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Fossil Species of Florida

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Mammalia, Perissodactyla, Hippomorpha, Equoidea, Equidae


Common Name: none

Alternate Scientific Name: Hippotherium ingenuum, Hipparion ingenuum, Nannippus ingenuus, Hipparion gratum

Source of Species Name: Not explicitly stated in Leidy’s (1885:33) original description. The species name is the neuter form of the Latin word ingenuus meaning of noble character.

Age Range: late middle to late Miocene; early Clarendonian (Cl2) to early Hemphillian (Hh2); from about 11 to 6 million years ago.

Florida Fossil Occurrences:

Florida map with occurrences indicated

Figure 1. Map of Florida, with black circles indicating counties where fossils of Cormohipparion ingenuum have been found (the circles do not indicate a specific location within the county where the fossils were found, and some counties may have two or more different locations producing this species).

Florida Fossil Sites with Cormohipparion ingenuum:
Alachua County—Gainesville Creeks Fauna (including Cofrin Creek, Gainesville High School Creek, Sharktooth Ravine, and Veterans Hospital Site); Haile 16C; Haile 19A; Haile 21A (reworked); Love Site; McGehee Farm; Pareners Branch Site
De Soto County—Peace River 1
Hamilton County—Occidental Phosphate Mine
Hardee County—Charlie Creek 1; Fort Green Mine; Hardee Complex Mine (C.F. Industries); Hickory Creek 1; Hickey Branch Site
Hillsborough County—Four Corners Mine; Leisey Shell Pit 1C; Kingsford Mine
Levy County—Mixsons Bone Bed
Manatee County—Four Corners Mine; Port Manatee
Marion County—Crystal Springs Mobil Homepark; Withlacoochee River 4A; Withlacoochee River 4X
Nassau County—St. Marys River
Polk County—Fort Meade Mine (Gardinier); Agricola Road Site, Hookers Prairie Mine; Nichols Mine Stream Matrix Locality; Grey Zone, Phosphoria Mine
Sarasota County—lag deposit below bed 11 in Quality Aggregates Shell Pit 8A

Overall Geographic Range: In addition to numerous records from Florida, the species is also known from the Lapara Creek Fauna of the Texas Coastal Plain (Goliad and Bee counties) and the Rancho Lobo Fauna of Honduras (Hulbert, 1988). Possibly known from the Tehuichila Fauna of Hidalgo, Mexico (see below). The type locality is Mixsons Bone Bed, Levy County, Florida (Cope, 1885; MacFadden, 1984).

Comments: Cormohipparion ingenuum was the first species of horse to be named from Florida. The species has been referred to many genera over the years. It was initially placed in Hippotherium, a genus first named from Europe, but in the late 1800s it was also widely used for North American hipparion horses (e.g., Cope, 1889). In the 1900s, most paleontologists favored the use of Hipparion instead of Hippotherium, and the species was routinely placed in this genus until 1940 (e.g., Gidley, 1907). In 1940, Nannippus was raised to generic rank and began to be used for smaller North American species previously assigned to Hipparion (e.g., Stirton, 1940). So between 1940 and 1988 the species was usually called Nannippus ingenuus (e.g., MacFadden, 1984). Finally, in 1988, it was assigned to the genus Cormohipparion, and made the type species of a new subgenus, Notiocradohipparion (Hulbert, 1988). So its full, formal scientific name is Cormohipparion (Notiocradohipparion) ingenuum (Leidy, 1884). However, those using the popular Paleobiology Database website should be aware that it uses an unpublished opinion that Cormohipparion is not a valid genus supposedly due to an inadequate type species (an opinion not shared by experts on fossil horses). So just to bring things full circle, the Paleobiology Database uses the name Hippotherium ingenuum for this species.

jaw of C. ingenuum

Figure 2. UF 32172, right mandible of Cormohipparion ingenuum with second premolar to third molar (p2-m3) from the Love Site, Alachua County, Florida; late Miocene. A, dorsal (occlusal) view; B, lateral view.

Since it was first named by Leidy (1884), Cormohipparion ingenuum has generally been considered a valid species, regardless of which genus it was placed in. The lone exception was a few years in the late 1800s when it was regarded as a junior synonym of a hipparion species from Nebraska, Pseudhipparion gratum, first by Cope (1889) and then by Lucas in Leidy and Lucas (1896). As more specimens of this species were found, the differences between the two species were apparent and the two were no longer thought to be the same species. Indeed they are no longer considered to be in the same genus. One potential senior synonym of Cormohipparion ingenuum is “Nannippus” montezuma. It is a late Miocene species from Mexico that was named by Leidy on the basis of a single tooth two years before he named Cormohipparion ingenuum. A second, similar specimen of “Nannippus” montezuma was figured by Carranza-Casteñada and Espinosa-Arrubarrena (1994). The enamel patterns on the occlusal surface of the two teeth from Mexico can be matched with Florida specimens referred to Cormohipparion ingenuum, and the two are similar in terms of size and crown height. But before the two can be synonymized, we must learn more about the Mexican species, especially its mandibular symphysis, lower cheekteeth, and development of the facial fossa, a depression on the side of the skull in front of the eye.

As described by Hulbert (1988), Cormohipparion ingenuum is medium-sized for a North American hipparion horse, with toothrow lengths generally in the range of 112-125 mm (ca. 4.5 inches). The complexity of enamel folds on the cheekteeth is moderate to high, but less than in Cormohipparion emsliei (Figure 3). The muzzle is very long, with the distance between the last incisor and the first cheektooth (second premolar) equal to about 75% of the toothrow length. During the late Miocene in Florida, Cormohipparion ingenuum is often found together with a second species of Cormohipparion, Cormohipparion plicatile. These two species are very similar in tooth enamel morphology, and single teeth or small samples of teeth can be difficult to assign to one or the other species with confidence. Lengths and widths of teeth and bones of Cormohipparion ingenuum are on average about 12% smaller than those of Cormohipparion plicatile, and, in an unworn state, the molars are about 9 mm (0.35 inches) shorter in Cormohipparion ingenuum. The facial fossa on Cormohipparion ingenuum is shallower and has a less distinct edge or rim than the one on Cormohipparion plicatile. Finally, Cormohipparion ingenuum has an enamel fold on the metaconid of the lower second premolar, both deciduous and permanent, that projects anteriorly, sometimes connecting with the paraconid (Figure 4). This feature is absent on these teeth in Cormohipparion plicatile.

teeth of Cormohipparion ingenuum

Figure 3. Upper cheekteeth of Cormohipparion ingenuum from Florida in occlusal view. A. UF 53401, right upper third premolar from the Love Site. B. UF 53388, right upper first molar from the Love Site. C. UF/TRO 7395, left upper second molar from one of the creeks in northwest Gainesville. This specimen shows a relatively high degree of enamel complexity for this species.

p2 of Cormohipparion ingenuum

Figure 4. UF 24632, left lower second premolar (p2) of Cormohipparion ingenuum from the Nichols Mine Stream Matrix Site, Polk County, Florida; late Miocene. The arrow points to the enamel projection that runs from the metaconid to the paraconid. Such a projection is characteristic of this species and its descendant, Cormohipparion emsliei.

Given its long, narrow muzzle and relatively short-crowned teeth (for a late Miocene horse), Cormohipparion ingenuum most likely fed on a mix of browse and green, fresh grasses. Other horses of the time, most notably within the genera Neohipparion and Calippus, show adaptations characteristic of horses for which grasses comprise more than half the diet. Stable carbon isotope analysis of tooth enamel from Cormohipparion ingenuum cannot determine the relative proportion of grass in its diet, as when it lived in Florida grasses mostly had the same proportions of stable carbon isotopes as shrubs and trees. However, such analysis of stable carbon isotopes does show that all equids from the Love Site, including Cormohipparion ingenuum, lived in relatively open habitats, in contrast to the tapirs, gomphothere, rhinos, and camelids (Feranec and MacFadden, 2006). Hoffman (2006) conducted a mesowear study on the teeth of some fossil equids from Florida. In grass-eating species, teeth wear relatively flat (low relief) and the cusps rapidly wear down and become blunt. Hoffman found that in a sample of Pleistocene Equus teeth, 100% had low relief and 73% had blunt cusps, signs of a pure grass diet in a dry environment. For three species of horse from the Love Site, Cormohipparion ingenuum had the fewest teeth with low relief (50%) and blunt cusps (15%). In contrast, 75% of the teeth of Neohipparion trampasense had low relief and 41% had blunt cusps. From this it can be inferred that the percentage of grass in the diet of Cormohipparion ingenuum was less than in Neohipparion trampasense, at least within these co-existing populations.

During the late Miocene, Cormohipparion ingenuum was one of the more common horses in Florida. At most fossil sites of that age, it is regularly one of the three most abundant species of horse. The youngest records of the species are at the Withlacoochee River 4A and 4X sites, in the Hemphillian 2 interval, about 6.5 million years ago. It is succeeded by Cormohipparion emsliei, which first appears about that time, and then persists until about 2 million years ago Because both of these species have relatively long chronologic ranges, they are not particularly useful for biochronology.

Scientific Publications and Other References Cited:

Carranza-Casteñada, Ó., and L. Espinosa-Arrubarrena. 1994. Late Tertiary equids from the state of Hidalgo, Mexico. Revista Mexicana de Ciencias Geológicas 11(2):182-192. http://dialnet.unirioja.es/servlet/articulo?codigo=281811&orden=0&info=link

Cope, E. D. 1889. A review of the North American species of Hippotherium. Proceedings of the American Philosophical Society 26:429-458. http://www.jstor.org/stable/983183

Feranec, R. S., and B. J. MacFadden. 2006. Isotopic discrimination of resource partitioning among ungulates in C3-dominated communities from the Miocene of Florida and California. Paleobiology 32(2):191-205. http://www.bioone.org/doi/full/10.1666/05006.1

Gidley, J. W. 1907. Revision of the Miocene and Pliocene Equidae of North America. Bulletin of the American Museum of Natural History 23(35):865-934. http://hdl.handle.net/2246/1429

Hoffman, J. M. 2006. Using stable carbon isotope, microwear, and mesowear analyses to determine the paleodiets of Neogene ungulates and the presence of C4 or C3 grasses in northern and central Florida. Master’s thesis, University of Florida, Gainesville, 101 p. http://purl.fcla.edu/fcla/etd/UFE0017840

Hulbert, R. C. 1988. Cormohipparion and Hipparion (Mammalia, Perissodactyla, Equidae) from the Late Neogene of Florida. Bulletin of the Florida State Museum 33:229–338. http://ufdcweb1.uflib.ufl.edu/ufdc/?b=UF00099409

Leidy, J. 1885. Rhinoceros and Hippotherium from Florida. Proceedings of the Academy of Natural Sciences of Philadelphia 37:32-33. http://www.jstor.org/stable/4061085

Leidy, J., and F. A. Lucas. 1896. Fossil vertebrates from the Alachua Clays of Florida. Transactions of the Wagner Free Institute of Science of Philadelphia 4:1-61. http://books.google.com/books/download/Fossil_Vertebrates_from_the_Alachua_Clay.pdf?id=7bkrAAAAYAAJ&output=pdf&sig=ACfU3U11WDC2nkV_RKWW8XdaVzGnt5orCA

MacFadden, B. J. 1984. Systematics and phylogeny of Hipparion, Neohipparion, Nannippus, and Cormohipparion (Mammalia, Equidae) from the Miocene and Pliocene of the New World. Bulletin of the American Museum of Natural History 179:1-196. http://hdl.handle.net/2246/997

Stirton, R. A. 1940. Phylogeny of North American Equidae. University of California Publication, Bulletin of the Department of Geological Science 25:165-198.

Original Author(s): Richard C. Hulbert Jr.

Original Completion Date: October 17, 2013

Editor(s) Name(s): Richard C. Hulbert Jr.

Last Up-dated On: October 18, 2013

This material is based upon work supported by the National Science Foundation under Grant Number CSBR 1203222, Jonathan Bloch, Principal Investigator. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.

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