D.
+ D: Missouri R., Neb.
+ E: Arkansas R., Fremont Co., Colo.
+ F: Arkansas R., Pueblo Co., Colo.
+ G: Pecos R., San Miguel Co., N. M.
+
+ ==============================+=====+=====+=====+=====+=====+=====+=====
+ | A | B | C | D | E | F | G
+ ------------------------------+-----+-----+-----+-----+-----+-----+-----
+ No. specimens examined | 1 | 7 | 6 | 10 | 10 | 10 | 10
+ | | | | | | |
+ No. specimens containing food | 1 | 6 | 1 | 2 | 1 | 3 | 7
+ ------------------------------+-----+-----+-----+-----+-----+-----+-----
+ KIND OF ORGANISM | | | | | | |
+ | | | | | | |
+ Aphasmidia |10.0 |00.7 | |03.0 | | |
+ Arthropoda | | | | | | |
+ Araneae | | | | | | |
+ Argiopidae | | | | |04.0 | |
+ Theridiidae | | | | |04.0 | |
+ Insecta | | | | | | |
+ Ephemeroptera (nymph) | | | | | | |
+ Baetidae | |05.0 | | | | |
+ Heptagenidae | |08.0 | | | | |
+ Hemiptera | | | | | | |
+ Corixidae |35.0 |00.3 | | | | |
+ Hymenoptera | | | | | | |
+ Formicidae | |21.0 | | | | |60.0
+ Coleoptera | | | | | | |
+ Staphylinidae | |01.7 |07.0 | | | |
+ Scolytidae | |13.3 |70.0 | | | |
+ Tenebrionidae | |05.7 | | |70.0 | |
+ Carabidae | |05.7 | | | |01.0 |
+ Curculionidae | |01.0 | | | | |
+ Coccinellidae | | | | | | |09.0
+ Trichoptera (case) | |01.7 | | | | |
+ Diptera | | | | | | |
+ Mymaridae | |00.3 | | | | |
+ Empididae | |01.3 | | | | |
+ Cecidomyiidae | | | | |04.0 | |
+ Trachinidae | |00.7 | | | | |
+ Simulidae | |06.7 |20.0 | | | |
+ Tabanidae | | | | |06.0 | |
+ Chironomidae | | | | |06.0 | |
+ Not identified to family| |01.0 | | | | |
+ Orthoptera | | | | | | |
+ Locustidae | |07.7 | | | | |
+ Tettigoniidae | | |03.0 |70.0 | | |09.0
+ Tetrigidae | | | | |06.0 | |
+ Homoptera | | | | | | |
+ Fulgoridae | |05.0 | | | | |01.0
+ Insect egg | |00.7 | | | | |
+ Plants | | | | | | |
+ Cyanophyceae | | 09.0| | | | 99.0| 20.0
+ Cyperaceae | | 02.0| | | | | 01.0
+ Zannichellia palustris | | 00.3| | | | |
+ Vascular remains | 55.0| | | 27.0| | |
+ | | | | | | |
+ Miscellaneous | | | | | | |
+ Sand | | 00.7| | | | |
+ Pharyngeal tooth | | 00.3| | | | |
+ +-----+-----+-----+-----+-----+-----+-----
+ Total (%) |100.0| 99.8|100.0|100.0|100.0|100.0|100.0
+ ------------------------------+-----+-----+-----+-----+-----+-----+-----
+
+Spawning apparently occurs when river levels recede to the seasonal
+lows. In late summer, temperatures of these rivers probably are maximal,
+their turbidities are reduced, and their sandy bottoms are stable.
+Underhill (1959) reports that this species is rare in the Vermillion
+River, a northeastern tributary of the Missouri River, except in autumn
+when large numbers occur near the mouth of the river. We suspect that
+this is associated with spawning.
+
+[Illustration: PLATE 21
+
+Distribution of collections examined.]
+
+[Illustration: PLATE 22
+
+_Hybopsis gracilis gracilis._ Missouri River, Thurston County, northeast
+of Macy, Nebraska. Largest specimen 87.5 mm standard length.]
+
+[Illustration: PLATE 23
+
+_Hybopsis gracilis gulonella._ Pecos River, San Miguel County, 3 miles
+south of town of Pecos, New Mexico. Largest specimen 91 mm standard
+length.]
+
+[Illustration: PLATE 24
+
+FIG. 1. Top: _Hybopsis gracilis gracilis_, 230.0 mm standard length,
+one of the largest specimens examined. Missouri River, Carson
+County-Walworth County line, 3 miles northeast of Mobridge, South
+Dakota, at mouth of Grand River.
+
+Bottom: _Hybopsis gracilis gulonella_, 121.6 mm standard length, the
+largest specimen examined of this subspecies. Beaver Creek, Fremont
+County, 10 miles northeast of Florence, Colorado, on Highway 115.]
+
+[Illustration: FIG. 2. Regression of head-depth on standard length in
+_Hybopsis gracilis gracilis_ from the Saskatchewan River, and in _H. g.
+gulonella_ from Beaver Creek, Arkansas River Drainage (KU 4769).]
+
+
+
+
+DISCUSSION
+
+
+_Hybopsis gracilis_ is highly variable in several morphological
+characteristics, including size and shape of head, body, and fins, and
+number of scales, vertebrae, and fin-rays. The variations are correlated
+in a way that indicates the existence of two subspecies. One of these,
+_H. g. gracilis_, attains large size, and has 1) a slender, streamlined
+body, 2) a depressed head that is acutely wedge-shaped in profile, 3)
+strongly falcate fins with the dorsal and pelvic fins originating
+anteriorly, and 4) many scales, vertebrae, and pectoral fin-rays. The
+second subspecies, for which _H. g. gulonella_ is the oldest applicable
+name, is small, and has 1) a deep, chubby body, 2) head convex in dorsal
+contour (less depressed than in _H. g. gracilis_), 3) fins less falcate
+than in the latter subspecies, with the dorsal and pelvic fins
+originating more posteriorly, and 4) fewer scales, vertebrae, and
+pectoral fin-rays than _H. g. gracilis_. These differences are
+consistently expressed throughout the size-ranges of the subspecies, and
+in series collected at the same or nearby localities in several
+different years. Considerable variability was found in features other
+than those mentioned above, but individual variation among specimens
+from the same locality and adjacent localities is so great that none is
+diagnostic of subspecies. For example, orbital size and length of fins
+(but not their falcate shape) are variables that have little diagnostic
+value, although both features seem to vary in clinal fashion, with the
+higher values in the north.
+
+Variation in _H. gracilis_, as shown in the graphic analysis (Figs. 1
+and 2) and distribution map (Plate 21), presents two clines: a
+north-south cline and a large-river to small-river (mainly east-west)
+cline. The absence of _H. gracilis_ from certain portions of river
+systems is a matter of concern. The species has not been found in the
+lower Arkansas River and the Rio Grande, nor in sandy tributary creeks
+in eastern Kansas and Missouri that appear to provide suitable habitat.
+It has already been noted that _H. g. gulonella_ seems to be the
+ecological equivalent of _Semotilus atromaculatus_ in streams in which
+_S. atromaculatus_ is not found. _S. atromaculatus_ occurs in creeks of
+eastern Kansas and Missouri, and may provide interspecific competition
+that prevents establishment of the flathead chub in these creeks.
+Regardless of cause, the gaps in distribution of _H. gracilis_ tend to
+limit gene flow.
+
+Many characters used in the separation of the two subspecies are known
+to be influenced by environmental conditions, especially temperature.
+Hubbs (1922, 1926, 1941), Schultz (1927), Vladykov (1934), Taning (1952)
+and Weisel (1955), among others, have pointed out a correlation between
+temperature (or developmental rate of fish) and the number of vertebrae,
+scales, and fin-rays. Likewise, Martin (1949) and Hart (1952) have shown
+that the proportions of some body-parts vary in response to temperature
+during early development. In _H. gracilis_, the general nature of the
+clines found in a majority of characters (but not all characters)
+suggests a temperature influence. However, temperature-dependent
+variability that has so far been demonstrated experimentally in fishes
+is generally of lesser magnitude than the differences distinguishing _H.
+g. gracilis_ and _H. g. gulonella_. To our knowledge, the most extreme
+differences that have been induced by modification of temperature are
+those reported for _Salmo trutta_ by Taning (1952:181-182), who states:
+"Shock treatment produced by especially great changes in temperature
+(_c._ 10-14 deg. C), especially during the super-sensitive period [of
+somatic differentiation that fixes vertebral number] may produce ... a
+difference of 3-4 vertebrae ... in offspring of the same parents." The
+difference cited approximates that which distinguishes natural
+populations of _H. g. gracilis_ and _H. g. gulonella_. Although we
+cannot assume that the sensitivity of the brown trout is the same as
+that of the flathead chub, the causative conditions in Taning's study
+could scarcely be expected in nature; furthermore, it seems significant
+that extremely high (as well as extremely low) mean numbers of scales
+and vertebrae were found at southern localities, and that low mean
+numbers of scales and vertebrae were found as far north as Wyoming and
+Montana. We think it likely that temperature does influence the
+expression of characters in _H. gracilis_, directly in individual
+development, and indirectly as a selective mechanism in the evolutionary
+process. The extent to which each kind of influence exists can be proved
+only by experimental work with both subspecies, which we hope to
+undertake at a later date.
+
+Other environmental factors that may have selective influence in this
+species are rate of current, volume of flow, and turbidity. Interaction
+of these environmental factors could result in genetic fixation of
+morphological characters through natural selection. The characters that
+distinguish _H. g. gracilis_ from _H. g. gulonella_ seem adaptive to
+life in large rivers and small streams. Evidence that these characters
+are under limited, direct environmental influence is found among
+populations in the Arkansas River System. Although populations in the
+Arkansas River have no continuity with populations of _H. g. gracilis_,
+upstream-downstream variations like those found in other river systems
+are apparent, but in lesser degree. The direction of variation in the
+Arkansas River is the reverse of that in the Platte and other
+tributaries of the Missouri River. For example, the populations farthest
+upstream (Florence, Pueblo) have slightly higher mean numbers of lateral
+line scales than do populations from Kansas, downstream.
+
+A remarkable effect of extreme parasitism in _H. gracilis_ has been
+described by Hubbs (1927). Very young chubs that harbored numerous
+tapeworms (_Proteocephalus_) had unusually large numbers of lateral-line
+scales, large eyes, short snouts, small fins, small mouths lacking
+barbels, and coalescent nares (internarial bridge weak or absent). Some
+of these abnormalities presumably resulted from retention of larval
+characteristics of the fish, correlated with the degree of infestation
+by tapeworms. No teratological adults were found, indicating that severe
+infections prevent survival to maturity.
+
+_H. g. gracilis_ occurs in three separate river systems (Mackenzie,
+Saskatchewan, Missouri-Mississippi) from latitude 36 deg. N to 66 deg. N, and
+longitude 89 deg. W to 123 deg. W. _H. g. gulonella_ exists as several
+seemingly-isolated populations in the upper parts of the Rio Grande,
+Pecos, South Canadian, Cimarron, Arkansas, Platte, and upper Missouri
+basins, from latitude 35 deg. N to 48 deg. N, and longitude 97 deg. W to 100 deg. W.
+
+There is evidence of high mobility on the part of both subspecies, based
+on irregularity of their occurrence in certain localities. Many
+collections have been made in the Cimarron River in the vicinity of
+Kenton, Oklahoma, from 1925 to the present, but only one of these (in
+1957) contained flathead chubs. Bait dealers who seine the South
+Canadian River in Dewey County, Oklahoma, have taken flathead chubs in
+abundance in some seasons, but not at all in others. Seasonal variation
+in abundance in the lower Vermillion River, South Dakota (Underhill,
+1959:100) has been cited, and the number collected in the lower Kansas
+River near Lawrence has varied similarly. Many rivers occupied by _H. g.
+gulonella_ (and by intergrades) are intermittent, and in some years
+their sand-filled channels become wholly dry for many miles. These
+factors probably promote mixing of the two subspecies, and may account,
+over long periods of time, for the wide dispersal of _H. g. gulonella_
+in the Missouri Basin. Flathead chubs are known from Pleistocene beds at
+Doby Springs, Oklahoma (the Doby Springs local fauna) (Smith, 1958:177).
+Drainage connections between the Arkansas, Kansas and Platte river
+systems existed in Kansan and Nebraskan times (Frye and Leonard,
+1952:189-190). Populations that have subsequently become isolated in
+those rivers could be accounted for in this way. Flathead chubs could
+have entered the Rio Grande-Pecos system by stream-capture from the
+Arkansas System, in northeastern New Mexico or southern Colorado. _H. g.
+gracilis_ undoubtedly entered the Saskatchewan and Mackenzie basins from
+the upper Missouri Basin, following glacial retreat (Walters, 1955:347).
+
+
+
+
+LITERATURE CITED
+
+
+AGASSIZ, L.
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+BRYANT, FRANCIS T.
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+
+
+_Transmitted November 8, 1960._
+
+
+28-5871
+
+
+[Transcriber's Note:
+
+The following changes have been made to the original text:
+
+ Table of Contents: page number of "Food" and "Spawning Season"
+ changed from 339 to 338
+ Page 327: "abbreviated AU" changed to "abbreviated UA"
+ Page 344: "Societe Geologique" changed to "Societe Geologique"]
+
+
+
+
+
+End of the Project Gutenberg EBook of Geographic Variation in the North
+American Cyprinid Fish, Hybopsis gracilis, by Leonard J. Olund and Frank B. Cross
+
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