|Panthera leo atrox
Temporal range: Pleistocene, 0.34–0.011 Ma
|Skeleton from the La Brea tar pits at the George C. Page Museum|
|Subspecies:||P. l. atrox|
|Panthera leo atrox
|The maximal range of cave lions - red indicates Panthera spelaea, blue Panthera atrox, and green Panthera leo leo/Panthera leo persica.|
The American lion (Panthera leo atrox)[note 1] – also known as the North American cave lion – is an extinct subspecies of lion that lived in North America during the Pleistocene epoch (340,000 to 11,000 years ago). Genetic analysis has revealed that it was the sister lineage to the Eurasian cave lion. It was part of the Pleistocene megafauna, a wide variety of large mammals that lived at the time. The majority of American lion fossils have come from the La Brea Tar Pits.
The American lion was initially considered a distinct species of Pantherinae, and designated as Panthera atrox / /, which means "cruel" or "fearsome panther" in Latin. Some paleontologists accepted this view, but others considered the American lion to be most closely related to the modern lion (Panthera leo) and its extinct relative, the Eurasian cave lion (Panthera leo spelaea or P. spelaea). It was later assigned as a subspecies of P. leo (P. leo atrox) rather than as a separate species.[note 1]
Cladistic studies using morphological characteristics have been unable to resolve the phylogenetic position of the American lion. One study considered the American lion, along with the cave lion, to be most closely related to the tiger (Panthera tigris), citing a comparison of the skull; the braincase, in particular, appears to be especially similar to the braincase of a tiger. Another study suggested that the American lion and the Eurasian cave lion were successive offshoots of a lineage leading to a leopard-extant lion clade. A more recent study comparing the skull and jaw of the American lion with other pantherines concluded that it was not a lion but a distinct species. It was proposed that it arose from pantherines that migrated to North America during the mid-Pleistocene and gave rise to American lions and jaguars (Panthera onca). Another study grouped the American lion with P. leo and P. tigris, and ascribed similarities to P. onca to convergent evolution.
However, mitochondrial DNA sequence data from fossil remains suggests that the American lion (P. l. atrox) represents a sister lineage to the Eurasian cave lion (P. l. spelaea), and likely arose when an early cave lion population became isolated south of the North American continental ice sheet about 340,000 years ago. The most recent common ancestor of the P. l. atrox lineage is estimated to have lived about 200,000 (118,000 to 346,000) years ago. This implies that it became genetically isolated from P. l. spelaea before the start of the Illinoian glaciation (a spelaea population is known to have been present in eastern Beringia by that time, where it persisted until at least 11,925 ± 70 years ago). This separation was maintained during the interstadials of the Illinoian and following Wisconsin glaciations as well as during the Sangamon interglacial between them. Boreal forests may have contributed to the separation during warmer intervals; alternatively, a reproductive barrier may have existed. The study also indicates that the modern lion is the closest living relative of P. atrox and P. spelaea.
The American lion is estimated to have measured 1.6 to 2.5 m (5 ft 3 in to 8 ft 2 in) from the tip of the nose to the base of the tail and stood 1.2 m (3.9 ft) at the shoulder. Thus, it was smaller than its contemporary competitor, the giant short-faced bear, which was the largest carnivoran of North America at the time, and arguably the saber-toothed cat, Smilodon populator, which may have weighed up to 400 kg (880 lb). In 2008, the American lion was estimated to weigh up to 420 kg (930 lb). A study in 2009 showed an average weight of 256 kg (564 lb) for males and 351 kg (774 lb) for the largest specimen analyzed. A study in 2012 estimated a range of 235–523 kg (518–1,153 pounds) for males and 175–365 kg (386–805 pounds) for females, which suggests that the lion was heavier than Smilodon.
About 80 American lion individuals have been recovered from the La Brea Tar Pits in Los Angeles, so their morphology is well known. Their features strongly resemble those of modern lions, but they were considerably larger, and are believed to have been the largest subspecies of lion.
Preserved skin remains found with skeletal material thought to be from the American lion in caves in Argentina indicate that the animal was reddish in color. Cave paintings from in El Ceibo in the province of Santa Cruz seem to confirm this, and reduce the possibility of confusion with fossil jaguars, as similar cave paintings show the latter cat accurately as being yellow in color.
The earliest lions known in the Americas south of Alaska are from the Sangamonian Stage - the last interglacial period - following which, the American lion spread from Alberta to Maryland, reaching as far south as Chiapas, Mexico. It was generally not found in the same areas as the jaguar, which favored forests over open habitats. It was absent from eastern Canada and the northeastern United States, perhaps due to the presence of dense boreal forests in the region. The American lion was formerly believed to have colonized northwestern South America as part of the Great American Interchange. However, the fossil remains found in the tar pits of Talara, Peru actually belong to an unusually large jaguar. On the other hand, fossils of a large felid from late Pleistocene localities in southern Chile and Argentina traditionally identified as an extinct subspecies of jaguar, Panthera onca mesembrina, have been reported to be remains of the American lion.
The American lion inhabited savannas and grasslands like the modern lion. In some areas of their range, American lions lived under cold climatic conditions. They probably used caves for shelter from the cold weather in those areas.[note 2] They may have lined their dens with grass or leaves, as the Siberian tiger does, a tiger subspecies that lives in North Asia.
The remains of American lions are not as abundant as those of other predators like Smilodon fatalis or dire wolves (Canis dirus) at the La Brea Tar Pits, which suggests that they may have been smart enough to avoid tar traps. American lions likely preyed on deer, horses, camels, tapirs, American bison, mammoths, and other large ungulates (hoofed mammals). Evidence for predation of bison by American lions is particularly strong as a mummified carcass nicknamed "Blue Babe" was discovered in Alaska with clear bite and claw marks from lions. Based on the largely intact nature of the carcass, it probably froze before the lions could devour it. The American lion went extinct along with most of the Pleistocene megafauna during the Quaternary extinction event. The most recent fossil, from Edmonton, dates to 11,355 ± 55 years ago. American lion bones have been found in the trash heaps of Paleolithic Native Americans, suggesting human predation may have contributed to its extinction.
A replica of the jaw of the first American lion specimen to be discovered can be seen in the hand of a statue of famous paleontologist Joseph Leidy, currently standing outside the Academy of Natural Sciences in Philadelphia.
- Asiatic lion
- Barbary lion
- Big cat
- Cape lion
- Central African lion
- Early Middle Pleistocene European cave lion
- East African lion
- European lion
- Southern African lion
- West African lion
- List of largest carnivorans
- List of largest prehistoric carnivorans
- The authors of the most recent genetic study, Barnett et al., classify the American lion as the subspecies P. l. atrox. However, as of 2014, it is more commonly accorded full species status as P. atrox in the scientific literature, according to Google Scholar (see talk page).
- This source confuses spelaea, which is the form found in Alaska and the Yukon, with atrox, the form known from Alberta southwards.
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- Marisol Montellano, Ballesteros; Carbot-Chanona, Gerardo. "Panthera leo atrox (Mammalia: Carnivora: Felidae) in Chiapas, Mexico". The Southwestern Naturalist. 54 (2): 217–222. doi:10.1894/clg-20.1.
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