Palaeoloxodon 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 1 metre (3.3 ft) 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), with its small body size a result of insular dwarfism.

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. 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.

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.

Palaeoloxodon falconeri derives from the 4-metre-tall (13 ft) 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. falconeri's ancestors most likely reached Sicily via swimming 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 2 m (6.6 ft) 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. 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.

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 96.5 cm (3 ft 2.0 in) in shoulder height and about 305 kg (672 lb) in weight, a composite adult female specimen MPUR/V n2 80 cm (2 ft 7.5 in) in shoulder height and about 168 kg (370 lb) in weight, and a composite newborn male specimen MPUR/V n3 33 cm (1 ft 1.0 in) in shoulder height and about 6.7 kg (15 lb) in weight. A later 2019 volumetric study revised the weight estimates for the adult male and adult female to about 250 kg (551 lb) and 150.5 kg (332 lb) respectively. The newborn male of the species was estimated in the same study to weigh 7.8 kg (17 lb). 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 endocranial vault indicates brain was around the size of a human's, and proportionally much larger relative to skull size than in 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. 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.

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.