Panthera spelaea Temporal range: Middle-Late Pleistocene, | |
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Skeleton in Natural History Museum, Vienna | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Mammalia |
Order: | Carnivora |
Suborder: | Feliformia |
Family: | Felidae |
Subfamily: | Pantherinae |
Genus: | Panthera |
Species: | †P. spelaea |
Binomial name | |
†Panthera spelaea Goldfuss, 1810 | |
Subspecies | |
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Red indicates the maximal range of Panthera spelaea, blue Panthera atrox , and green Panthera leo . | |
Synonyms | |
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Panthera spelaea, commonly known as the cave lion (or less commonly as the steppe lion), is an extinct Panthera species that was native to Eurasia and northwest North America during the Pleistocene epoch. Genetic analysis of ancient DNA has revealed that while closely related, it was a distinct species genetically isolated from the modern lion (Panthera leo), [1] with the genetic divergence between the two species estimated at around 500,000 years ago. [2] The earliest fossils of the P. spelaea lineage (either regarded as the separate species Panthera fossilis or the subspecies P. spelaea fossilis) in Eurasia date to around 700,000 years ago (with possible late Early Pleistocene records). [3] It is closely related and probably ancestral to the American lion (Panthera atrox). [2] The species ranged from Western Europe to eastern Beringia in North America, and was a prominent member of the mammoth steppe fauna, and an important apex predator across its range. It became extinct about 13,000 years ago. [4] It closely resembled living lions with a coat of yellowish-grey fur though unlike extant lions, males appear to have lacked manes.
Panthera spelaea interacted with both Neanderthals and modern humans, who used their pelts and in the case of the latter, depicted them in artistic works.
In 1774, Zoolithenhöhle cave near the village of Burggaillenreuth in Bavaria, southern Germany was brought to scientific attention by Johan Friedrich Esper, who realised that the bones of extinct animals were present in the cave. [5] In 1810, a fossil skull from the cave was given the scientific name Felis spelaea by Georg August Goldfuss. [6] It possibly dates to the Last Glacial Period. [7] [1] [4]
Several anatomical studies of remains of Panthera spelaea were conducted during the early-mid 19th century, who generally agreed that the species had lion affinities. [4] During the 20th century and the first decade of the 21st century, Panthera spelaea was often regarded as a subspecies of the modern lion, and therefore as Panthera leo spelaea. [8] [9] [10] [1] One author considered the cave lion to be more closely related to the tiger based on a comparison of skull shapes, and proposed the scientific name Panthera tigris spelaea. [11]
Results from morphological studies showed that it is distinct in cranial and dental anatomy to justify the specific status of Panthera spelaea. [12] [13] Results of phylogenetic studies also support this assessment. [14] [15] [16]
In 2001, the subspecies Panthera spelaea vereshchagini was proposed for seven specimens found in Siberia and Yukon, which have smaller skulls and teeth than the average P. spelaea. [17] Before 2020, genetic analysis using ancient DNA provided no evidence for their distinct subspecific status; DNA signatures from P. spelaea from Europe and Alaska were indistinguishable, suggesting one large panmictic population. [15] [18] However, analysis of mitochondrial genome sequences from 31 cave lions showed that they fall into two monophyletic clades. One lived across western Europe and the other was restricted to Beringia during the Pleistocene. For this reason, the Beringian population is considered a distinct subspecies, P. s. vereshchagini. [18] [19]
Lion-like pantherine felids first appeared in the Tanzanian Olduvai Gorge about 1.7 to 1.2 million years ago. These cats dispersed into Eurasia from East Africa around the end of the Early Pleistocene and the beginning of the Middle Pleistocene, giving rise to Panthera fossilis. The oldest widely accepted fossils of P. fossilis in Europe date to around 700,000 years ago, such as that from Pakefield in England, [20] [21] [3] [22] with possible older fossils from Western Siberia dating to the late Early Pleistocene, [23] with a 2024 study suggesting a presence in Spain by 1 million years ago. [24] Different authors considered Panthera fossils as either a distinct species ancestral to P. spelaea, [25] or as a subspecies of P. spelaea. [22] [26] Recent nuclear genomic evidence suggest that interbreeding between modern lions and all Eurasian fossil lions took place up until 500,000 years ago, but by 470,000 years ago, no subsequent interbreeding between the two lineages occurred. [20] [1] [2]
The following cladogram shows the genetic relationship between P. spelaea and other pantherine cats. [16]
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The arrival of Panthera (spelaea) fossilis in Europe was part of a faunal turnover event around the Early-Middle Pleistocene transition in which many of the species that characterised the preceeding late Villafranchian became extinct. In the carnivore guild, this notably included the giant hyena Pachycrocuta and the sabertooth cat Megantereon . Following the arrival of Panthera (spelaea) fossilis the lion-sized sabertooth cat Homotherium and the "European jaguar" Panthera gombaszoegensis became much rarer, [24] ultimately becoming extinct in Europe during the late Middle Pleistocene, with competition with lions suggested to be a likely important factor. [27] [28]
Specimens intermediate between P. fossilis and Late Pleistocene P. spelaea are referred to as the subspecies P. s. intermedia. [21] The transition from P. fossilis to Late Pleistocene P. spelaea shows significant reduction in body size, as well as changes in skull and tooth morphology. [29] Mitochondrial DNA sequence data from fossil lion remains show that the American lion represents a sister group of Late Pleistocene P. spelaea, and likely arose when an early P. spelaea population became isolated south of the Cordilleran Ice Sheet. Initially this was suggested to be around 340,000 years ago, [15] but later studies suggested that the split between the two species was probably younger, around 165,000 years ago, consistent with the late first appearance of P. spelaea in Eastern Beringia (now Alaska and adjacent regions) during the Illinoian (around 190-130,000 years ago). [30]
Carvings and cave paintings of cave lions, which were discovered in the Lascaux and Chauvet Caves in France, were dated to 15,000 to 17,000 years old. [31] [32] A drawing in the Chauvet cave depicts two cave lions walking together. The one in the foreground is slightly smaller than the one in the background, which has been drawn with a scrotum and without a mane. [33] Such cave paintings suggest that male cave lions completely lacked manes, or at most had very small manes. [4]
Early members of the cave lion lineage assigned to Panthera (spelaea) fossilis during the Middle Pleistocene were considerably larger than individuals of P. spelaea from the Last Glacial Period and modern lions, with some of these individuals having an estimated length of 2.5–2.9 metres (8.2–9.5 ft), shoulder height of 1.4–1.5 metres (4.6–4.9 ft) and body mass of 400–500 kilograms (880–1,100 lb), respectively, making them among the largest cats to have ever lived. The Late Pleistocene Panthera spelaea spelaea was noticeably smaller though still large relative to living cats, with an estimated length of 2–2.1 metres (6.6–6.9 ft) and shoulder height of 1.1–1.2 metres (3.6–3.9 ft), respectively, The species showed a progressive size reduction over the course of the Last Glacial Period up until its extinction, with the last P. spelaea populations comparable in size to small-sized modern lions, with a body mass of only 70–90 kilograms (150–200 lb), a body length of 1.2–1.3 metres (3.9–4.3 ft) and shoulder height of 70–75 centimetres (2.30–2.46 ft) respectively. [26] [34]
P. spelaea had a relatively longer and narrower muzzle compared to that of the extant lion, with the zygomatic region being strongly arched, with the carnassial teeth having differences in cusp morphology (displaying preparastyles). [4] Like modern lions, females were smaller than males. [35] Compared to the earlier P. (spelaea) fossilis, Late Pleistocene P. spelaea spelaea differs (in addition to previously mentioned size differences) in having larger incisor teeth, more narrow and flattened canines, as well narrower upper and lower third and fourth premolars, which display some differences in cusp morphology, with the lower first molar being narrower and more elongate. [26] The orbits (eye sockets) of P. spelaea spelaea are also relatively larger and muzzle marginally narrower compared to P. (spelaea) fossilis, with the nasal region also being proportionally narrower, while the postorbital and mastoid regions of the skull are wider, with the tympanic bullae being more inflated. [36]
In 2016, hair found near the Maly Anyuy River was identified as cave lion hair through DNA analysis. Comparison with hair of a modern lion revealed that cave lion hair was probably similar in colour as that of the modern lion, though slightly lighter. In addition, the cave lion is thought to have had a very thick and dense undercoat comprising closed and compressed yellowish-to-white wavy downy hair with a smaller mass of darker-coloured guard hairs, possibly an adaptation to the Ice Age climate. [37] While juveniles fur coat colour was yellowish, adult cave lions are suggested to have had grey fur. [19]
During the Last Glacial Period, P. spelaea formed a contiguous population across the mammoth steppe, from Western Europe to northwest North America. [4] [38] It was widely distributed in the Iberian Peninsula, [39] Italian Peninsula, [40] Southeast Europe, [41] Great Britain, [4] Central Europe, [42] [43] [44] the East European Plain, [4] the Ural Mountains, [45] most of Northeast Asia (ranging as far south as Northeast China [46] and possibly the Korean peninsula [47] ), and across the Bering land bridge into Alaska and Yukon. [4] The cave lion had a wide elevation range, with finds extending up over 2,000 metres (6,600 ft) above sea level in the European Alps and in Buryatia in Northern Asia, though they probably did not occupy mountainous habitats all-year round. [48] The cave lion probably inhabited predominantly open habitats such as steppe and grasslands although it would have also have occurred in open woodlands as well. [4] While during the Last Glacial Period it was often associated with cold environments, the species also inhabited temperate environments, [49] such as in Europe during the Last Interglacial/Eemian. [50]
P. spelaea was one of the keystone species of the mammoth steppe, being one of the main apex predators alongside the gray wolf, cave hyena and brown bear. [52] Large amounts of bones belonging to P. spelaea were excavated in caves, where bones of cave hyena, cave bear and Paleolithic artefacts were also found. [53] [54] Despite their common name, "cave lions" probably only infrequently if ever used caves, and were present in regions where caves were absent. [55] Some of these accumulations of cave lion bones in cave hyena dens have been attributed to confrontations between cave hyenas and cave lions over carcasses, with the remains of cave lions killed in these confrontations subsequently transported to the dens. [56] [55]
Isotopic analyses of bone collagen samples extracted from remains in Europe [57] [52] and East Beringia [58] indicate that reindeer were particularly prominent in the diet of cave lions in these regions during the Last Glacial Period. [52] Cave lions also seem to have opportunistically preyed on the cubs of cave bears. [52] [57] Isotopic analysis of other European specimens suggests a diet including wild horse, woolly mammoth and cave bears for these individuals. [52] It may have sought out hibernating bears in montane caves as a food source during the winter. [59] Bite marks found on the bones of straight-tusked elephants in Neumark Nord, Germany, dating to the Last Interglacial, have been suggested to be the result of scavenging by cave lions. [60]
Other possible prey species were giant deer, red deer, muskox, aurochs, wisent, steppe bison, and young woolly rhinoceros. It likely competed for prey with the European leopards, cave hyenas, brown bears and grey wolves in Eurasia, [62] along with short-faced bears, Homotherium , and Beringian wolves in Beringia. [52]
Whether or not cave lions existed in prides like modern lions is unclear. [19] Isotopic analysis on cave lions by Hervé Bocherens and colleagues lead them to suggest that cave lions may have been solitary, due to cave lions shifting their diets after the disappearance of cave hyenas, carcasses being consumed the cave hyenas as well, suggests they were at a competitive disadvantage, and the scattering of isotopic data between individuals. [57] [52] [63] Some other authors have also argued that the absence of manes in cave lions suggests that cave lions did not live in prides, given the importance of manes in the social hierarchy of modern lions. [19] Boeskorov et al. 2021 suggested both European and Beringian cave lions may have hunted in larger prides than modern lions because sexual dimorphism in cave lions was more pronounced than in modern African lions and solitary big cats. However, they admitted the data is insufficient to come down to a certain conclusion. [19]
Cave lion cubs appear to have lived in dens during their earliest stages of life, like modern lion cubs and were likely solely raised by females, like living Panthera species. [19]
Cave lions were hunted and their pelts exploited in Europe by Neanderthals during the Middle Paleolithic, [64] and during the Upper Paleolithic by modern humans in Spain as evidenced in the La Garma site dating to the Magdalenian. [65] Modern humans also drew cave paintings of cave lions, engraved their likeness on bones and created sculptures of them, including the famous anthropomorphic lion-man figure from Hohlenstein-Stadel cave in Germany dating to around 41-35,000 years ago with the body of a human and the head of a lion. Cave lion canines with perforated holes may have been worn as personal ornaments. [64] Decorated stones with engravings representing cave lions have been found in southern Italy. [66]
Radiocarbon dating suggests that the species went extinct approximately simultaneously across its range during the last few thousand years of the Late Pleistocene, around 14-15,000 years ago, possibly surviving around 1000 years later in the far east North American portion of its range. This timing roughly corresponds to the onset of the Bølling–Allerød Interstadial warm period and the consequent collapse of the mammoth steppe ecosystem. The precise cause of its extinction is unclear, but possibly involved environmental change from open habitats to closed forests, changes in prey abundance, as well as human impact, though it is difficult to distentangle the precise causes of its extinction. [4] Cave lions appear to have undergone a population bottleneck that considerably reduced their genetic diversity between 47,000 and 18,000 years ago, probably driven at least in part by climatic instability. [67]
In 2008, a well-preserved mature cave lion specimen was unearthed near the Maly Anyuy River in Chukotka Autonomous Okrug, which still retained some clumps of hair. [68]
In 2015, two frozen cave lion cubs, estimated to be between 25,000 and 55,000 years old, were discovered close to the Uyandina River in Yakutia, Siberia in permafrost. [69] [70] [71] Research results indicate that the cubs were likely barely a week old at the time of their deaths, as their milk teeth had not fully erupted. Further evidence suggests the cubs were hidden at a den site until they were strong enough to follow their mother back to the pride, as with modern lions. Researchers believe that the cubs were trapped and killed by a landslide, and that the absence of oxygen underground hindered their decomposition and allowed the cubs to be preserved in such good condition. A second expedition to the site where the cubs were found was planned for 2016, in hopes of finding either the remains of a third cub or possibly the cubs' mother. [72]
In 2017, another frozen specimen, thought to be a lion cub, was found in Yakutia on the banks of the Tirekhtyakh River (Russian : Тирехтях), a tributary of the Indigirka River. This male cub was thought to be slightly older than the 2015 cubs at the time of its death; it is estimated to have been around one and a half to two months. [73] In 2018, another preserved carcass of a cub was found in a location 15 m (50 ft) away. It was considered to be around a month old when it died approximately 50,000 years ago, and presumed to be a sibling of the male cub. [74] However, carbon dating showed them to have lived about 15,000 years apart, with the female estimated to have lived 28,000 years ago, and the male 43,448 years ago. [19] Both cubs were well preserved, albeit with a few damages, with the female possibly being the "best preserved" animal discovered from the Ice age. [75]
The lion is a large cat of the genus Panthera, native to Africa and India. It has a muscular, broad-chested body; a short, rounded head; round ears; and a dark, hairy tuft at the tip of its tail. It is sexually dimorphic; adult male lions are larger than females and have a prominent mane. It is a social species, forming groups called prides. A lion's pride consists of a few adult males, related females, and cubs. Groups of female lions usually hunt together, preying mostly on medium-sized and large ungulates. The lion is an apex and keystone predator.
The leopard is one of the five extant cat species in the genus Panthera. It has a pale yellowish to dark golden fur with dark spots grouped in rosettes. Its body is slender and muscular reaching a length of 92–183 cm (36–72 in) with a 66–102 cm (26–40 in) long tail and a shoulder height of 60–70 cm (24–28 in). Males typically weigh 30.9–72 kg (68–159 lb), and females 20.5–43 kg (45–95 lb).
Panthera is a genus within the family Felidae, and one of two extant genera in the subfamily Pantherinae. It contains the largest living members of the cat family. There are five living species: the jaguar, leopard, lion, snow leopard and tiger, as well as a number of extinct species, including the cave lion and American lion.
Homotherium is an extinct genus of scimitar-toothed cat belonging to the extinct subfamily Machairodontinae that inhabited North America, Eurasia, and Africa during the Pliocene and Pleistocene epochs from around 4 million to 12,000 years ago. It was one of the last surviving members of the subfamily alongside the more famous sabertooth Smilodon, to which it was not particularly closely related. It was a large cat, comparable in size to a lion, functioning as an apex predator in the ecosystems it inhabited. In comparison to Smilodon, the canines of Homotherium were shorter, and it is suggested to have had a different ecology from Smilodon as a pursuit predator adapted to running down large prey in open habitats, with Homotherium also proposed to have likely engaged in cooperative hunting.
The woolly rhinoceros is an extinct species of rhinoceros that inhabited northern Eurasia during the Pleistocene epoch. The woolly rhinoceros was a member of the Pleistocene megafauna. The woolly rhinoceros was covered with long, thick hair that allowed it to survive in the extremely cold, harsh mammoth steppe. It had a massive hump reaching from its shoulder and fed mainly on herbaceous plants that grew in the steppe. Mummified carcasses preserved in permafrost and many bone remains of woolly rhinoceroses have been found. Images of woolly rhinoceroses are found among cave paintings in Europe and Asia. The range of the woolly rhinoceros contracted towards Siberia beginning around 17,000 years ago, with the youngest known records being around 14,000 years old in northeast Siberia, coinciding with the Bølling–Allerød warming, which likely disrupted its habitat, with environmental DNA records possibly extending the range of the species around 9,800 years ago. Its closest living relative is the Sumatran rhinoceros.
The steppe bison or steppe wisent is an extinct species of bison. It was widely distributed across the mammoth steppe, ranging from Western Europe to eastern Beringia in North America during the Late Pleistocene. It is ancestral to all North American bison, including ultimately modern American bison. Three chronological subspecies, Bison priscus priscus, Bison priscus mediator, and Bison priscus gigas, have been suggested.
Crocuta is a genus of hyena containing the largest extant member of the family, the spotted hyena (Crocuta crocuta). Several fossil species are also known, with the Pleistocene Eurasian cave hyenas either being regarded as distinct species or subspecies of the spotted hyena.
The American lion, with the species name meaning "savage" or "cruel", also called the North American lion) is an extinct pantherine cat native to North America during the Late Pleistocene from around 130,000 to 12,800 years ago. Genetic evidence suggests that its closest living relative is the lion, with the American lion representing an offshoot from the lineage of the largely Eurasian cave lion, from which it is suggested to have split around 165,000 years ago. Its fossils have been found across North America, from Canada to Mexico. It was about 25% larger than the modern lion, making it one of the largest known felids to ever exist, and an important apex predator.
The mammoth steppe, also known as steppe-tundra, was once the Earth's most extensive biome. During glacial periods in the later Pleistocene it stretched east-to-west, from the Iberian Peninsula in the west of Europe, then across Eurasia and through Beringia and into the Yukon in northwest Canada; from north-to-south, the steppe reached from the Arctic southward to southern Europe, Central Asia and northern China. The mammoth steppe was cold and dry, and relatively featureless, though climate, topography, and geography varied considerably throughout. Certain areas of the biome—such as coastal areas—had wetter and milder climates than others. Some areas featured rivers which, through erosion, naturally created gorges, gulleys, or small glens. The continual glacial recession and advancement over millennia contributed more to the formation of larger valleys and different geographical features. Overall, however, the steppe is known to be flat and expansive grassland. The vegetation was dominated by palatable, high-productivity grasses, herbs and willow shrubs.
The Pantherinae is a subfamily of the Felidae; it was named and first described by Reginald Innes Pocock in 1917 as only including the Panthera species, but later also came to include the clouded leopards. The Pantherinae genetically diverged from a common ancestor between 9.32 to 4.47 million years ago and 10.67 to 3.76 million years ago.
The history of lions in Europe is part of the wider history of the lion species complex. The rediscovery and confirmation of their presence in Europe, already known by myths, historical accounts and ancient art, was made possible by the finds of fossils of Pleistocene, Holocene and Ancient lions excavated in Europe since the early 19th century. The first excavated lion fossil was found in southern Germany, and described by Georg August Goldfuss using the scientific name Felis spelaea. It probably dates to the Würm glaciation, and is 191,000 to 57,000 years old. Since then, older lion skull fragments were excavated in Germany and in other parts of Europe, including in Western Europe. Some of them were described by Wilhelm von Reichenau under Felis fossilis in 1906.
Panthera gombaszoegensis, also known as the European jaguar, is a Panthera species that lived from about 2.0 to 0.35 million years ago in Europe, as well as likely elsewhere in Eurasia. The first fossils were excavated in 1938 in Gombasek Cave, Slovakia. P. gombaszoegensis was a medium-large sized species that formed an important part of the European carnivore guild for a period of over a million years. Many authors have posited that it is the ancestor of the American jaguar, with some authors considering it the subspecies Panthera onca gombaszoegensis, though the close relationship between the two species has been questioned by some authors.
Panthera fossilis is an extinct species of cat belonging to the genus Panthera, known from remains found in Eurasia spanning the Middle Pleistocene and possibly into the Early Pleistocene.
Cave lions are large extinct carnivorous felids that are classified either as subspecies of the lion, or as distinct but closely related species, depending on the authority.
Cave hyena are extinct species or subspecies of hyena known from Eurasia, which ranged from Western Europe to eastern Asia and Siberia during the Pleistocene epoch. It is well represented in many European caves, primarily dating to the Last Glacial Period. It was an apex predator that preyed on large mammals, and was responsible for the accumulation of hundreds of large Pleistocene mammal bones in areas including horizontal caves, sinkholes, mud pits, and muddy areas along rivers.
Leopards have a long history in Europe, spanning from the Early-Middle Pleistocene transition, around 1.2-0.6 million years ago, until the end of the Late Pleistocene, around 12,000 years ago, and possibly later into the early Holocene. Remains of leopards have been found across Europe, from the Iberian Peninsula to the Caucasus.
The cave wolf is an extinct glacial mammoth steppe-adapted wolf that lived during the Middle Pleistocene to the Late Pleistocene. It inhabited Europe, where its remains have been found in many caves. Its habitat included the mammoth steppe grasslands and boreal needle forests. This large wolf was short-legged compared to its body size, yet its leg size is comparable with that of the Arctic wolf C. l. arctos. Genetic evidence suggests that Late Pleistocene European wolves shared high genetic connectivity with contemporary wolves from Siberia, with continual gene flow from Siberian wolves into European wolves over the course of the Late Pleistocene. Modern European wolves derive most of their ancestry from Siberian wolf populations that expanded into Europe during and after the Last Glacial Maximum, but retain a minor fraction of their ancestry from earlier Late Pleistocene European wolves.
Ursus ingressus is an extinct species of the family Ursidae that lived in Central Europe during the Late Pleistocene. It is named after the Gamssulzen Cave in Austria, where the holotype of this species was found.
The steppe brown bear is a disputed extinct subspecies of brown bear that lived in Eurasia during either the Pleistocene or the early Holocene epochs, but its geological age is uncertain. Fossils of the bear have been found in various caves in Slovakia, particularly those of Vazec, Vyvieranie, Lisková, Kupcovie Izbicka, and Okno. Other authors have argued that the subspecies should be rendered invalid, as its geological age is unclear and "its skull is identical to modern U. arctos."
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