A lower Pleistocene deposit containing fossil vertebrates near Broadwater, Morrill county, Nebraska, has been reported upon by the writers, beginning three years ago. Five fossil quarries have been opened since the site was discovered in 1936

Barbour, Erwin Hinckley

Schultz, C. Bertrand

English

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University of Nebraska - Lincoln
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Bulletin of the University of Nebraska State
Museum Museum, University of Nebraska State
1939
A New Giant Camel GIGANTOCAMELUS
FRICKI, gen. et sp. nov.
Erwin Hinckley Barbour
C. Bertrand Schultz
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Part of the Entomology Commons, Geology Commons, Geomorphology Commons, Other
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Barbour, Erwin Hinckley and Schultz, C. Bertrand, "A New Giant Camel GIGANTOCAMELUS FRICKI, gen. et sp. nov." (1939).
Bulletin of the University of Nebraska State Museum. 30.
http://digitalcommons.unl.edu/museumbulletin/30
BULLETIN OF THE UNIVERSITY OF NEBRASKA 
STATE MUSEUM 
Erwin Hinckley Barbour. Director 
VOLUME 2 LINCOLN, NEBRASKA, SEPTEMBER 1939 NUMBER 2 
A New Giant Camel 
GIGANTOCAMELUS FRICKI, gen. et sp. nov. 
By ERWIN HINCKLEY BARBOUR AND C. BERTRAND SCHULTZ 
DEVELOPMENT OF THE BROADWATER-LISCO QUARRIES 
A LOWER Pleistocene deposit containing fossil vertebrates near Broad-water, Morrill county, Nebraska, has been reported upon by the 
writers, beginning three years ago.! Five fossil quarries have been opened 
since the site was discovered in 1936. A quantity of fine specimens from 
this area is now in the collections of the University of Nebraska State 
Museum. During June 1936, members of the Nebraska field party,2 while 
exploring east of the Broadwater quarries, discovered several localities 
that yielded Stegomastodon and camel bones. In one of these (SYz of sec. 
11, T. 18 N., R. 46 W., Garden county) the distal end of an unusually large 
camel metapodial (No. 9-19-6-36 S.P.) and associated skeletal elements 
were found. The site was revisited in September 1937, and at that time 
numerous bones including a skull (No. 1-20-9-37 S.P.) were unearthed. 
Mr. Charles Sothman of Lisco, who had charge of the land where the camel 
bones were found, reported to the collectors that he had noticed similar 
fossil remains farther east. During the falls of 1937 and 1938 Messrs. 
Sweet, Middleswart and Chaloupka of Bridgeport did a considerable 
amount of exploratory work which was extended through the winters. 
Numerous prospects were located and test pits were dug. Three quarries 
were opened in the SEY4 of sec. 13, T. 18 N., R. 46 W., 3 miles east 
and 2Yz miles north of Lisco, Garden county. During 1938, from June 
10 to October 1, the Lisco quarries were worked by a field party from the 
1 See Bibliography, p. 26. Barbour & Schultz (1936, p. 308; 1937A, p. 1-10; 1937B, p. 185-9). 
2 Field work at Broadwater was carried on under direction of the junior writer. The collecting 
party included Messrs. E. L. Blue, Thompson M. Stout, Frank Crabill, Gordon Graham, Jack Graham, 
David Abbott, Dean Ked, Fred Schall, Mrs. C. Bertrand Schultz, and was aided by Messrs, S. R. 
Sweet, T. C. Middleswart, W. F. Chaloupka, and John Ochoa. 
17 
18 UNIVERSITY OF NEBRASKA MUSEUM BULLETIN 
Fig, 5.--Gigalltocamelus jric/.;..i, new genus and species. C0111posite skeleton. No. 
1-25-8-38 S.P., The University of Nebraska State Museum. X 1/30. The skeleton has 
been skillfully mounted without visible supports by Mr. Henry Reider and Mr. Frank 
Bell. 
University of Nebraska State Museum, assisted by a Works Progress 
Administration project under the supervision of Jack Graham and Paul 
Burkholder. Forty crates of rare camel material were shipped to the 
Museum from these quarries. A detailed report based on these specimens 
will appear in a forthcoming paper. 
In October 1938, several camel prospects were located east of the original 
quarries in Sljz of sec. 21, T. 18 N., R. 45, Garden county, on the land of 
Bertha Vocke and Conrad Wallace. The largest examples of Giganto-
camelus have come from these new pits. The Lisco area is being worked 
extensively during the 1939 field season by a Museum party. 
The writers are grateful to Mr. Childs Frick for his special interest in 
the Lisco quarries and for permitting the study of his excellent collection 
of Megacamelus from Arizona. Thanks are also due to Messrs. S. R. Sweet, 
Fig. 6.-Crown view of skull of Gigantocamelus friel,;. No. l A·25 -8-38 S.P. , T he Uni versity of Nebraska State Museum. X 9/40. 
20 UNIVERSITY OF NEBRASKA MUSEUM BULLETIN 
T. C. Middleswart, and W. F Chaloupka for their assistance in helping 
to develop the various camel quarries. Mr. Frank Ruby of Lisco aided 
the Museum parties by granting permission to excavate at the type locality. 
The Works Progress Administration staff in Nebraska, especially Mrs. 
Ethel May Sanmann, Mr. E. O. Raasch, and Miss Lilla Graham, liberally 
cooperated with the Museum in securing sufficient help in the field and 
laboratory to excavate and prepare the fossil camel bones. 
DESCRIPTION AND DISCUSSION 
Gigantocamelus fricki, NEW GENUS AND SPECIES 
Type.-Skull, No. IA-25-8-38 S.P., University of Nebraska State Museum. 
Referred.-Mandible, No. IB-25-8-38, S.P. (from different individual than skull), 
and composite skeleton, No. 1-25-8-38 S.P. (mounted with type skull; limb elements, 
except for metapodials, appear to be from one individual) and a large collection of 
skulls, rami and skeletal parts from the Lisco quarries. 
Locality.-Lisco quarries I, 2 and 3, SE\<4 of sec. 13, T. 18 N., R. 46 W., Garden 
county, Nebraska. 
Horizon.-Lower Pleistocene. 
Generic and Specific Characters.-Largest of known camelids; form and proportions 
approaching those of Megacamelus and Titanotylopus, but differing in dental formula 
and other characters; dental formula, 10-1/3 , C 1/1, P 3/3 , M 3/3, with premolar 2, 
above and below, absent; 1 3 rarely present; inferior and superior canines enlarged into 
tusks; posterior portion of canine very thin and with a sharp edge; mandible long and 
narrow, not so massive as that of Titanotylopus; skeletal parts more massive and much 
larger than those of Camelops; average metapodials and other limb elements more 
massive than those of Megacamelus. 
Associated Genera.-Smilodon, Megalonyx, Stegomastodon and Equus. The fauna 
of the Broadwater quarries in Morrill county is listed at the end of this report. 
Measurements.-See table of measurements on opposite page. 
Discussion.-The Lisco specimens appear to differ from any known 
camel remains. It is difficult to assign them to an already established 
genus and the writers consider the differences to be of generic value. With 
a large series of superior and inferior dentitions available, it is noted that 
the dental formula is very stable. The enlargement of the canines, as noted 
in Gigantocamelus, is unusual among the camels. A few examples from 
Lisco have smaller canines than the average, but these may represent 
females. Enlarged canines are also found in Titanotylopus (Barbour 
& Schultz 1934, p. 291-4), a large camel that lived later in the 
Pleistocene. This latter genus is known only from a partial mandible but 
it seems to be quite distinct from Gigantocamelus in the definite absence 
of P1 and the greatly reduced distance between the canine and Pa• 
Titanotylopus may be more closely related to Camelops. 
Childs Frick (1929, p. 107) has described a huge extinct camel, 
Megacamelus, from the Hopi Indian Agency of Arizona. This form has a 
A NEW GIANT CAMEL, GIGANTOCAMELUS FRICKI 21 
MEASUREMENTS 
SKULL MEASUREMENTS 
lA-25-8-38 1-20-10-38 
Length (max., including supraoccipital crest and premaxillae) . 
Condylo·basal length (condyles to anterior of premaxillae) .. 
Width (max., at orbits) ............ . 
Width (min., interorbital). 
Length of dental series (G-M 3 inclusive) 
Length, P 3~M 3 inclusive 
Length, P Lp 4 
Length of superior molar series. 
Diastema, C to pl. 
Diastema, P 1 to P 3 . 
Diameter (max.) of canine at base 
Length of canine. 
Length of pl. 
JAW MEASUREMENTS 
IB-25-8-38 
S.P. 
Length (max., including incisors). 
Length from posterior of condyle to anterior of canine 
Depth of ramus below anterior of third inferior molar 
Length of dental series (C-M3 inclusive). 
Length of inferior molar-premolar 
series (including P 1) 
Length, P 3-M 3 
Length, P 3-P 4 .' 
Length, M I-M 3 
Diastema, C-p 1 
Diastema, P I-P 3 
660 A 
633 
88 
452 
340 
210 
55 
159 
79 
106 
MEASUREMENTS OF SKELETAL ELEMENTS 
Length of: 
Scapula (max.) 
Humerus (articular) 
Radius (articular) 
Radius-ulna (max.). 
Metacarpal (max.) 
Femur (articular) ............... . 
Tibia (articular) 
Calcaneum (max.) 
Metatarsal (max.) 
3E==estimated; A==approximate. 
S.P. S.P. 
mm. mm. 
757 855E3 
720 840 A 
345 368 A 
284 
390 424 
206 197 
67 65 
141 135 
56 44 A 
92 143 A 
55 45 
77 81 
29 36 
9-20-9-37 2-25-8-38 
S.P. S.P. 
635 E 
603 A 
94 
443 
372 
254 
60 
201 
52 
104 
90 
327 
2ll 
51 
162 
100 
1-25-8-38 
S.P. 
560 E 
497 
551 
653 
425 
563 
477 
176 
404 
Fig. 7.-Palatine view of skull of Gigantocamelus fricki. No. IA-25-8-38 S.P., The University of Nebraska State Museum. X 9/40. 
Fig. 8.-Side view of skull of Gigantocamelus tricki. No. lA-2S- 8-3 8 S.P., The University of Nebraska State Museum. X 9/ 40. 
Fig. 9.-Crown view of mandible of Gigantocamelus tricki. No. 9 -20-9-37 S.P., The University of Nebraska State Museum. X 9/40. 
Note deciduous canines still present. 
24 UNIVERSITY OF NEBRASKA MUSEUM BULLETIN 
marked facial fossa, I 3 is present and the canines are not enlarged. These 
characters are not observed in Gigantocamelus. The skeletal elements 
appear to be more massive in the Nebraska form. The parts used in the 
mount are from small individuals. Unfortunately, there were not enough 
of the largest bones for a mount. One of these giants would stand nearly 
12 feet tall. 
Megatylopus (Matthew & Cook 1909, p. 396-401), an Upper Tertiary 
camel from Nebraska, cannot readily be compared with Gigantocamelus. 
Megatylopu.f is a smaller genus with a dentition, Pia, C1h, p3-21a-2, M31a. 
The reduction in the premolar series here suggests that these two genera 
represent independent lines of development. Pliauchenia spatula Cope, a 
species often referred to the genus Megatylopus, seems to be much more 
closely allied to Gigantocamelus fricki than to M. gigas, the genotypic 
species of Megatylopus. 
LIST OF MAMMALS FROM BROADWATER QUARRIES 4 
I NSECTIVORA 
Sorex sp. Shrew. 
EDENTATA 
Mylodon sp. Ground sloth. 
LAGOMORPHA 
Lepus? sp. Jack rabbit. 
Sylvilagus? sp. Cottontail. 
RODENTIA 
Sciurid. Squirrel. 
Geomys sp. Pocket gopher. 
Thomomys? sp. Pocket gopher. 
Procastoroides sweeti Barbour and Schultz. Ancestral giant beaver. 
Dipoides? sp. Ancestral beaver. 
Peromyscus sp. Deer mouse. 
Ondatra sp. Muskrat. 
Mimomys? sp. Vole. 
Microtinid indct. Vole. 
Zapus sp. Jumping mOUse. 
Neotoma? sp. Wood rat. 
CARNIVORA 
Canis sp., near C. latrans Say. Coyote. 
Canis sp., near Canis (Aenocyon) dirus Leidy. Dire wolf. 
Satherium piscinaria middleswarti Barbour and Schlutz. Otter. 
Felid. Cat. 
PROBOSCIDEA 
Stegomastodon miri/icw primitiNls Osborn. Mastodont. 
PERISSODACTYLA 
Equus sp., near E. excclslIs Leidy. Horse. 
Equus sp., more primitive species. Horse. 
Equid, very light-limbed form; known only from a single metapodial. Horse. 
40 The Broadwater quarries are located 4 miles east and 1 mile north of Broadwater, in NEY4 of 
sec. 20 and NWY4 of sec. 21, T. 19 N., R. 47 W., Morrill county, Nebraska, on the farm of Mr. Dan 
J. Boman. 
Fig. 10.-Side view of right ramus of Giganiocame/us f,';cki. No. 2·25·8·38 S.P., The University of Nebraska State Museum. X 9/40. ' 
26 UNIVERSITY OF NEBRASKA MUSEUM BULLETIN 
ARTIODACTYLA 
Camelops sp., much larger form than C. l(ansanus Leidy. Camel. 
Tanupolama sp., much larger form than T. americanus (Wortman). Llama-like 
camel. 
Gigantocamelus fricki Barbour and Schultz. Giant camel. 
Capromeryx sp., larger form than C. fura/a Matthew. Small antelope. 
Antilocaprid, probably Tetrameryx. Four-horned antelope. 
The collection from the Broadwater quarries also contains the follow-
ing unidentified vertebrates: 
PISCES 
Various forms. 
AMPHIBIA 
A large collection of amphibian material, especially frogs. Three or four families 
are represented. This material is now being studied by Dr. Edward H. 
Taylor of the Department of Zoology, University of Kansas. 
REPTILIA 
Turtle, perhaps two forms. 
Snake, at least one form. 
AVES 
Various forms. 
BIBLIOGRAPHY 
Barbour, Erwin H. and C. Bertrand Schultz. 1934. A new giant camel, Titanotyloplls 
nebraskensis, gen. et sp. nov. Eul. Neb. State Mus. 1 (36) :291-4. May. 
------1936. Notice of a new bone bed in the early Pleistocene of Morrill 
county, Nebraska. Bul. Neb. State Mus. 1 (45) :383. April. 
------1937A. An early Pleistocene fauna from Nebraska. Am. Mus. Nov. 
(942) :1-10. Sept. 10. 
------1937B. Pleistocene and post-glacial mammals of Nebraska. In "Early 
Man," p. 185-9. Lippincott. 
Cope, E. D. 1875. On some new fossil Ungulata. Proc. Acad. Nat. Sci. Phila., p. 258. 
------1884. The extinct Mammalia of the Valley of Mexico. Proc. Am. Philos. 
Soc. 22:16-18. 
----1893. A preliminary report on the vertebrate paleontology of the Llano 
Estacado. 4th Ann. Rep. Geol. Surv. Texas. p. 70-3. 
Frick, Childs. 1929. History of the earth (Childs Frick Tertiary-Quaternary explora-
tions, 1928). Nat. Hist. 24(1) :106-8. Jan.-Feb. 
Gregory, J05eph T. 1937. Association of skull and limb bones in a new species of 
camel, with a review of the genus Pliauchenia (Abstract). Proc. Geol. Soc. Am. for 
1936, p. 388. 
Hay, Oliver P. 1913. Camels of the fossil genus Came/ops. Proc. U. S. Nat. Mus. 
46(2025) :267-77. Dec. 6. 
Leidy, Jooeph. 1854. Description of a fossil apparently indicating an extinct species 
of the camel tribe. Proc. Acad. Nat. Sci. Phila. 7:172-3. 
Matthew, W. D. 1918. Contributions to the Snake Creek fauna. Bul. Am. Mus. Nat. 
Hist. 38(7) :216-17. April 18. 
Matthew, W. D. and Harold J. Cook. 1909. A pliocene fauna from Nebraska. Bu!. 
Am. Mus. Nat. Hist. 26(27) :395-407. Sept. 3. 
Schultz, C. Bertrand. 1934. The Pleistocene mammals of Nebraska. Bu!. Neb. State 
Mus. 1(41):388. 
Wortman, J. L. 1898. The extinct Camelidae of North America and some associated 
forms. Bu!. Am. Mus. 10(7) :93-142. April 9. 
Fig. H.-Crown view of the anterior portion of mandible of Titanotylopus nebras-
kensis Barbour & Schultz. No. 1-6-9-33 S.P., The University of Nebraska State Museum . 
X 215. Drawing by Lynn Robert Wolfe. 
Fig. 12.- Crown view of the anterior portion of mandible of Gigantoeamelus frieki . 
No. 9-20-9-37 S.P., The University of Nebraska State Museum. X 2/5. Drawing by 
Lynn Robert Wolfe. 


A New Giant Camel
\u3ci\u3eGIGANTOCAMELUS FRICKI\u3c/i\u3e, gen. et sp. nov.

DigitalCommons@University of Nebraska

University of Nebraska - LincolnDigitalCommons@University of Nebraska - LincolnBulletin of the University of Nebraska StateMuseum Museum, University of Nebraska State1939A New Giant Camel GIGANTOCAMELUSFRICKI, gen. et sp. nov.Erwin Hinckley BarbourC. Bertrand SchultzFollow this and additional works at: http://digitalcommons.unl.edu/museumbulletinPart of the Entomology Commons, Geology Commons, Geomorphology Commons, OtherEcology and Evolutionary Biology Commons, Paleobiology Commons, Paleontology Commons,and the Sedimentology CommonsThis Article is brought to you for free and open access by the Museum, University of Nebraska State at DigitalCommons@University of Nebraska -Lincoln. It has been accepted for inclusion in Bulletin of the University of Nebraska State Museum by an authorized administrator ofDigitalCommons@University of Nebraska - Lincoln.Barbour, Erwin Hinckley and Schultz, C. Bertrand, "A New Giant Camel GIGANTOCAMELUS FRICKI, gen. et sp. nov." (1939).Bulletin of the University of Nebraska State Museum. 30.http://digitalcommons.unl.edu/museumbulletin/30BULLETIN OF THE UNIVERSITY OF NEBRASKA STATE MUSEUM Erwin Hinckley Barbour. Director VOLUME 2 LINCOLN, NEBRASKA, SEPTEMBER 1939 NUMBER 2 A New Giant Camel GIGANTOCAMELUS FRICKI, gen. et sp. nov. By ERWIN HINCKLEY BARBOUR AND C. BERTRAND SCHULTZ DEVELOPMENT OF THE BROADWATER-LISCO QUARRIES A LOWER Pleistocene deposit containing fossil vertebrates near Broad-water, Morrill county, Nebraska, has been reported upon by the writers, beginning three years ago.! Five fossil quarries have been opened since the site was discovered in 1936. A quantity of fine specimens from this area is now in the collections of the University of Nebraska State Museum. During June 1936, members of the Nebraska field party,2 while exploring east of the Broadwater quarries, discovered several localities that yielded Stegomastodon and camel bones. In one of these (SYz of sec. 11, T. 18 N., R. 46 W., Garden county) the distal end of an unusually large camel metapodial (No. 9-19-6-36 S.P.) and associated skeletal elements were found. The site was revisited in September 1937, and at that time numerous bones including a skull (No. 1-20-9-37 S.P.) were unearthed. Mr. Charles Sothman of Lisco, who had charge of the land where the camel bones were found, reported to the collectors that he had noticed similar fossil remains farther east. During the falls of 1937 and 1938 Messrs. Sweet, Middleswart and Chaloupka of Bridgeport did a considerable amount of exploratory work which was extended through the winters. Numerous prospects were located and test pits were dug. Three quarries were opened in the SEY4 of sec. 13, T. 18 N., R. 46 W., 3 miles east and 2Yz miles north of Lisco, Garden county. During 1938, from June 10 to October 1, the Lisco quarries were worked by a field party from the 1 See Bibliography, p. 26. Barbour & Schultz (1936, p. 308; 1937A, p. 1-10; 1937B, p. 185-9). 2 Field work at Broadwater was carried on under direction of the junior writer. The collecting party included Messrs. E. L. Blue, Thompson M. Stout, Frank Crabill, Gordon Graham, Jack Graham, David Abbott, Dean Ked, Fred Schall, Mrs. C. Bertrand Schultz, and was aided by Messrs, S. R. Sweet, T. C. Middleswart, W. F. Chaloupka, and John Ochoa. 17 18 UNIVERSITY OF NEBRASKA MUSEUM BULLETIN Fig, 5.--Gigalltocamelus jric/.;..i, new genus and species. C0111posite skeleton. No. 1-25-8-38 S.P., The University of Nebraska State Museum. X 1/30. The skeleton has been skillfully mounted without visible supports by Mr. Henry Reider and Mr. Frank Bell. University of Nebraska State Museum, assisted by a Works Progress Administration project under the supervision of Jack Graham and Paul Burkholder. Forty crates of rare camel material were shipped to the Museum from these quarries. A detailed report based on these specimens will appear in a forthcoming paper. In October 1938, several camel prospects were located east of the original quarries in Sljz of sec. 21, T. 18 N., R. 45, Garden county, on the land of Bertha Vocke and Conrad Wallace. The largest examples of Giganto-camelus have come from these new pits. The Lisco area is being worked extensively during the 1939 field season by a Museum party. The writers are grateful to Mr. Childs Frick for his special interest in the Lisco quarries and for permitting the study of his excellent collection of Megacamelus from Arizona. Thanks are also due to Messrs. S. R. Sweet, Fig. 6.-Crown view of skull of Gigantocamelus friel,;. No. l A·25 -8-38 S.P. , T he Uni versity of Nebraska State Museum. X 9/40. 20 UNIVERSITY OF NEBRASKA MUSEUM BULLETIN T. C. Middleswart, and W. F Chaloupka for their assistance in helping to develop the various camel quarries. Mr. Frank Ruby of Lisco aided the Museum parties by granting permission to excavate at the type locality. The Works Progress Administration staff in Nebraska, especially Mrs. Ethel May Sanmann, Mr. E. O. Raasch, and Miss Lilla Graham, liberally cooperated with the Museum in securing sufficient help in the field and laboratory to excavate and prepare the fossil camel bones. DESCRIPTION AND DISCUSSION Gigantocamelus fricki, NEW GENUS AND SPECIES Type.-Skull, No. IA-25-8-38 S.P., University of Nebraska State Museum. Referred.-Mandible, No. IB-25-8-38, S.P. (from different individual than skull), and composite skeleton, No. 1-25-8-38 S.P. (mounted with type skull; limb elements, except for metapodials, appear to be from one individual) and a large collection of skulls, rami and skeletal parts from the Lisco quarries. Locality.-Lisco quarries I, 2 and 3, SE\<4 of sec. 13, T. 18 N., R. 46 W., Garden county, Nebraska. Horizon.-Lower Pleistocene. Generic and Specific Characters.-Largest of known camelids; form and proportions approaching those of Megacamelus and Titanotylopus, but differing in dental formula and other characters; dental formula, 10-1/3 , C 1/1, P 3/3 , M 3/3, with premolar 2, above and below, absent; 1 3 rarely present; inferior and superior canines enlarged into tusks; posterior portion of canine very thin and with a sharp edge; mandible long and narrow, not so massive as that of Titanotylopus; skeletal parts more massive and much larger than those of Camelops; average metapodials and other limb elements more massive than those of Megacamelus. Associated Genera.-Smilodon, Megalonyx, Stegomastodon and Equus. The fauna of the Broadwater quarries in Morrill county is listed at the end of this report. Measurements.-See table of measurements on opposite page. Discussion.-The Lisco specimens appear to differ from any known camel remains. It is difficult to assign them to an already established genus and the writers consider the differences to be of generic value. With a large series of superior and inferior dentitions available, it is noted that the dental formula is very stable. The enlargement of the canines, as noted in Gigantocamelus, is unusual among the camels. A few examples from Lisco have smaller canines than the average, but these may represent females. Enlarged canines are also found in Titanotylopus (Barbour & Schultz 1934, p. 291-4), a large camel that lived later in the Pleistocene. This latter genus is known only from a partial mandible but it seems to be quite distinct from Gigantocamelus in the definite absence of P1 and the greatly reduced distance between the canine and Pa• Titanotylopus may be more closely related to Camelops. Childs Frick (1929, p. 107) has described a huge extinct camel, Megacamelus, from the Hopi Indian Agency of Arizona. This form has a A NEW GIANT CAMEL, GIGANTOCAMELUS FRICKI 21 MEASUREMENTS SKULL MEASUREMENTS lA-25-8-38 1-20-10-38 Length (max., including supraoccipital crest and premaxillae) . Condylo·basal length (condyles to anterior of premaxillae) .. Width (max., at orbits) ............ . Width (min., interorbital). Length of dental series (G-M 3 inclusive) Length, P 3~M 3 inclusive Length, P Lp 4 Length of superior molar series. Diastema, C to pl. Diastema, P 1 to P 3 . Diameter (max.) of canine at base Length of canine. Length of pl. JAW MEASUREMENTS IB-25-8-38 S.P. Length (max., including incisors). Length from posterior of condyle to anterior of canine Depth of ramus below anterior of third inferior molar Length of dental series (C-M3 inclusive). Length of inferior molar-premolar series (including P 1) Length, P 3-M 3 Length, P 3-P 4 .' Length, M I-M 3 Diastema, C-p 1 Diastema, P I-P 3 660 A 633 88 452 340 210 55 159 79 106 MEASUREMENTS OF SKELETAL ELEMENTS Length of: Scapula (max.) Humerus (articular) Radius (articular) Radius-ulna (max.). Metacarpal (max.) Femur (articular) ............... . Tibia (articular) Calcaneum (max.) Metatarsal (max.) 3E==estimated; A==approximate. S.P. S.P. mm. mm. 757 855E3 720 840 A 345 368 A 284 390 424 206 197 67 65 141 135 56 44 A 92 143 A 55 45 77 81 29 36 9-20-9-37 2-25-8-38 S.P. S.P. 635 E 603 A 94 443 372 254 60 201 52 104 90 327 2ll 51 162 100 1-25-8-38 S.P. 560 E 497 551 653 425 563 477 176 404 Fig. 7.-Palatine view of skull of Gigantocamelus fricki. No. IA-25-8-38 S.P., The University of Nebraska State Museum. X 9/40. Fig. 8.-Side view of skull of Gigantocamelus tricki. No. lA-2S- 8-3 8 S.P., The University of Nebraska State Museum. X 9/ 40. Fig. 9.-Crown view of mandible of Gigantocamelus tricki. No. 9 -20-9-37 S.P., The University of Nebraska State Museum. X 9/40. Note deciduous canines still present. 24 UNIVERSITY OF NEBRASKA MUSEUM BULLETIN marked facial fossa, I 3 is present and the canines are not enlarged. These characters are not observed in Gigantocamelus. The skeletal elements appear to be more massive in the Nebraska form. The parts used in the mount are from small individuals. Unfortunately, there were not enough of the largest bones for a mount. One of these giants would stand nearly 12 feet tall. Megatylopus (Matthew & Cook 1909, p. 396-401), an Upper Tertiary camel from Nebraska, cannot readily be compared with Gigantocamelus. Megatylopu.f is a smaller genus with a dentition, Pia, C1h, p3-21a-2, M31a. The reduction in the premolar series here suggests that these two genera represent independent lines of development. Pliauchenia spatula Cope, a species often referred to the genus Megatylopus, seems to be much more closely allied to Gigantocamelus fricki than to M. gigas, the genotypic species of Megatylopus. LIST OF MAMMALS FROM BROADWATER QUARRIES 4 I NSECTIVORA Sorex sp. Shrew. EDENTATA Mylodon sp. Ground sloth. LAGOMORPHA Lepus? sp. Jack rabbit. Sylvilagus? sp. Cottontail. RODENTIA Sciurid. Squirrel. Geomys sp. Pocket gopher. Thomomys? sp. Pocket gopher. Procastoroides sweeti Barbour and Schultz. Ancestral giant beaver. Dipoides? sp. Ancestral beaver. Peromyscus sp. Deer mouse. Ondatra sp. Muskrat. Mimomys? sp. Vole. Microtinid indct. Vole. Zapus sp. Jumping mOUse. Neotoma? sp. Wood rat. CARNIVORA Canis sp., near C. latrans Say. Coyote. Canis sp., near Canis (Aenocyon) dirus Leidy. Dire wolf. Satherium piscinaria middleswarti Barbour and Schlutz. Otter. Felid. Cat. PROBOSCIDEA Stegomastodon miri/icw primitiNls Osborn. Mastodont. PERISSODACTYLA Equus sp., near E. excclslIs Leidy. Horse. Equus sp., more primitive species. Horse. Equid, very light-limbed form; known only from a single metapodial. Horse. 40 The Broadwater quarries are located 4 miles east and 1 mile north of Broadwater, in NEY4 of sec. 20 and NWY4 of sec. 21, T. 19 N., R. 47 W., Morrill county, Nebraska, on the farm of Mr. Dan J. Boman. Fig. 10.-Side view of right ramus of Giganiocame/us f,';cki. No. 2·25·8·38 S.P., The University of Nebraska State Museum. X 9/40. ' 26 UNIVERSITY OF NEBRASKA MUSEUM BULLETIN ARTIODACTYLA Camelops sp., much larger form than C. l(ansanus Leidy. Camel. Tanupolama sp., much larger form than T. americanus (Wortman). Llama-like camel. Gigantocamelus fricki Barbour and Schultz. Giant camel. Capromeryx sp., larger form than C. fura/a Matthew. Small antelope. Antilocaprid, probably Tetrameryx. Four-horned antelope. The collection from the Broadwater quarries also contains the follow-ing unidentified vertebrates: PISCES Various forms. AMPHIBIA A large collection of amphibian material, especially frogs. Three or four families are represented. This material is now being studied by Dr. Edward H. Taylor of the Department of Zoology, University of Kansas. REPTILIA Turtle, perhaps two forms. Snake, at least one form. AVES Various forms. BIBLIOGRAPHY Barbour, Erwin H. and C. Bertrand Schultz. 1934. A new giant camel, Titanotyloplls nebraskensis, gen. et sp. nov. Eul. Neb. State Mus. 1 (36) :291-4. May. ------1936. Notice of a new bone bed in the early Pleistocene of Morrill county, Nebraska. Bul. Neb. State Mus. 1 (45) :383. April. ------1937A. An early Pleistocene fauna from Nebraska. Am. Mus. Nov. (942) :1-10. Sept. 10. ------1937B. Pleistocene and post-glacial mammals of Nebraska. In "Early Man," p. 185-9. Lippincott. Cope, E. D. 1875. On some new fossil Ungulata. Proc. Acad. Nat. Sci. Phila., p. 258. ------1884. The extinct Mammalia of the Valley of Mexico. Proc. Am. Philos. Soc. 22:16-18. ----1893. A preliminary report on the vertebrate paleontology of the Llano Estacado. 4th Ann. Rep. Geol. Surv. Texas. p. 70-3. Frick, Childs. 1929. History of the earth (Childs Frick Tertiary-Quaternary explora-tions, 1928). Nat. Hist. 24(1) :106-8. Jan.-Feb. Gregory, J05eph T. 1937. Association of skull and limb bones in a new species of camel, with a review of the genus Pliauchenia (Abstract). Proc. Geol. Soc. Am. for 1936, p. 388. Hay, Oliver P. 1913. Camels of the fossil genus Came/ops. Proc. U. S. Nat. Mus. 46(2025) :267-77. Dec. 6. Leidy, Jooeph. 1854. Description of a fossil apparently indicating an extinct species of the camel tribe. Proc. Acad. Nat. Sci. Phila. 7:172-3. Matthew, W. D. 1918. Contributions to the Snake Creek fauna. Bul. Am. Mus. Nat. Hist. 38(7) :216-17. April 18. Matthew, W. D. and Harold J. Cook. 1909. A pliocene fauna from Nebraska. Bu!. Am. Mus. Nat. Hist. 26(27) :395-407. Sept. 3. Schultz, C. Bertrand. 1934. The Pleistocene mammals of Nebraska. Bu!. Neb. State Mus. 1(41):388. Wortman, J. L. 1898. The extinct Camelidae of North America and some associated forms. Bu!. Am. Mus. 10(7) :93-142. April 9. Fig. H.-Crown view of the anterior portion of mandible of Titanotylopus nebras-kensis Barbour & Schultz. No. 1-6-9-33 S.P., The University of Nebraska State Museum . X 215. Drawing by Lynn Robert Wolfe. Fig. 12.- Crown view of the anterior portion of mandible of Gigantoeamelus frieki . No. 9-20-9-37 S.P., The University of Nebraska State Museum. X 2/5. Drawing by Lynn Robert Wolfe. 

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A New Giant Camel \u3ci\u3eGIGANTOCAMELUS FRICKI\u3c/i\u3e, gen. et sp. nov.

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