Stegodon

''Stegodon'' (from the Ancient Greek στέγω (''stégō''), meaning "to cover", and ὀδούς (''odoús''), meaning "tooth", named for the distinctive ridges on the animal's molars) is an extinct genus of proboscidean, related to elephants. It was originally assigned to the family Elephantidae along with modern elephants but is now placed in the extinct family Stegodontidae. Like elephants, ''Stegodon'' had teeth with plate-like lophs that are different from those of more primitive proboscideans like gomphotheres and mammutids. Fossils of the genus are known from Africa and across much of Asia, as far southeast as Timor (with a single record in southeast Europe). The oldest fossils of the genus are found in Late Miocene strata in Asia, likely originating from the more archaic ''Stegolophodon,'' subsequently migrating into Africa. While the genus became extinct in Africa during the Pliocene.

Extinct animals of Indonesia

Morphology

The skull of ''Stegodon'' is relatively tall but short, and similar in many respects to those of living elephants. The lower jaw in comparison to early elephantimorphs and its ancestor ''Stegolophodon'' is shortened (brevirostrine), and lacks lower tusks/incisors. The molar teeth are superficially like those of elephants, consisting of parallel lamellae that form ridges but are generally relatively low crowned (brachydont), the numbers of ridges are greater in later species.van der Made, J
The Evolution of the Elephants and Their Relatives in the Context of Changing Climate and Geography
In ''Elefantentreich—Eine Fossilwelt in Europa''; Verlag Beier & Beran: Langenweißbach, Germany, 2010; pp. 340–360. ISBN 978-3-939414-48-3. Members of the genus lack permanent premolars. The tusks are proportionally large, with those of the biggest species being among the largest known tusks in proboscideans, with a particularly large tusk of ''S. ganesa'' from the Early Pleistocene of India measured to be long, with an estimated mass of approximately , substantially larger than the largest recorded modern elephant tusk. These tusks have a slight upward curvature, and project forwards and parallel to each other, with the tusks often so close together that they are almost touching, such that the trunk would probably have had to rest on top of the tusks rather than be freely hanging between them as in living elephants.

Size

The Chinese ''S. zdanskyi'' is suggested to be the largest species, and is known from an old male (50-plus years old) from the Yellow River that is tall and would have weighed approximately in life. It had a humerus long, a femur long, and a pelvis wide. The Indian ''S. ganesa'' is suggested to have a shoulder height of about , and a body mass of around . The Javanese species ''S. trigonocephalus'' is suggested to have been around tall, with a body mass of around . ''S. orientalis'' was around the size of an Asian elephant (''Elephas'' ''maximus'').

Similar to modern-day elephants, stegodonts were likely good swimmers, allowing them to disperse to remote islands in Indonesia, the Philippines and Japan. Once present on the islands, due to the process of insular dwarfism, as a result of decreased land area and the reduction of predation and competition pressure, they reduced in body size, with the degree of dwarfism varying between islands as the result of local conditions. One of the smallest species, ''Stegodon sumbaensis'' from Sumba in Indonesia, is estimated at around 8% of the size of mainland ''Stegodon'' species, with a body mass of . Sometimes the same island was colonised multiple times by ''Stegodon,'' as in Flores, where the Early Pleistocene strongly dwarfed species ''Stegodon sondaari'', which was tall at the shoulder and weighed about , was replaced by the species ''Stegodon florensis'' during the Middle Pleistocene which was initially substantially larger, but progressively reduced in size over time, with the earlier subspecies ''Stegodon florensis florensis'' from the Middle Pleistocene estimated to be around 50% the size of mainland ''Stegodon'' species with a shoulder height of around and a body mass of around 1.7 tons, while the later ''Stegodon florensis insularis'' from the Late Pleistocene is estimated to be around 17% the size of mainland ''Stegodon'' species, with a shoulder height of around , and a body mass of about .Puspaningrum, Mika; Van Den Bergh, Gerrit; Chivas, Allan; Setiabudi, Erick; Kurniawan, Iwan; Brumm, Adam; and Sutikna, Thomas,
Preliminary results of dietary and environmental reconstructions of Early to Middle Pleistocene Stegodons from the So'a Basin of Flores, Indonesia, based on enamel stable isotope records
(2014). Faculty of Science, Medicine and Health - Papers: part A. 2035.

During Pliocene-Early Pleistocene (from around 4-1 million years ago), a succession of endemic dwarf species of ''Stegodon,'' probably representing a single lineage lived in the Japanese archipelago, probably derived from the mainland Chinese ''S. zdanskyi.'' In chronological succession these species are ''Stegodon miensis'' (4-3 million years ago) ''Stegodon protoaurorae'' (3-2 million years ago) and '' Stegodon aurorae,'' (2-1 million years ago) which show a progressive size reduction through time, possibly as a result of reducing land area of the Japanese archipelago. The latest and smallest species ''S. aurorae'' is estimated to be 25% the size of its mainland ancestor with a body mass of around . ''S. aurorae'' also shows morphological straits associated with dwarfism, like shortened limbs.

Ecology

Like modern elephants, but unlike more primitive proboscideans, ''Stegodon'' is thought to have chewed using a proal movement (a forward stroke from the back to the front) of the lower jaws. This jaw movement is thought to have evolved independently in elephants and stegodontids. ''Stegodon'' populations from the Late Pliocene of the India (including ''Stegodon insignis'') are suggested to have been variable mixed feeders, while those from the earliest Pleistocene (including ''Stegodon ganesa'') of the same region are suggested to have been nearly pure grazers based on isotopic analysis. Based on dental microwear analysis, populations of ''Stegodon'' from the Pleistocene of China (''Stegodon orientalis'' and ''Stegodon huananensis'') and mainland southeast Asia (''S. orientalis'') were found to be browsers, with clear niche differentiation from sympatric ''Elephas'' populations, which tended towards mixed feeding (both browsing and grazing), though isotopic analysis of ''Stegodon cf. orientalis'' specimens from the late Middle Pleistocene of Thailand suggests that these individuals were mixed feeders that consumed a significant amount of C4 grass. Specimens of ''Stegodon trigonocephalus'' from the Early-Middle Pleistocene of Java were found to be mixed feeders to grazers, with a diet similar to that of sympatric '' Elephas hysudrindicus''. The dwarf species from Flores, ''Stegodon sondaari'' and ''Stegodon florensis'', are suggested to have been mixed feeders and grazers, respectively, based on stable carbon isotopes. Specimens of ''Stegodon kaiesensis'' from the Pliocene of East Africa were found to be browsers to mixed feeders, based on mesowear analysis.

Tracks of a group of ''Stegodon'' from the Late Pliocene of Japan suggest that like modern elephants, ''Stegodon'' lived in social herds.

On Flores, where dwarf ''Stegodon'' species were the only large herbivores, they were likely the main prey of the Komodo dragon.

Taxonomy

In the past, stegodonts were believed to be the ancestors of the true elephants and mammoths, but currently they are believed to have no modern descendants. ''Stegodon'' is likely derived from ''Stegolophodon'', an extinct genus known from the Miocene of Asia, with transitional fossils between the two genera known from the Late Miocene of Southeast Asia and Yunnan in South China. ''Stegodon'' is more closely related to elephants and mammoths than to mastodons. Like elephants, stegodontids are believed to have derived from gomphotheres.

Phylogeny

The following cladogram shows the placement of the genus ''Stegodon'' among other proboscideans, based on hyoid characteristics:

List of species

* ''Stegodon kaisensis'' Late Miocene – Pliocene, Africa
* ''Stegodon zdanskyi'' Late Miocene – Pliocene, China
* ''Stegodon huananensis'' Early Pleistocene, China
* ''Stegodon orientalis'' Middle – Late Pleistocene, China, Southeast Asia, Japan, Taiwan
* ''Stegodon namadicus/S. insignis/S. ganesa'' Pliocene – Late Pleistocene, India
* ''Stegodon miensis'' Pliocene, Japan
* ''Stegodon protoaurorae'' Late Pliocene – Early Pleistocene, Japan
* '' Stegodon aurorae'' Early Pleistocene – early Middle Pleistocene, Japan
* ''Stegodon sondaari'' Early Pleistocene, Flores, Indonesia
* ''Stegodon florensis'' Middle – Late Pleistocene, Flores, Indonesia
* ''Stegodon luzonensis'' Middle Pleistocene, Luzon, Philippines
* ''Stegodon trigonocephalus'' late Early Pleistocene – early Late Pleistocene, Java, Indonesia
* ''Stegodon sompoensis'' Late Pliocene – Early Pleistocene, Sulawesi, Indonesia
* ''Stegodon sumbaensis'' Middle – Late Pleistocene, Sumba, Indonesia
* ''Stegodon timorensis'' Middle Pleistocene, Timor, Indonesia
* ''Stegodon mindanensis'' Pleistocene Mindanao, Philippines
An indeterminate ''Stegodon'' molar of an uncertain locality and age is known from Greece, representing the only record of the genus in Europe. Indeterminate remains are also known from the Early Pleistocene and early Middle Pleistocene of Israel.

Relationship with humans

Remains at a number of sites suggest that humans (in a broad sense, including archaic humans) interacted with ''Stegodon''. At a cave deposit on Gele Mountain near Chongqing in southwest China, a mandible of ''Stegodon orientalis'' was used to make a handaxe, with dating suggesting the bone is around 170,000 years old. At the late Middle Pleistocene Panxian Dadong cave site in southern Guizhou Province, southwest China, dating to around 300-190,000 years ago, numerous remains of juvenile (0-12 years of age) and a much smaller number of adult remains of adult ''Stegodon orientalis'', representing a minimum of 12 individuals were found at the site in association with stone tools and human remains. It suggested that ''Stegodon'' remains were brought to the cave by humans though none of the elements show clear evidence of processing.Schepartz, Lynne, and Sari Miller-Antonio. 2010. �
Large Mammal Exploitation in Late Middle Pleistocene China: A Comparison of Rhinoceros & Stegodonts at Panxian Dadong
” ''Before Farming'' 4: 1–14. At the Xinlong Cave site in the Three Gorges area of Chongqing, suggested to date to around 200-130,000 years ago, two ''Stegodon'' cf. ''orientalis'' tusks have been found along with human remains. These tusks appear to have been delibrately engraved with patterns and are suggested to have been brought into the cave by humans. At the Late Pleistocene Ma’anshan site also in Guizhou, remains of ''Stegodon orientalis'' including both adults and juveniles among other animals are found in two layers, the older dating to around 53,000 years Before Present (BP), with the younger dates to around 19,295-31,155 years BP with the minimum number of individuals being 7 and 2 for the older and younger layers respectively, with the older layer containing adults and juveniles while in the younger later only juveniles are present. Bones at the site display cut marks indicating butchery, and are thought to have been accumulated at the site by people, likely by hunting or possibly scavenging in the case of the large adults found in the older layer.

At Liang Bua cave on Flores dating to around 80-50,000 years ago, remains of the dwarf ''Stegodon'' species ''Stegodon florensis'' are associated with stone tools produced by the dwarf archaic human species ''Homo floresiensis,'' with a small number of the bones bearing cut marks''.'' The ambiguous circumstantial association between bones and stone tools, and the rarity of cut marks makes it unclear to what if to any degree, hunting of ''Stegodon'' was practiced by ''Homo floresiensis.''

Evolution and extinction

The oldest fossils of ''Stegodon'' in Asia date to the Late Miocene, around 8-11 million years ago, with the oldest fossils of the genus in Africa being around 7-6 million years old. ''Stegodon'' became extinct in Africa during the late Pliocene, around 3 million years ago suggested to be the result of expansion of grassland habitats.

The Javanese species ''Stegodon trigonocephalus'' became extinct around 130-80,000 years ago during the latest Middle Pleistocene-early Late Pleistocene (Marine Isotope Stage 5) following a change to more humid conditions, which may have reduced grazing habitat. The last records of ''Stegodon florensis'' date to around 50,000 years ago, around the time of arrival of modern humans to Flores (the earliest evidence of which dates to 46,000 years ago), suggesting that effects of modern human activity were likely the cause of their extinction.

''Stegodon'' became extinct in the Indian subcontinent (''Stegodon namadicus''/''Stegodon'' sp''.),'' mainland Southeast Asia and China (''S. orientalis'') at some point during the Late Pleistocene epoch, while Asian elephants, which existed in sympatry with ''Stegodon'' in these regions, are still extant. The precise timing of extinction is uncertain for these regions, though in India records of ''Stegodon'' may date as recently as 35-30,000 years ago. The survival of the Asian elephant as opposed to ''Stegodon orientalis'' in Southeast Asia and South China has been suggested to be due to its more flexible diet in comparison to ''S. orientalis''. Although some authors have claimed a Holocene survival in China for ''S. orientalis,''H. Saegusa
"Comparisons of Stegodon and Elephantid Abundances in the Late Pleistocene of Southern China"
, The World of Elephants – Second International Congress, (Rome, 2001), 345–349. these claims cannot be substantiated due to loss of specimens and issues regarding dating.

References

{{Taxonbar, from=Q772364

Stegodontidae
Miocene proboscideans
Miocene mammals of Asia
Miocene mammals of Africa
Pliocene mammals of Africa
Pliocene mammals of Asia
Pleistocene mammals of Africa
Pleistocene mammals of Asia
Pliocene proboscideans
Pleistocene proboscideans
Miocene genus first appearances
Prehistoric placental genera
Fossil taxa described in 1847
Taxa named by Hugh Falconer
Pleistocene genus extinctions