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Saber-toothed predator

Group of extinct animals

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It is a corrected version of File:Saber tooth.jpg File based on: File:Inostrancevia_alexandri.JPG File:Hoplophoneus_primevus_IMG_4443.jpg File:Barbourofelis_loveorum.jpg File:SmilodonSkeleton.jpg File
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Through Predation, Holocene and Tiger

Among the earliest animals that can be described as "sabertooths" were Middle-Late Permian (~274-252 million years ago) non-mammalian therapsids including the gorgonopsians as well as some basal therocephalians (lycosuchids and scylacosaurids).

Saber-toothed mammals have been found worldwide from the Eocene epoch to the early Holocene epoch (52.4 million years ago – 8,200 years ago). One of the best-known genera is the "saber-toothed cat" Smilodon, the species of which, especially S. fatalis, are popularly referred to as "saber-toothed tigers", although they are not closely related to tigers (Panthera), and are instead members of the extinct cat subfamily Machairodontinae (the true saber-toothed cats), most members of which had saber-teeth of varying lengths.

Despite some similarities, not all mammalian saber-tooths were closely related to saber-toothed cats or felids in-general. For example, many members are classified into different family of Feliformia, the Nimravidae; or from a separate order such as Machaeroides and Apataelurus, which are members of the order Oxyaenodonta, and one extinct lineage of metatherian mammals (related to marsupials), represented by the thylacosmilids of the order Sparassodonta. In this regard, these saber-toothed mammals can be viewed as examples of convergent evolution. This convergence is remarkable due not only to the development of elongated canines, but also a suite of other characteristics, such as a wide gape and bulky forelimbs, which is so consistent that it has been termed the "saber-tooth suite."

Among the feliform sabertooth lineages, the family Nimravidae was the oldest, with the oldest fossils dated to 42 Ma of the Eocene. Some sabertooth predators have been known to have lived in the same habitats as seen with basal therocephalians and gorgonopsians in Middle-Late Permian, as well as machairodonts and nimravids (specifically Barbourofelinae) in the Late Miocene.

Evolution

The different groups of saber-toothed predators evolved their saber-toothed characteristics entirely independently. They are most known for having maxillary canines which extended down from the mouth when the mouth was closed.

The first saber-tooths to appear were non-mammalian therapsids, the gorgonopsians; they were one of the first groups of animals within Synapsida to experience the specialization of saber teeth, and many had long canines. The oldest definitive worldwide gorgonopsian fossil was found in Port des Canonge Formation of Mallorca in the western Mediterranean dating to earliest Wordian of the Middle Permian, although the stratigraphic position of the gorgonopsian, as well as surrounding fossil track record may suggest it is significantly older, potentially Roadian stage of the Middle Permian or even of the Kungurian or Artinskian stages of the Early Permian.

The second and third instances of sabertooth predators were presented by basal therocephalians (scylacosaurids and lycosuchids). The oldest known scylacosaurid, Eutheriodon, was found in the Eodicynodon Assemblage Zone, which dates to the Wordian stage. While earliest lycosuchid fossils were found in the Tapinocephalus Assemblage Zone of the Capitanian stage of the Middle Permian, phylogeny suggests lycosuchids were the most basal therocephalians.

Gorgonopsians were subordinate to the dinocephalians and basal therocephalians, with the exceptions such as Phorcys and Jirahgorgon, who were probably the top predators of their locality. However, all dinocephalians and most basal therocephalians would later go extinct during the primary phase of the Capitanian mass extinction event, which may have been caused by volcanism that originated from the Emeishan Traps. While some basal therocephalians, such as Lycosuchus and Alopecognathus, survived the primary phase, they would later go extinct during the secondary wave of extinction. The extinction of dinocephalians and basal therocephalians, gorgonopsians occupied niches left vacant by increasing in size and becoming top predators. Gorgonopsians were able to replace the basal therocephalians as they were less restricted by prey sizes due to their more powerful jaws.

During Wuchiapingian-Changhsingian stages of the Late Permian, many gorgonopsians began to go extinct in Africa and Eastern Europe. The cause of the gorgonopsians extinction in Eastern Europe was the inability to adapt to the changing temperature and humidity and were replaced by archosauriforms and large therocephalians. In Africa, most of the large-bodied rubidgeines died out early in the Daptocephalus Assemblage Zone. Rubidgea, the last rubidgeine, went extinct during a turnover event that separates the lower and upper subzones, being replaced by Inostrancevia. The last gorgonopsians, Inostrancevia africana and Cyonosaurus, went extinct during the Permian–Triassic extinction event, which was likely due to volcanic activities that originated from Siberian Traps. The resulting eruption caused a significant climatic disruption unfavorable to their survival, leading to their extinction. Their ecological niches gave way to modern terrestrial ecosystems including sauropsids, mostly archosaurs, and among the few therapsids surviving the event, mammals. The extinction of the gorgonopsians marked the beginning of a sabertooth hiatus that lasted for 200 million years.

The fourth instance of saber-teeth is from machaeroidines of the extinct order Oxyaenodonta. The earliest known machaeroidine was Machaeroides simpsoni, which first appeared in the Early Eocene. The last macheroidines died out in the middle Eocene, which was linked to the significant faunal overturn during the transition period between the middle and late Eocene. Some experts hypothesized that their extinction was the result of competition with nimravids, other experts found no evidence of competitive displacement, as the excellent North American fossil record indicates oxyaenids were declining before the appearance of the replacement taxa such as nimravids. In addition, the youngest records of machaeroidines predate the oldest records of nimravids in North America.

Instead, their extinction was likely due to the changing climate. During the last 10 million years of the Eocene (43 to 33 Ma), the planet transitioned from a warm moist tropical world to a cooler, seasonally arid one. Because of their low mobility, as well as preference for closed habitats, oxyaenids couldn't adapt to the more open, temperate forests.

The fifth saber-tooth appearance is the basal feliform (carnivoran) family Nimravidae, which also includes the barbourofelines. The oldest known nimravid was found in the Lushi and Dongjun formations of China, which dated to the middle Eocene. The next oldest nimravid was Maofelis middle of the Eocene epoch, about 41.03 Ma. The earliest record of nimravids in North America was represented by Pangurban, which first appeared around 40 Ma. The diversification of the early nimravids was likely the result of the decline and extinction of oxyaenids, which opened the niche of felid-like carnivores. Nimravids made their first appearance in Europe during the early Oligocene following the Grand Coupre. Nimravids also saw their greatest diversity during the early Oligocene with at least 13 contemporary species.

The family then saw a decline in diversity in both Europe and North America, both corresponding with the increase in aridity, and in the case of North American nimravids, competition with amphicyonids. The extinction of North American nimravids started the infamous cat gap, a 7 million year period when no cat-like predators were present in North America. Barbourofelines probably evolved from Nimravinae dispersing into Africa during the early Miocene. The presence of large hyaenodonts prevented them from reaching a large size but were able to carve a niche due to their dental morphology. Eventually, they dispersed from Africa into Eurasia around 18 Ma and later North America around 12 Ma.

The arrival of barbourofelines in North America was thought to have placed a role in the decline and extinction of hesperocyonines. Over course of the Late Miocene, barbourofelines declined in diversity, going extinct in Europe and East Asia around 9.1 and 8.5 Ma respectively. Their extinction in Europe was correlated with the Vallesian-Turolian turnover event, also known as the Vallesian Crisis, which saw high extinction rates along with high levels of appearances of mammalian fauna. The Vallesian Crisis saw an increase of precipitation of seasonality, which gave way for drier, more open environments. Albanosmilus jourdani, the last European nimravid, went extinct due to the inability to adapt to the open environments. The last nimravids, represented by Albanosmilus whitfordi and Barbourofelis fricki, went extinct around 7 Ma. Some experts hypothesized the cause of their extinction was the result of competition with machairodonts as they were highly successful despite the expansion of grasslands. Other experts suggested it was more likely they went extinct due to the expansion of grasslands and the decline of favorable prey such as antilocaprids, camelids, dromomerycids, and equids.

The sixth appearance of saberteeth was Thylacosmilidae. They were part of an extinct order of metatherian mammals known as sparassodonts. The earliest known thylacosmilid fossil was dated to around 20.2 Ma, although a suspected origin within the Eocene-Oligocene boundary has been hypothesized for the family. One of the last thylacosmilids, Thylacosmilus atrox, went extinct during the late Pliocene, around 3 Ma. Originally, it was hypothesized that Thylacosmilus was outcompeted by carnivorans such as Smilodon. However, more recent evidence found no evidence of temporal or niche overlap between the two predators, instead extinction of Thylacosmilus and other sparassodonts was the result of the environmental changes. The youngest known thylacosmilid was Pampaluctor calibar, which persisted into the Early Pleistocene and coexisted with carnivorans such as Chapalmalania, as well as canids and mustelids.

The seventh and last saber-toothed group to evolve were the machairodonts themselves. Mitochondrial DNA found that machairodonts split off from ancestors of living cats around 20 Ma, with Homotherium and Smilodon diverging from one another around 18 Ma. Machairodonts probably evolved from the basal felid Pseudaelurus quadridentatus showed a trend towards elongated upper canines, and is believed to be at the base of the machairodontine evolution. The earliest known machairodont was Miomachairodus from the late Middle Miocene. The earliest known homothere, Machairodus, first appeared in the fossil record around 12 Ma in Africa, before appearing in Europe around 10.4 Ma. The genus would later evolve into Amphimachairodus, which evolved around 9.8 Ma in East Asia. It would later make an appearance in Europe during the early Turolian replacing Machairodus. It would also disperse into North America during the Hemphillian stage, with the oldest fossils being found in Withlacoochee River 4A of Florida. Amphimachairodus was initially rarer than Nimravides, another homothere part of distinct linage, however Amphimachairodus would later replace Nimravides as grasslands began to expand in North America. The genus is also noted to have a pan-African distribution, and may have been the ancestor of Homotherium. The earliest Homotherium fossils were found in Africa roughly 4.35 Ma, with the earliest Eurasian fossils dating to 4.2 Ma. The genus would make its first appearance in North America during the Late Pliocene between 3.6 and 2.6 Ma. A homothere, which has been attributed to Xenosmilus or Homotherium, were found in South America dating from the Early to Middle Pleistocene, roughly 1.0-0.5 Ma.

Smilodontin first appeared in the Late Miocene with Promegantereon being the oldest known genus of the tribe, it would later be replaced by Paramachaerodus during the Turolian. Megantereon was another member of the tribe, with the oldest possible fossils associated to the genus being found in the Late Miocene Africa around 7 Ma. The oldest confirmed fossils of Megantereon were found in Kenya, dating to the Late Pliocene roughly 3.5-3.0 Ma, with possible older records dating to the Early Pliocene. In Eurasia, the oldest confirmed fossils were found in the Les Etouaries (France), which has been dated to 2.78 Ma. Smilodon first appeared in the fossil record during the Blancan stage of the Pleistocene in North America, possibly evolving from Megantereon. Smilodon first appears in South America during the Ensenadan stage of the Early Pleistocene.

Machairodonts began to decline during Late Miocene, with the decline of North American machairodonts coinciding with the decline of horses. This decline would persist into the Pleistocene, the cause of their decline in the Plio-Plestocene has been debated by experts. The extinction of African machairodonts has been hypothesized to be the result of competition with hominins. This has been contested by some experts, which argued that the expansion of grasslands and loss of forest covers were more detrimental to the large carnivorans as well the decline of megaherbivores. Additionally, evidence for anthropogenic extinctions by pre-erectus hominins to have been inconclusive, as it would suggest australopiths and early Homo were stealing prey from large carnivorans long before visible archaeological or anatomical evidence of carnivory among hominins. However, this contradicts zooarcheological evidence that suggests by 2.6 Ma, homininins were targeting medium sized prey, which has a larger impact on larger carnivores compared to smaller carnivores. Due to their specialization on consuming flesh, megapredators were more vulnerable to ancient anthropogenic extinctions. Additionally, there's little evidence of megapredators relying on megaherbivores.

In Europe, the extinction of Megantereon coincided with the expansion of grasslands, while Homotherium went extinct because of competition with early humans and Panthera fossilis. Homotherium and Smilodon were the last known members of the subfamily by the Late Pleistocene. The youngest Homotherium fossil was recovered in Alberta, Canada, and was dated to 12,715–12,655 years before the present. On the other hand, the youngest Smilodon fatalis fossil was recovered in the La Brea and was dated to 13,000 years ago. The extinction of Homotherium and Smilodon fatalis was contemporary with the wave of extinctions of most large animals across the Americas. The last known sabertooth predator was Smilodon populator, which was able to persist into the early Holocene, with the youngest fossils from the Jirau Paleontological Site being dated to 8,189–9,079 years before the present, likely going extinct because of the combination of climatic changes and human activity.

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