Tasmanian tiger, Thylacinus cynocephalus
AI generated image.
88 years ago today, the last Tasmanian tiger died in Beaumaris Zoo, Hobart, Tasmania.
It was the last in a line of carnivorous marsupial going back at least 23-25 million years ago, in the extended period of Earth's pre-'Creation Week' history when creationists believe there was nothing out of which a magic man made of nothing made everything in 6 days, just 10,000 years ago. According to creationist mythology, the Tasmanian tiger would have had no ancestors, being magically made from dirt just like every other living species.
This makes it hard for creation to explain the evidence of all those fossils known to be far older than 10,000 years and showing evidence of the evolution of extant species from ancient ancestors as species diversified from a single common ancestor which lived hundreds of millions of years ago, but then facts were never a problem for counter-factual creationism.
What information do you have on the extinct Tasmanian tiger? The Tasmanian tiger, also known as the thylacine (Thylacinus cynocephalus), was a carnivorous marsupial native to Tasmania, mainland Australia, and New Guinea. The thylacine looked somewhat like a medium-to-large dog with a slender body, a head resembling that of a wolf or dog, and distinctive dark stripes across its back and tail, giving it the nickname "Tasmanian tiger." However, it was more closely related to kangaroos and other marsupials.How the oldest ancestors of the Tasmanian tiger were discovered by palaeontologists from the University of New South Wales, Australia, is the subject of a Taylor & Francis news release:
Key Information about the Tasmanian Tiger:
- Physical Description:
- The thylacine was about the size of a large dog, with a length of up to 1.8 to 2 meters (including the tail) and a height at the shoulder of about 60 cm.
- Its fur was short and coarse, typically tan or yellow-brown, with 13 to 20 dark stripes across its back and tail.
- It had a long, stiff tail, similar to a kangaroo's, and could open its jaws incredibly wide, up to 120 degrees.
- Habitat and Behavior:
- The thylacine was a nocturnal and solitary animal, hunting at night and resting during the day in a den or hollow log.
- It primarily fed on small to medium-sized animals, such as kangaroos, birds, and small mammals. Its diet may have also included carrion.
- Extinction:
- The thylacine was driven to extinction on the Australian mainland thousands of years ago, likely due to competition with humans and the dingo, a wild dog introduced to Australia.
- In Tasmania, the species persisted until the 20th century. The last known wild thylacine was killed in 1930, and the last known individual in captivity died in 1936 at the Hobart Zoo in Tasmania.
- Its extinction was primarily due to human activities, including hunting (encouraged by a bounty system), habitat destruction, and the introduction of diseases.
- Conservation Efforts and "Rediscovery" Claims:
- Despite being declared extinct, there have been numerous unconfirmed sightings and efforts to find surviving thylacines, but none have been scientifically verified.
- Some scientific projects have explored the possibility of "de-extinction" using preserved DNA from museum specimens, but these efforts remain largely theoretical.
- Cultural Significance:
- The thylacine holds a unique place in Tasmanian culture and Australian folklore, often seen as a symbol of the tragedy of extinction and the need for wildlife conservation.
- It appears on Tasmania's coat of arms and has been the subject of various books, documentaries, and studies.
Would you like to know more about any specific aspect of the Tasmanian tiger?
Earliest known ancestors of the extinct Tasmanian Tiger discovered – and some could even eat the bones and teeth of their prey
A marsupial which had an “extremely thick” jawbone, enabling it to consume even the bones and teeth of its prey is among a discovery of three, new ancient species of the modern Thylacines – otherwise known as the Tasmanian tiger, which went extinct 88 years ago.
These new species each roamed Australia around 23-to-25 million years ago, during the late Oligocene, making them the “undoubted oldest members of this family ever discovered”.
Today – Australia’s National Threatened Species Day, which marks the death of the last Tasmanian Tiger in Hobart’s Beaumaris Zoo on the 7th of September 1936 – scientists from the University of New South Wales (UNSW) Vertebrate Palaeontology Lab publish their findings in the Journal of Vertebrate Paleontology.
The once suggested idea that Australia was dominated by reptilian carnivores during these 25 million-year-long intervals is steadily being dismantled as the fossil record of marsupial carnivores, such as these new thylacinids, increases with each new discovery. The diversity of mammalian carnivores at Riversleigh during this period rivals that seen in any other ecosystem, including the great mammalian carnivore radiation that developed in South America.
Timothy Churchill, lead author
University of New South Wales
Sydney, New South Wales, Australia.
The three new species were each found in the fossil-rich deposits in Riversleigh World Heritage Area.
The largest of these new species, Badjcinus timfaulkneri, weighed somewhere between 7-11 kilograms, about the same size as a large Tasmanian Devil. Alike the Tasmanian Devil, timfaulkneri possessed an extremely thick jawbone enabling it to consume the bones and teeth of its prey. This species is related to the much smaller, previously discovered B. turnbulli (2.7 kg) – which until now was the only other undoubted thylacinid known from the late Oligocene.
The dentary and isolated first molar of B. timfaulkneri were recovered from Hiatus Site which is even older than Riversleigh’s White Hunter Site where B. turnbulli was previously found, making B. timfaulkneri the oldest undoubted thylacine discovered so far.
Badjcinus timfaulkneri is named after Tim Faulkner, the director and co-owner of the Australian Reptile Park and managing director of Aussie Ark. Tim has dedicated his life to the conservation of Australia’s wildlife including the largest still-living marsupial carnivore, the Tasmanian Devil.
The second new species is Nimbacinus peterbridgei. This was about the size of a Maltese Terrier (~3.7 kg). This species is represented by a near-complete dentary from White Hunter Site. Nimbacinus peterbridgei was a predator that probably focused on small mammals and other diverse prey species that lived with it in the ancient forests. Species of Nimbacinus appear to be more closely related to the Tasmanian Tiger than other thylacinids of similar age. This means Nimbacinus peterbridgei is probably the oldest direct ancestor of the Tasmanian Tiger yet known.
Nimbacinus peterbridgei was named after Australian geologist, speleologist and bibliophile Peter Bridge. He has devoted his life to helping uncover Australia’s ancient past, particularly in the caves of Western Australia.
The last species, Ngamalacinus nigelmarveni was a ~5.1kg thylacinid – approximately the size of a Red fox. It was also from White Hunter Site at Riversleigh. The blades on the lower molars of species of Ngamalacinus are elongated with deep V-shaped carnassial (‘meat-cutting’) notches, suggesting they were highly carnivorous – more so than any of the other thylacinids of similar size.
Ngamalacinus nigelmarveni is named after Nigel Marven, a renowned British television documentary presenter famous for paleontology-inspired series like Prehistoric Park and Sea Monsters.
The presence of three distinct lineages of specialised thylacinids during the late Oligocene highlights how quickly they diversified after first appearing in the fossil record. These thylacinids exhibits very different dental adaptations, suggesting there were several unique carnivorous niches available during this period. All but one of these lineages, the one that led to the modern Thylacine, became extinct around 8 million years ago.
That lineage of these creatures that survived for more than 25 million years ended with the death of Benjamin, the last Tasmanian Tiger in Hobart’s Beaumaris Zoo on the 7th of September 1936.
Professor Michael Archer, co-author
University of New South Wales
Sydney, New South Wales, Australia.
ABSTRACTOf course, it would be stupid to assume the Bronze Age pastoralists who wrote the Bible knew anything about Australia, or even a southern hemisphere. Since they believe Earth was a small flat place with a dome over it, they wouldn't even have considered hemispheres, northern of southern. Their view of the world was so narrow and restricted they thought all they had to explain was the small area within a day or two's walk of the Canaanite Hills, so nothing outside that small area was included; not an animals, mountain, continent or people; nothing.
New thylacinid species of Badjcinus, Nimbacinus, and Ngamalacinus are described from upper Oligocene deposits of the Riversleigh World Heritage Area, northwestern Queensland. Badjcinus timfaulkneri, Nimbacinus peterbridgei, and Ngamalacinus nigelmarveni are among the oldest thylacinids yet known and indicate an earlier diversification of the family than previously understood. Maximum parsimony analysis supports a sister group relationship between Ng. nigelmarveni and Ng. timmulvaneyi, but the relationships of the two other new taxa are unresolved. Bayesian dated total evidence analysis using morphological and molecular data supports the generic assignment of B. timfaulkneri and Ng. nigelmarveni but not that of Ni. peterbridgei. Both phylogenies herein support a taxonomic reassignment of Thylacinus macknessi to the genus Wabulacinus, a conclusion also supported by the results of previous studies. Body mass estimates based on molar size regressions indicate body sizes ranging from 3.7 kg to 11.4 kg for the new thylacinid species. Badjcinus timfaulkneri exhibits an extremely deep jaw compared with other thylacinids, with mandibular bending strength analysis suggesting that it was a highly durophagous carnivore much like the modern dasyurid Sarcophilus harrisii. This analysis also suggests Ni. peterbridgei had a dentary more similar in shape to that of plesiomorphic thylacinid faunivores such as Ni. dicksoni and T. cynocephalus suggesting that it had a relatively more generalist faunivorous diet. The molars of Ng. nigelmarveni suggest they were better suited for longitudinal slicing than the molars of B. timfaulkneri and Ni. peterbridgei, indicating a more hypercarnivorous diet compared with that of those species.
INTRODUCTION
There are 12 extinct species in the dasyuromorphian family Thylacinidae, 10 of which are from the Oligo-Miocene (26–5.3 Ma) (Rovinsky et al., 2019). Unlike during the Plio-Pleistocene (5.3–0.12 Ma), which is dominated by large hypercarnivorous species of Thylacinus (15–55 kg), the Oligo-Miocene radiation exhibits considerably higher generic diversity, with seven monospecific clades known from the Riversleigh World Heritage Area in northwestern Queensland, all of which were between 3–10 kg in body mass. This restriction in size suggests thylacinids occupied most of the small- to medium-sized faunivorous niches at Riversleigh (1–10 kg). Contemporary peramelemorphians (∼50 g–1.5 kg) (Gurovich et al., 2014; Travouillon et al., 2013; Travouillon et al., 2010, 2014.1) and thylacoleonids (∼10–50 kg) (Gillespie, 2023; Gillespie et al., 2016, 2019.1a, 2019.2b) occupied relatively smaller and larger carnivore niches.
The oldest undoubted thylacinid, Badjcinus turnbulli Muirhead & Wroe, 1998, is known only from White Hunter Site in the Riversleigh World Heritage Area. This and other late Oligocene sites at Riversleigh have not yet been radiometrically dated. White Hunter Site is interpreted to be late Oligocene in age because of the presence of the ilariid Kuterintja ngama, otherwise only known from the Ngama Local Fauna from the Etadunna Formation, which is magnetostratigraphically dated to 24.8–25 Ma (Myers & Archer, 1997; Woodburne et al., 1994). Riversleigh’s Faunal Zone A (FZA) deposits contain taxa that support a late Oligocene age (Arena et al., 2016.1; Travouillon et al., 2006). The relatively plesiomorphic dentition of B. turnbulli has led to difficulty in taxonomic assignment, with phylogenetic analyses placing it either as a basally branching member of Thylacinidae (Kealy & Beck, 2017; Muirhead & Wroe, 1998; Murray & Megirian, 2006.1a; Wroe & Musser, 2001), as a stem dasyurid (Wroe et al., 2000), or as a sister group to Dasyuromorphia as a whole (Kealy & Beck, 2017).
Only two other thylacinid fossils are known from upper Oligocene deposits. Originally assigned to Nimbacinus dicksoni but later reassigned to Thylacinidae incertae sedis, an isolated m2 (QM F16809) from D-Site at Riversleigh is the only other thylacinid known from Riversleigh’s upper Oligocene deposits (Muirhead & Archer, 1989; Murray & Megirian, 2000.1; Wroe & Musser, 2001). An isolated, broken M2 (NTM P2815–10) of a thylacinid is also known from the Pwerte Marnte Marnte Local Fauna (LF) in the Northern Territory, a deposit assumed to be upper Oligocene on the basis of biocorrelation (Murray & Megirian, 2006.2b; Woodburne et al., 1994). Although this upper molar, which is similar in size to the putative thylacinid Mutpuracinus archibaldi, was suggested by Murray and Megirian (2006.2b) to be the oldest thylacinid in the fossil record, there are doubts about its identification as a thylacinid (see Discussion).
Nimbacinus dicksoni Muirhead & Archer, 1989, is the best preserved and researched Miocene thylacinid (Attard et al., 2014.2; Murray & Megirian, 2000.1; Wroe & Musser, 2001). Multiple specimens including a near complete skull and skeleton are known from Middle Miocene deposits at Riversleigh and from the Bullock Creek LF in the Northern Territory. The dentition of Ni. dicksoni is relatively more plesiomorphic than that of other thylacinids (except possibly Muribacinus gadiyuli) in retaining slightly reduced metaconids on m2–4 and unreduced stylar cusps on M1–3. Previous morphofunctional analyses of the skull of Ni. dicksoni suggest it was a voracious predator capable of hunting prey larger than itself, with biting capabilities most similar to extant species of Dasyurus, rather than to the larger Thylacinus cynocephalus (Attard et al., 2014.2).
In addition to Nimbacinus dicksoni, four monotypic thylacinid genera are known from upper and lower dentitions recovered from Early and Middle Miocene Riversleigh deposits. These include the medium-sized (∼5–7 kg) Wabulacinus ridei and Ngamalacinus timmulvaneyi Muirhead, 1997.1, as well as the diminutive (∼1–2 kg) Muribacinus gadiyuli Wroe, 1996, and the large (∼18 kg) Maximucinus muirheadae Wroe, 2001.1a (Myers, 2001.2). The dentition of Ng. timmulvaneyi, W. ridei, and Ma. muirheadae have been considered to be relatively plesiomorphic in comparison with species of Thylacinus, but more derived than Ni. dicksoni (Muirhead, 1997.1). The diminutive Mur. gadiyuli is dentally the most plesiomorphic thylacinid known (Wroe, 1996).
Thylacinus macknessi Muirhead, 1992, from Riversleigh’s Early Miocene Neville’s Garden Site, is tentatively regarded as the earliest known member of the genus Thylacinus (Muirhead & Gillespie, 1995). This taxon possesses unique dental adaptations associated with a shift within the Thylacinus lineage towards hypercarnivory, including near complete loss of metaconids on m2–4, loss of entoconids, reduction of the lingual portion of the talonid margin in m2–4 and a lingual shift of the hypoconid so that the cristid obliqua forms a continuous longitudinal blade with the paracristid.
The powerful thylacine, T. potens Woodburne, 1967, from the Alcoota Local Fauna in the Northern Territory, has been interpreted on the basis of biocorrelation to be Late Miocene between 8.5 and 5.5 Ma (Megirian et al., 1996.1, 2010.1). It is the largest and most hypercarnivorous thylacinid known. It has been estimated to be between 30–56 kg in adult body mass (Myers, 2001.2; Wroe, 2001.1a), with some estimates exceeding 120 kg (Yates, 2014.3). Two additional species of Thylacinus with dental adaptations for increased carnivory, T. yorkellus and T. megiriani, are known from Upper Miocene to Lower Pliocene deposits (Murray, 1997.2; Yates, 2015).
Tyarrpecinus rothi Murray & Megirian, 2000.1, is a small thylacinid from the Late Miocene Alcoota Local Fauna of the Northern Territory. It is known from a broken maxilla that retains P2 and an isolated M2. The phylogenetic relationships and paleobiology of this taxon cannot be confidently determined until more complete craniodental material is found.
The quoll-sized Mutpuracinus archibaldi Murray & Megirian, 2000.1, known from a near complete skull with an incomplete upper and lower dentition from the Middle Miocene Bullock Creek LF in the Northern Territory (Murray & Megirian, 2006.1a), was initially considered to be an early thylacinid because of craniodental and basicranial similarities to plesiomorphic thylacinids such as Ni. dicksoni. However, more recent phylogenetic analyses suggest it should be regarded as Dasyuromorphia incertae sedis because of its lack of craniodental synapomorphies uniting it with undoubted thylacinids (Churchill et al., 2023.1; Kealy & Beck, 2017; Rovinsky et al., 2019).
Two further medium-sized (1–10 kg) incertae sedis dasyuromorphians are known from Miocene deposits; Whollydooleya tomnpatrichorum Archer, Christmas et al., 2016.2, from Miocene deposits in New Riversleigh (an area approximately 10 km southwest of the Riversleigh World Heritage Area) and Apoktesis cuspis Campbell, 1976, from upper Oligocene deposits at Lake Ngapakaldi in the Tirari Desert of South Australia. Either may be related to thylacinids or dasyurids (Archer, Christmas et al., 2016.2; Campbell, 1976). However, the lack of adequate fossil material to critically assess the relationships of these two enigmatic taxa precludes a more precise assignment beyond Dasyuromorphia incertae sedis. Whollydooleya tomnpatrichorum is only known from a single lower molar while the location of the skull and dentaries attributed to A. cuspis is currently unknown.
In this study, we describe three new species of thylacinid from Riversleigh’s oldest deposits: the upper Oligocene Hiatus and White Hunter Sites. The fossil specimens herein are all dentaries retaining near complete or partial lower dentitions.
So, the idea that they would have believed the Tasmanian tiger was magically created without ancestors 10,000 years ago or less is utterly preposterous and could only be believed by someone at least as blind to the evidence as were the authors of Genesis.
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