Elephas falconeri

''Palaeoloxodon falconeri'' is an extinct species of dwarf elephant that lived during the Middle Pleistocene (sometime between around 500–200,000 years ago) on the Mediterranean islands of Sicily and Malta. It is amongst the smallest of all dwarf elephants, under in height as fully grown adults. A member of the genus ''Palaeoloxodon'', it derived from a population of the mainland European straight-tusked elephant (''Palaeoloxodon antiquus'').

Taxonomy

In 1859, during the digging of a watertank near the town of Zebbug in central Malta, a sediment filled cavern was excavated, leading to the discovery of an elephant molar, which the owner of the property later presented to Malta Library Museum. This prompted Thomas Abel Brimage Spratt to search through the excavated sediment as well as to continue further excavation of the cavern (now known as Zebbug Cave), yielding additional elephant molars as well as other animal remains.V.L. Herridg
Dwarf Elephants on Mediterranean Islands: A Natural Experiment in Parallel Evolution. PhD Thesis, Vol 1.
pp. 16-17, 76-77, 81, 90, 135 University College London (2010) In 1862, British paleontologist Hugh Falconer presented to the British Association at Cambridge a description of remains of dwarf elephants that had been discovered by Spratt in Zebbug cave. In 1867/68, following Falconer's death in 1865, the species ''Elephas melitensis'' was named in a posthumous publication of Falconer's notes by British paleontologist George Busk, in a paper combining Falconer's notes with Busk's own contributions. In the same publication Busk named the species ''Elephas falconeri'' for many of the smallest molars selected from the material originally ascribed by Falconer (for whom the species is named) to ''Elephas melitensis''.Palombo, M.R. (2001)
''Endemic elephants of the Mediterranean Islands: knowledge, problems and perspectives''
The World of Elephants, Proceedings of the 1st International Congress (October 16–20, 2001, Rome): 486–491.

The species ''Elephas/Palaeoloxodon melitensis'', formerly considered a distinct species or which ''P. falconeri'' was considered a synonym of (for example in Pohlig, 1893 and Fabiani 1928 and 1932), is now generally treated as a synonym of ''P. falconeri'' since a 1968 publication by Ambrosetti. Henry Fairfield Osborn in his 1942 posthumous monograph considered the species a member of the genus ''Palaeoloxodon,'' though some later 20th century authors continued to treat it as species of ''Elephas''. Some publications during the 1990s tentatively suggested ''P. falconeri'' may be a kind of dwarf mammoth (genus ''Mammuthus''). By the 2010s its placement as a member of the genus ''Palaeoloxodon'' was widely accepted. Due to the species name ''P. falconeri'' being based on Maltese material, and uncertainty about the taxonomy of Sicilian and Maltese dwarf elephants and whether or not species were shared between the two islands has led modern authors to refer to the Sicilian material (such as that from Spinagallo Cave) as ''Palaeoloxodon'' ex gr. (''ex grege'') ''P. falconeri'' to reflect this uncertainty.

Evolution and chronology

''Palaeoloxodon falconeri'' derives from the 4 metre tall straight-tusked elephant (''P. antiquus''), which arrived in Europe approximately 800,000 years ago. The oldest radiometrically dated fossils of ''Palaeoloxodon'' on Sicily date to around 500,000 years ago, with the colonisation possibly occurring as early as 690,000 years ago or earlier. ''P. falconeris ancestors most likely reached Sicily from the Italian mainland, likely via a series of islands that now form part of the southern Calabrian peninsula. Middle Pleistocene elephant remains from Luparello fissure in northwest Sicily considerably larger than "typical" ''P. falconeri'' are thought to likely represent ancestors of ''P. falconeri''. Remains at several sites appear to show the size of ''P. falconeri'' and its ancestors becoming smaller over time. The chronology of the species on Sicily compared to that of the larger endemic species of ''Palaeoloxodon'' on the island, the tall '' Palaeoloxodon cf. mnaidriensis'', is somewhat uncertain. It is generally thought that ''P. falconeri'' is the earlier species dating to the Middle Pleistocene, and that ''P''. cf. ''mnaidriensis'' descends from a subsequent separate late Middle Pleistocene colonisation of the island by ''P. antiquus,'' suggested to date to approximately 200,000 years ago. ''P. falconeri'' likely dispersed to Malta from Sicily during an episode or episodes of low sea level during glacial periods, which exposed as dry land the large submarine plateau (the Hyblean-Malta plateau) between the two islands, reducing the distance between the two islands to a relatively narrow strait. The chronology of Maltese localities is poorly constrained. The important locality of Spinagallo Cave in southeast Sicily where a large sample of ''P. falconeri'' individuals have been found is suggested to date to around 366-233,000 years ago based on optically stimulated luminescence dating and uranium–thorium dating.

Description

''Palaeoloxodon falconeri'' is considered to be a textbook example of insular dwarfism, with adult individuals around the size of modern elephant calves, drastically smaller than their mainland ancestors. In a 2015 study of specimens from Spinagallo Cave, a composite adult male specimen MPUR/V n1 was estimated to measure in shoulder height and about in weight, a composite adult female specimen MPUR/V n2 in shoulder height and about in weight, and a composite newborn male specimen MPUR/V n3 in shoulder height and about in weight. A later 2019 volumetric study revised the weight estimates for the adult male and adult female to about and respectively. The newborn male of the species was estimated in the same study to weigh . This makes ''P. falconeri'' the smallest known elephant species, along with the roughly equivalently sized but much more poorly known '' Palaeoloxodon cypriotes'' of Cyprus, and dwarf mammoth '' Mammuthus creticus'' of Crete. The Maltese remains of dwarf elephants including ''P. falconeri'' are much more fragmentary than those found in Sicily.

The morphology of the skull demonstrates neotenic traits similar to those present in juvenile elephants, including the loss of the fronto-parietal crest present in other ''Palaeoloxodon'' species. The brain was around the size of a human's, and proportionally much larger relative to skull and body size than ''P. antiquus.'' In comparison to adult ''P. antiquus'' individuals, the neck was elongated, the torso was proportionally wider and longer, and the forelimbs were shorter while the hindlimbs were longer, resulting in a concave back. The limbs were proportionally more slender than ''P. antiquus'', presumably because they needed to bear less weight. The feet were more digitigrade than modern elephants due to being proportionally narrower and higher. The morphology of the limbs and feet suggest that ''P. falconeri'' may have been more nimble than living elephants, and better able to move on steep and uneven terrain. Female members of the species were tuskless. Due to the much smaller body size resulting in increased heat loss, it is possible that the species was covered by a more dense coat of hair than present in living elephants in order to maintain a stable body temperature, though if it was present it was still likely sparse, due to elephants lacking sweat glands. The ears were also likely proportionally much smaller than living elephants for similar thermodynamic reasons. Histology analysis of their bones, teeth and tusks demonstrates that despite their small size, individuals of ''P. falconeri'' grew very slowly, reaching sexual maturity at around 15 years of age (older than living elephants), with some individuals aged around 22 still having unfused limb bone epiphyses, indicating that they were still growing. The growth rate was only slightly lower post-sexual maturity, which contrasts with African bush elephants, whose growth slows considerably after sexual maturity. At least one individual reached a lifespan of at minimum 68 years, comparable to full-sized elephants. Dental microwear suggests that ''P. falconeri'' was a mixed feeder (both browsing and grazing).

Ecology

Sicily during the time of ''P. falconeri'' exhibited a depauperate fauna, with the only other terrestrial mammal species on the island being the cat-sized giant dormouse ''Leithia'' (the largest dormouse ever) as well as the giant dormouse '' Maltamys,'' the otter '' Nesolutra,'' and the shrew ''Crocidura esuae'' which is possibly the ancestor of the living Sicilian shrew, ''C. sicula'' though this is disputed (the presence of a fox of the genus ''Vulpes'' has been suggested but is unconfirmed).''Bonfiglio, L., Marra, A. C., Masini, F., Pavia, M., & Petruso, D. (2002)
Pleistocene faunas of Sicily: a review
In W. H. Waldren, & J. A. Ensenyat (Eds.), ''World islands in prehistory: international insular investigations''. British Archaeological Reports, International Series, 1095, 428–436.'' Sicily was also inhabited by a variety of bird species, as well as frogs (''Discoglossus'', '' Bufotes'', '' Hyla''), lizards ('' Lacerta''), snakes (''Hierophis'', '' Natrix''), pond turtles, tortoises (including the large '' Solitudo'' and smaller Hermann's tortoise), and bats.''''

On Malta, ''Palaeoloxodon falconeri'' co-occurs again with ''Leithia'' and ''Maltamys'', ''Solitudo'' and ''Discoglossus'', as well as with the giant swan ''Cygnus falconeri''. At several Maltese localities, small ''P. falconeri'' elephants are found in the same strata as larger dwarf elephants, historically assigned to '' Palaeoloxodon mnaidriensis''. It is unclear whether these represent distinct contemporaneous species, or whether these are time-averaged assemblages mixing remains of animals that lived at different times.

Extinction

''Palaeoloxodon falconeri'' became extinct on Sicily as part of a faunal turnover event due to the tectonic uplift of northeast Sicily and Calabria towards the end of the Middle Pleistocene resulting in the narrowing of the Strait of Messina and the corresponding distance between the island and the Italian mainland, similar to the geography in the region today, allowing a number of large mammal species from mainland Italy to colonise the island, including carnivores like cave hyenas, cave lions, grey wolves and brown bears, and herbivores like wild boar, red deer, fallow deer, aurochs, steppe bison and the hippo ''Hippopotamus pentlandi.'' The straight-tusked elephant again recolonised the island during this episode, giving rise to '' Palaeoloxodon cf. mnaidriensis'', which though strongly dwarfed, was considerably larger than ''P. falconeri'', with its larger body size likely a reaction to these large predators and competitors. This turnover including the arrival of ''Palaeoloxodon cf. mnaidriensis'' is suggested to have occurred at earliest around 200,000 years ago, corresponding with a sea level drop at the onset of the Penultimate Glacial Period (Marine Isotope Stage 6), with ''Palaeoloxodon cf. mnaidriensis'' likely present on Sicily by 160,000 years ago, corresponding to the lowest sea levels of MIS 6 around 160-140,000 years ago.

The timing of extinction of ''P. falconeri'' on Malta is uncertain, though remains of dwarf elephants are not known from Għar Dalam cave younger than 151,200 years ago.D'Souza, L. C.
An endemic radiation of deer in the Late Pleistocene of Malta
1 Oct 2019 PhD Thesis, University of Bristol pp. 24, 30, 38, 294, 300 Although ''P. falconeri'' has historically been suggested to have been present at Għar Dalam, detailed analysis of elephant molars found in the cave suggests that ''P. falconeri'' is not present in Għar Dalam. The oldest fossiliferous stratigraphic layer of Għar Dalam (the "Bone Breccia" layer) is over 163,000 years old, which contains the remains of other, larger dwarf elephants, as well as remains of other animals not found at other Maltese sites containing ''P. falconeri'', such as hippopotamus and probable red deer or endemic offshoots.

Gallery

References

{{Taxonbar, from=Q727788

falconeri
Pleistocene proboscideans
Pleistocene species
Fossil taxa described in 1867
Pleistocene mammals of Europe
Fossils of Malta
Archaeological discoveries in Malta