A list of prehistoric and extinct species whose fossils have been found in Port Kennedy Bone Cave, located within the limits of Valley Forge National Historical Park, located in Montgomery County, Pennsylvania, US.
Most of the fossils excavated from the site are deposited within the collections of the Academy of Natural Sciences Philadelphia, including those unearthed by both the crews of anthropologist Henry Mercer (1895–96) and paleontologist Edward Drinker Cope. Daggers denote extinct species.
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
† Long-nosed peccary [1] [2] [3] | †Mylohyus nasutus | One of two fossil peccaries known from Irvingtonian North America. Several fossils were referred to a new species named Mylohyus tetragonus by Edward Drinker Cope in 1899. [3] Fossils were also assigned to M. pennsylvanicus as well, [3] but all have been assigned to M. nasutus. [1] | ||
† Teleopternus orientalis [3] | Four molars. [4] | A species known from only a single specimen originally described by Cope in 1899. [3] The teeth are large, with Cope estimating it to be about the size of an elk. [3] [1] The phylogenetic placement of the species has been stated to be cervid or camelid. [5] [1] | ||
White-tailed deer [5] [1] | Odocoileus virginianus | Several specimens. | An extant species of deer, originally described from the site as a new species of mule deer, Cariacus laevicornis, by Cope (1896). [6] C. laevicornis was named based on several teeth and two partial antlers. [4] [6] |
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
American badger [7] | Taxidea taxus | Fossils of badgers are uncommon, making up little of the carnivoran fossils compared to canids and felids. [1] First referred to Taxidea americana, a synonym of T. taxus. [3] | ||
American black bear [1] [2] [8] | Ursus americanus | Port Kennedy features the earliest known fossils of black bears, with Cope mentioning their presence in 1895. [2] [1] Black bears are medium-sized and omnivorous, though smaller than Arctodus pristinus. [8] | ||
† Miracinonyx inexpectata [9] | A relative of the cougar which convergently evolved several cheetah-like characteristics built for running. It too was carnivorous and medium-sized, around 70 kg (150 lbs). [10] Fossils are known from much of the United States, including very mountainous regions such as the Grand Canyon, implying they may have had high-altitude adaptations. | |||
American river otter [7] | Lutra canadensis | A single partial mandible and teeth. [6] | The North American river otter is a medium-sized, semiaquatic carnivore endemic to eastern North America. The oldest fossils of American river otters come from Port Kennedy and Cumberland Cave. [11] [1] Cope considered the Port Kennedy specimen distinct, dubbing it L. rhoadsii, but it has been lumped with L. canadensis. [12] [1] | |
† Canis armbrusteri [1] | Teeth and postcranial remains. [1] | A canid larger than the other Canis species, C. priscolotrans, known from only several large upper carnassials and postcranial remains. [1] The fossils have been assigned to the species C. ambrusteri, though is slightly smaller than respective fossils known from Cumberland Cave, Maryland. [1] [13] Genetic data studied in 2021 found that the Rancholabrean species C. dirus actually belongs to the genus Aenocyon in a different lineage. This study implies that this species may be from the Aenocyon lineage. [14] | ||
Bobcat [1] | Lynx rufus | Mentioned by Cope (1895) as Lynx rufus, [2] but was referred to a new species, L. calcaratus, in 1899. [3] This species however is a synonym of L. rufus. [1] [11] | ||
† Mustela diluviana [7] [1] | A species of weasel unique to Port Kennedy, M. diluviana was named by Cope in 1899. However, Hay (1936) referred it to Martes , [7] though Daeschler, Spamer, & Paris (1993) kept it in Mustela. [1] | |||
† Panthera onca augusta [1] [15] [16] | Very few specimens, a rare species from the site. [15] | A giant subspecies of the modern jaguar. The material was not mentioned until 1941 by George Gaylord Simpson. [1] [15] | ||
Gray fox [3] [2] | Urocyon cinereoargenteus | Port Kennedy has one of the first records of the gray fox, which were first described by Cope in 1895 as specimens of Vulpes cinereoargenteus. [2] Gray foxes are small and omnivorous, often eating hares and mice. [17] [18] | ||
Jaguarundi [1] | Puma yagouaroundi | A single specimen. | The only fossil of a jaguarundi was initially assigned to Felis eyra, [2] but likely represent an early form of the jaguarundi. [11] | |
† Arctodus pristinus [8] [1] | Many individuals, including several partial skulls and mandibles. [3] | Arctodus was one of the largest known carnivorans in history and belonged to the Tremarctinae, a subfamily of bears endemic to the Americas. Studies suggest that much like many modern bears, Arctodus was an omnivore with no direct adaptations for either hypercarnivory or scavenging as previously believed. This species is smaller than the later Arctodus simus, at only 133 kg (293 lbs). [19] | ||
† Osmotherium spelaeum [7] | Many specimens. [7] [1] | Osmotherium spelaeum is endemic to Port Kennedy and very common, bearing the most specimens of any mustelid. [7] Cope (1899) described six species based on fragmentary material that are junior synonyms of O. speleaum. [1] [11] | ||
† Gulo schlosseri [1] | G. schlosseri is considered to be the ancestor of the extant Gulo gulo, with fossils exclusive to the Irvingtonian. [20] [11] [1] | |||
† Brachyprotoma obtusata [7] | A partial mandible bearing three teeth. | Originally described as Mephitis obtustata by Cope (1899), [3] it was a strange species of skunk that lived as far north as Yukon Territory, Canada. [21] The holotype was lost for many years, until being rediscovered in 1993 and figured. [1] | ||
† Smilodon gracilis [22] [23] | Few fragmentary specimens, including a partial skull. | Smilodon is among the most well-known mammals from the Ice Age, but S. gracilis is far smaller than later species. S. gracilis was described on the basis of a canine from Port Kennedy by Cope in 1880 and was the ancestor to Rancholabrean species. [24] [25] Unlike the American lion, which is a true cat, Smilodon was a member of the Machairodontinae. Based on the microwear texture of the teeth it has been suggested that Smilodon fed on both harder material and soft flesh, preferring the later following injuries to the jaws and teeth. | ||
† Canis edwardii [26] | Cope named a new species of Canis, C. priscolatrans, in his 1899 monograph on the fossils from the site. He named it on the basis of two molars and a premolar, the cotypes. [27] [3] Several paratypes were also assigned, including a partial canine and phalanx, these specimens of considerable size. [27] [3] The validity of C. priscolatrans was in question for decades, but the dimensions and anatomies of the teeth are not distinct from that of C. edwardii. [26] [28] Tedford et al (2009) declared in a nomen dubium, but tentatively considered it a synonym of C. edwardii based on their similarities. [26] |
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
†Wheatley's ground sloth [1] | †Megalonyx wheatleyi | Many specimens, including several partial skulls, mandibles, and associated remains. | Megalonyx wheatleyi is one of the most common species from Port Kennedy, with the site featuring one of the largest samples of the taxon. It was first named by Cope in 1871 along with 3 other Megalonyx species in his initial description of the site. The fossils he used were fragmentary, with the syntypes of M. wheatleyi consisting only of teeth. Cope named another species in 1899, M. scalper, but all species from the area have been synonymized with M. wheatleyi. |
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
Short-tailed shrew [1] [3] | Blarina brevicauda | A single jaw in matrix. | Like with many other Port Kennedy mammals, Cope considered the material from the site to be of Blarina distinct, dubbing B. simplicidens in his 1899 monograph. [3] It has been recognized as a junior synonym of B. brevicauda. [29] [1] |
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
Eastern cottontail [1] | Sylvilagus floridanus | "a large number of individuals" [1] | Originally assigned to the hare species Lepus sylvaticus , [30] but it is considered a junior synonym of Sylvilagus floridanus. [1] [11] | |
†Port Kennedy pika [1] | †Ochotona palatina | Teeth. | Cope described Praotherium palatinus based on several teeth in 1871, [30] but it was reassigned to the pika genus Ochotona in 1980. [11] However, its status is uncertain and has only fragmentary material. [1] [11] |
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
† Giant horse [1] | † Equus pectinatus | A large species of fossil horse, though the material has also been referred to the species E. giganteus, E. major , and E. fraternus . [3] [1] However, the most recent assessment placed all specimens within E. pectinatus. [1] | ||
† Hays' tapir [1] | † Tapirus haysii | A large species of tapir known from the Irvingtonian sediments of eastern North America. Tapirs are typically semiaquatic herbivores with long proboscis at the front of their skull. T. haysii was named previously by Joseph Leidy in 1860 [31] before a host of new fossils were described by Cope. [2] [3] Later in 1945, George Gaylord Simpson referred all of the Port Kennedy fossils to a new species he dubbed T. copeii, [32] a junior synonym of T. haysii due to lack of sufficient distinguishing traits. [33] [1] |
Common name | Species | Material | Notes | |
---|---|---|---|---|
† American mastodon [34] | † Mammut americanum | Many fragmentary specimens, including juveniles. | The American mastodon is the only known proboscidean from Port Kennedy and the largest animal from the site. [30] It consumed a variety of wooded plants, being a mixed browser in forests. [35] |
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
†Cope's muskrat [30] [36] | †Ondatra hiatidens | Five specimens. | A fossil species of muskrat, a semiaquatic type of herbivorous rodent endemic to Port Kennedy. It was originally named by Cope (1871), [30] though he later named the junior synonyms of Arvicola hiatidens and Anaptogonia cloacina in 1871 and 1899 respectively. [37] Though it has been noted that species determination with fossils from the site is difficult due to the small pool of samples. [38] [1] | |
†Diluvian water rat [1] [36] | †Neofiber diluvianus | Cope named two species of microtines, Microtus diluvianus and Schistodelta sulcata, but only the former is valid. [6] [3] M. diluvianus was moved to Neofiber by Hibbard (1955). [37] It was endemic to Port Kennedy, extant water rats being semiaquatic and nocturnal omnivores. | ||
Groundhog [1] | Marmota cf. monax | A partial humerus. | Not reported until it was described by Daeschler, Spamer, & Parris (1993). [1] | |
Meadow jumping mouse [3] | Zapus hudsonicus | A single partial mandible bearing one cheek tooth. [3] | Cope (1899) mentioned a specimen of Zapus hudsonicus, but it has been lost. [1] [3] | |
North American porcupine [39] [1] [3] | Erethizon dorsatum | [40] | ||
North American beaver [1] [3] [2] | Castor canadensis | A single mandible and three isolated teeth. [3] | ||
†Squirrel [1] [30] | †Sciurus calycinus | Two partial lower jaws. | Sciurus calycinus was dubbed by Cope in 1871, [30] but has been considered a synonym of the red squirrel, flying squirrel, or gray squirrel. There has not been an assessment, however. [1] | |
Voles [38] | Arvicolinae indet. | Vole fossils too fragmentary to be assigned on the specific level are known have been unearthed. [1] |
Only members of the family Coleopteridae have been reported from Port Kennedy, with chunks of clay containing fragments of beetles. [1] [41] Several novel species of beetles from the site were described by George H. Horn in 1874 on the basis of eltyra and thoraxes, though they have all been lost. [41]
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
"Ground beetles" [41] [1] | †Cychrus wheatleyi, Cychrus sp. | C. wheatleyi is endemic to Port Kennedy. | ||
"Woodland ground beetles" [1] [41] | Pterostichus sp. | |||
†"Colorful foliage ground beetles" [41] [1] | †Cymindis aurora | C. aurora is endemic to Port Kennedy. | ||
†"Vivid metallic ground beetles" [1] [41] | †Chlaenius punctulatus | C. punctulatus is endemic to Port Kennedy. | ||
"Notch-mouthed ground beetles" [1] [41] | †Dicaelus alutaceus, Dicaelus sp. | D. alutaceus is endemic to Port Kennedy. | ||
"Dung beetles" [1] [41] | †Choeridium. (=Ateuchus) ebeninum, †Phaenaeus antiquum, †Aphodius precursor | All "dung beetles" described by Horn are endemic to Port Kennedy. [41] |
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
Turkey | Meleagrinae indet. | A single specimen. | The turkey fossils have been identified previously as Meleagris gallopavo , but differed from Meleagris in some respects. [42] [1] |
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
Eastern box turtle [43] [1] | Terrepene carolina | Several specimens including carapaces and postcranial remains. [43] | Fossils had been referred to T. eurypygia by Hay (1908), but were reassigned to T. carolina by Parris & Daeschler (1995). [43] Many remains are assigned to cf. Terrapene sp., but likely belong to the same species. [43] | |
Blanding's turtle [43] | Emydoidea blandingii | A nearly complete plastron. [43] | ||
Eastern racer [1] | Coluber sp. | Vertebrae | The Coluber fossils from Port Kennedy have morphological similarities to Masticophis , but are more likely to be from the former due to their geography. [1] | |
†Tortoise [1] [43] | †Geochelone (Hesperotestudo) percrassa | A carapace and plastron fragments. [43] | Geochelone was a large, herbivorous genus of tortoises that lived in the Americas until their extinction, possibly brought upon by human arrival. [43] The only fossils of G. percrassa come from the cave, though they were originally described as the species Clemmys percrassa by Cope in his 1899 monograph. [3] | |
Wood turtle [43] | Clemmys insculpta | A single fragmentary shell. [43] |
Common name | Species | Material | Notes | Image |
---|---|---|---|---|
American beech [1] [44] | Fagus grandifola | |||
Pin oak [44] [1] | Quercus palustris | |||
White oak [1] [44] | Quercus alba | |||
Bur oak [44] [1] | Quercus macrocarpa | |||
American hazel [1] [44] | Corylus americana | |||
Pitch pine [1] [44] | Pinus rigida | |||
Cocksbur hawthorne or fireberry hawthorne [1] [44] | Crataegus crus-galli or C. chrysocarpa | |||
Hawthorne [44] [1] | Crataegus sp. | Fossils of a hawthorne that cannot be identified at the specific level. | ||
Shagbark hickory [44] | Carya avata | |||
Pignut hickory [44] | Carya glabra | |||
Mockernut hickory [44] | Carya tamentosa | |||
Virginia creeper [44] | Parthenocissus quinquefolia | |||
Sphagnum moss [44] | Sphagnum sp. | Common on blocks of matrix. [1] |
Smilodon is a genus of felids belonging to the extinct subfamily Machairodontinae. It is one of the best known saber-toothed predators and prehistoric mammals. Although commonly known as the saber-toothed tiger, it was not closely related to the tiger or other modern cats. Smilodon lived in the Americas during the Pleistocene epoch. The genus was named in 1842 based on fossils from Brazil; the generic name means "scalpel" or "two-edged knife" combined with "tooth". Three species are recognized today: S. gracilis, S. fatalis, and S. populator. The two latter species were probably descended from S. gracilis, which itself probably evolved from Megantereon. The hundreds of specimens obtained from the La Brea Tar Pits in Los Angeles constitute the largest collection of Smilodon fossils.
Ground sloths are a diverse group of extinct sloths in the mammalian superorder Xenarthra. Ground sloths varied widely in size, with the largest, belonging to genera Megatherium and Eremotherium, being around the size of elephants. Ground sloths are a paraphyletic group, as living tree sloths are thought to have evolved from ground sloth ancestors.
The dire wolf is an extinct canine. The dire wolf lived in the Americas during the Late Pleistocene and Early Holocene epochs. The species was named in 1858, four years after the first specimen had been found. Two subspecies are recognized: Aenocyon dirus guildayi and Aenocyon dirus dirus. The largest collection of its fossils has been obtained from the Rancho La Brea Tar Pits in Los Angeles.
Panthera atrox, better known as the American lion, also called the North American lion, or American cave lion, is an extinct pantherine cat. Panthera atrox lived in North America during the Pleistocene epoch, from around 340,000 to 12,800 years ago. The species was initially described by American paleontologist Joseph Leidy in 1853 based on a fragmentary mandible (jawbone) from Mississippi; the species name ('atrox') means "savage" or "cruel". The status of the species is debated, with some mammalogists and paleontologists considering it a distinct species or a subspecies of Panthera leo, which contains living lions. However, novel genetic evidence has shown that it is instead a distinct species derived from the Eurasian cave or steppe lion, evolving after its geographic isolation in North America. Its fossils have been excavated from Alaska to Mexico. It was about 25% larger than the modern lion, making it one of the largest known felids.
Miracinonyx is an extinct genus of felids belonging to the subfamily Felinae that was endemic to North America from the Pleistocene epoch and morphologically similar to the modern cheetah, although its apparent similar ecological niches have been considered questionable due to anatomical morphologies of the former that would have limited the ability to act as a specialized pursuit predator. The genus was originally known from fragments of skeletons, but nearly complete skeletons have been recovered from Natural Trap Cave in northern Wyoming.
Megalonyx is an extinct genus of ground sloths of the family Megalonychidae, native to North America. It evolved during the Pliocene Epoch and became extinct during at the end of the Late Pleistocene, living from ~5 million to ~13,000 years ago. The type species, M. jeffersonii, the youngest and largest known species, measured about 3 meters (9.8 ft) in length and weighed up to 1,000 kilograms (2,200 lb).
Platygonus is an extinct genus of herbivorous peccaries of the family Tayassuidae, endemic to North and South America from the Miocene through Pleistocene epochs, existing for about 10.289 million years. P. compressus stood 2.5 feet tall.
Oxyaena is an extinct genus of placental mammals from extinct subfamily Oxyaeninae within extinct family Oxyaenidae, that lived in Europe, Asia and North America during the early Eocene.
The Fram Formation is an Upper Devonian (Frasnian) sequence of rock strata on Ellesmere Island that came into prominence in 2006 with the discovery in its rocks of examples of the transitional fossil, Tiktaalik, a sarcopterygian or lobe-finned fish showing many tetrapod characteristics. Fossils of Laccognathus embryi, a porolepiform lobe-finned fish, and Qikiqtania, a close relative of Tiktaalik, were also found in the formation. The Fram Formation is a Middle to Upper Devonian clastic wedge forming an extensive continental facies consisting of sediments derived from deposits laid down in braided stream systems that formed some 375 million years ago, at a time when the North American craton ("Laurentia") was straddling the equator.
Nothrotheriops is a genus of Pleistocene ground sloth found in North America, from what is now central Mexico to the southern United States. This genus of bear-sized xenarthran was related to the much larger, and far more famous Megatherium, although it has recently been placed in a different family, Nothrotheriidae. The best known species, N. shastensis, is also called the Shasta ground sloth.
Tremarctos floridanus, occasionally called the Florida spectacled bear, Florida cave bear, or rarely Florida short-faced bear, is an extinct species of bear in the family Ursidae, subfamily Tremarctinae. T. floridanus was widespread in the Southeastern United States during the Rancholabrean epoch, with scattered reports of fossils from other parts of North America and from earlier epochs.
Arctodus is an extinct genus of short-faced bear that inhabited North America during the Pleistocene. There are two recognized species: the lesser short-faced bear and the giant short-faced bear. Of these species, A. simus was larger, is known from more complete remains, and is considered one of the most charismatic of North America's megafauna. A. pristinus was largely restricted to the Early Pleistocene of the Eastern United States, whereas A. simus had a broader range, with most finds being from the Late Pleistocene of the United States, Mexico and Canada. A. simus evolved from A. pristinus, but both species likely overlapped in the Middle Pleistocene. Both species are relatively rare in the fossil record.
Hemiauchenia is a genus of laminoid camelids that evolved in North America in the Miocene period about 10 million years ago. This genus diversified and expanded into to South America in the Late Pliocene approximately 3 to 2 million years ago, as part of the Great American Biotic Interchange. The genus became extinct at the end of the Pleistocene. The monophyly of the genus has been considered questionable, with phylogenetic analyses finding the genus to paraphyletic or polyphyletic, with some species suggested to be more closely related to living lamines than to other Hemiaucenia species.
The blunt-toothed giant hutia is an extinct species of giant hutia from Anguilla and Saint Martin that is estimated to have weighed between 50 and 200 kg. It was discovered by Edward Drinker Cope in 1868 in a sample of phosphate sediments mined in an unknown cave in Anguilla and sent to Philadelphia to estimate the value of the sediments. It is the sole species of the genus Amblyrhiza in the fossil family Heptaxodontidae.
The Port Kennedy Bone Cave is a limestone cave in the Port Kennedy section of Valley Forge National Historical Park, Pennsylvania, USA. The Bone Cave "contained one of the most important middle Pleistocene fossil deposits in North America".
Thecachampsa is an extinct genus of gavialoid crocodylian, traditionally regarded as a member of the subfamily Tomistominae. Fossils have been found from the eastern United States in deposits of Miocene age. Those named in the 19th century were distinguished primarily by the shape of their teeth, and have since been combined with T. antiquus. More recently erected species were reassigned from other genera, although their assignment to Thecachampsa has since been questioned.
Atlantochelys is an extinct genus of sea turtle from the Upper Cretaceous of New Jersey. For 163 years, only a partial humerus was known, but the second part of the same bone was found in 2012. The full size has been extrapolated as being 3 m (9.8 ft).
Brachyprotoma, also known as the short-faced skunks, is an extinct genus of large skunk that inhabited Pleistocene North America, with specimens having been found from Yukon to West Virgina.There currently exists only one accepted species, Brachyprotoma obtusata.
Osmotherium is an extinct genus of skunk from Pleistocene North America. it contains a single species, Osmotherium spelaeum. The genus name, Osmotherium, hails from Aincient Greek, osmḗ, "smell"; and therium, "beast"; meaning smelly beast. The species name, spelaeum, Latin for "cave", in reference to the sole locality which its remains have been found in, Port Kennedy Bone Cave.