Stegodon

Not to be confused with Stegadon, a fictional creature from the Warhammer game.

Stegodon ("roofed tooth" from the Ancient Greek words στέγω, stégō, 'to cover', + ὀδούς, odoús, 'tooth' because of 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 mastodons.^[1] The oldest fossils of the genus are found in Late Miocene strata in Asia, likely originating from the more archaic Stegolophodon, shortly afterwards migrating into Africa.^[2] While the genus became extinct in Africa during the Pliocene, Stegodon remained widespread in Asia until the end of the Pleistocene.^[3]

Stegodon Temporal range: Late Miocene–Late Pleistocene, 11.6–0.01 Ma PreꞒ Ꞓ O S D C P T J K Pg N
Stegodon skeleton at the Gansu Provincial Museum
Scientific classification
Kingdom:	Animalia
Phylum:	Chordata
Class:	Mammalia
Order:	Proboscidea
Family:	†Stegodontidae
Genus:	†Stegodon Falconer, 1847
Species
†S. aurorae (Matsumoto, 1918) †S. elephantoides (Clift, 1828) †S. florensis Hooijer, 1957 †S. ganesha (Faloner and Cautley, 1846) †S. kaisensis Hopwood, 1939 †S. luzonensis von Koenigswald, 1956 †S. miensis (Matsumoto, 1941) †S. mindanensis (Naumann, 1890) †S. orientalis Owen, 1870 †S. sompoensis Hooijer, 1964 †S. sondaari van den Bergh, 1999 †S. trigonocephalus (Martin, 1887) †S. zdanskyi Hopwood, 1935

Morphology

Size

 

Skeletal restoration of S. zdansky

Some species of Stegodon were amongst the largest proboscideans. S. zdanskyi is known from an old male (50-plus years old) from the Yellow River that is 3.87 m (12.7 ft) tall and would have weighed approximately 12.7 tonnes (12.5 long tons; 14.0 short tons) in life. It had a humerus 1.21 m (4.0 ft) long, a femur 1.46 m (4.8 ft) long, and a pelvis 2 m (6.6 ft) wide.^[4] Size varies across species, large stegodonts are comparable in size with modern elephants. Aside from S. zdanskyi, species like S. ganesha, S. miensis, S. orientalis, S. elephantoides and S. kaisensis are also relatively large bodied. Large stegodonts usually occur in the mainland. There also exist medium sized stegodonts present in large islands like those of Japan and Java. These stegodonts may include: S. aurorae, S. trigonocephalus, S. insignis and S. florensis florensis. Stegodonts that live in smaller islands usually result in further dwarfism.

Dwarfism

S. florensis insularis is an extinct subspecies of Stegodon endemic to the island of Flores, Indonesia, and an example of insular dwarfism. The direct ancestor of S. florensis insularis is the larger-bodied S. florensis florensis, from Early Pleistocene and early Middle Pleistocene sites on Flores.^[5] Remains of S. florensis insularis are known from the cave of Liang Bua.

 

Life-sized models of Stegodon

Similar to modern-day elephants, stegodonts were likely good swimmers,^[6][7] as their fossils are frequently encountered on Asian islands (such as Sulawesi, Flores, Timor, Sumba in Indonesia; Luzon and Mindanao in the Philippines; Taiwan; and Japan), all locations not connected by land bridges with the Asian continent even during periods of low sea level (during the cold phases of the Pleistocene). A general evolutionary trend in large mammals on islands is island dwarfing. Many among the dwarfed species of Stegodonts came from the lineage of S. ganesha, S. zdanskyi and S. elephantoides. The smallest dwarf species known is S. sumbaensis from Sumba,^[8] with an estimated body mass of 250 kg.^[9] The slightly larger S. sondaari, known from Early Pleistocene layers on the Indonesian island of Flores, had an estimated body weight of between 355 and 650 kg.^[9] Another estimate gives a shoulder height of 1.2 m (3.9 ft) and a weight of 350–400 kg (770–880 lb).^[4] Philippine pygmy stegodonts also have a small stature bigger than or around the size of S. sondaari and S. sompoensis of Celebes,^[10] with S. mindanensis having a projected weight of 400 kg.^[11] S. luzonensis and S. sompoensis have estimated masses of around 1,300 kg and 1,000 kg respectively.^[9] A medium- to large-sized stegodont, S. florensis, with a body weight of about 1,700 kg, appeared about 850,000 years ago, and then also evolved into a dwarf form, S. f. insularis, with an estimated body mass of about 570 kg.^[9][5] Another estimate gives a shoulder height of 2 m (6.6 ft) and a weight of 2 t (2.0 long tons; 2.2 short tons).^[4] The latter was contemporaneous with, and hunted by, the dwarf hominin Homo floresiensis, and disappeared about 49,600 years ago,^[12] earlier than initially thought.^[13] Dwarf stegodonts were believed to be the main prey of the still-extant Komodo dragon before modern humans introduced their modern main prey in its range, banded pig, rusa deer, and water buffalo.^[14]

Ecology

Like modern elephants, but unlike more primitive probscideans, Stegodon is thought to have chewed using a proal movement (a forward stroke from the back to the front) of the lower jaws.^[1] Based on dental microwear analysis, populations of Stegodon from the Pleistocene of China and Southeast Asia were found to be browsers, with clear niche differentiation from sympatric Elephas populations, which tended towards mixed feeding (both browsing and grazing).^[15][16]

Taxonomy

 

Fossils of S. aurorae (left) and S. orientalis (right) at the National Museum of Nature and Science, Tokyo

 

Skull of S. ganesha

 

Fossilized Stegodon jaw with molar displayed at Philippine National Museum

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.^[2] Stegodon is generally considered to be more closely related to elephants and mammoths than either gomphotheres or mastodons.^[17] Some taxonomists consider the stegodonts a subfamily of the Elephantidae. The most important difference between Stegodon and (other) Elephantidae can be observed in the molars. Stegodont molars consist of a series of low, roof-shaped ridges, whereas in elephants, each ridge has become a high-crowned plate. Furthermore, stegodont skeletons are more robust and compact than those of elephants.

In Bardia National Park in Nepal, a population of Indian elephants, possibly due to inbreeding, exhibits many Stegodon-like morphological features. These primitive features are considered recent mutations rather than atavisms.^[18][19]

Fossils of the small, specialized stegodont S. aurorae are found in the Osaka Plain, Japan, and date from around 2 million to 7 million years ago. This species possibly evolved from S. shinshuensis.^[20]

Phylogeny

 

Fossilized Stegodon jaw with molar displayed at Philippine National Museum

The following cladogram shows the placement of the genus Stegodon among other proboscideans, based on hyoid characteristics:^[17]

	Mammut americanum (American mastodon) Gomphotherium sp. Stegodon zdanskyi Loxodonta africana (African bush elephant) Elephas maximus (Asian elephant) Mammuthus columbi (Columbian mammoth)

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
• 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
• Stegodon florensis Middle – Late Pleistocene, Flores
• Stegodon luzonensis Pleistocene, Philippines
• Stegodon trigonocephalus Pleistocene, Java
• Stegodon sompoensis Pleistocene, Sulawesi
• Stegodon sumbaensis Pleistocene, Sumbawa
• Stegodon timorensis Pleistocene, Timor

Extinction

Stegodon became extinct in the Indian subcontinent, mainland Southeast Asia and China by the end of the Late Pleistocene epoch, while Asian elephants, which existed in sympatry with Stegodon in these regions, are still extant.^[21][16][22] The survival of the Asian elephant as opposed to Stegodon has been suggested to be due to its more flexible diet in comparison to Stegodon.^[16] A review of 130 papers written about 180 different sites with proboscidean remains in southern China revealed Stegodon to have been more common than Asian elephants; the papers gave many recent radiocarbon dates, the youngest being 2,150 BCE (4,100 BP).^[23] However, Turvey et al. (2013) reported that one of the faunal assemblages including supposed fossils of Holocene Stegodon (from Gulin, Sichuan Province) is actually late Pleistocene in age; other supposed fossils of Holocene stegodonts were lost and their age cannot be verified. The authors concluded that the latest confirmed occurrences of Stegodon from China are from the late Pleistocene, and that its Holocene survival cannot be substantiated.^[22]

References

1. Saegusa, Haruo (March 2020). "Stegodontidae and Anancus: Keys to understanding dental evolution in Elephantidae". Quaternary Science Reviews. 231: 106176. doi:10.1016/j.quascirev.2020.106176.
2. Ao, Hong; Zhang, Peng; Dekkers, Mark J.; Roberts, Andrew P.; An, Zhisheng; Li, Yongxiang; Lu, Fengyan; Lin, Shan; Li, Xingwen (January 2016). "New magnetochronology of Late Miocene mammal fauna, NE Tibetan Plateau, China: Mammal migration and paleoenvironments". Earth and Planetary Science Letters. 434: 220–230. doi:10.1016/j.epsl.2015.11.019.
3. O’Regan, H. J.; Bishop, L. C.; Lamb, A.; Elton, S.; Turner, A. (1 January 2005). "Large mammal turnover in Africa and the Levant between 1.0 and 0.5 Ma". Geological Society, London, Special Publications. 247 (1): 231–249. doi:10.1144/GSL.SP.2005.247.01.13. ISSN 0305-8719.
4. Larramendi, A. (2016). "Shoulder height, body mass and shape of proboscideans" (PDF). Acta Palaeontologica Polonica. 61. doi:10.4202/app.00136.2014. S2CID 2092950.
5. Van Den Bergh, G. D., Aweb, R. D., Morwood, M. J., Sutiknab, T., Jatmikob and Saptomo, E. W. 2008. The youngest stegodon remains in Southeast Asia from the Late Pleistocene archaeological site Liang Bua, Flores, Indonesia. Quaternary International 182(1): 16–48.
6. Simpson, G. (1977). "Too Many Lines; The Limits of the Oriental and Australian Zoogeographic Regions". Proceedings of the American Philosophical Society, 121(2), 107–120. Retrieved from http://www.jstor.org/stable/986523
7. Bird, Michael I.; Condie, Scott A.; O’Connor, Sue; O’Grady, Damien; Reepmeyer, Christian; Ulm, Sean; Zega, Mojca; Saltré, Frédérik; Bradshaw, Corey J. A. (2019). "Early human settlement of Sahul was not an accident". Scientific Reports. 9 (1): 8220. doi:10.1038/s41598-019-42946-9. PMC 6579762. PMID 31209234.
8. Turvey, Samuel T.; Crees, Jennifer J.; Hansford, James; Jeffree, Timothy E.; Crumpton, Nick; Kurniawan, Iwan; Setiyabudi, Erick; Guillerme, Thomas; Paranggarimu, Umbu; Dosseto, Anthony; van den Bergh, Gerrit D. (30 August 2017). "Quaternary vertebrate faunas from Sumba, Indonesia: implications for Wallacean biogeography and evolution". Proceedings of the Royal Society B: Biological Sciences. 284 (1861): 20171278. doi:10.1098/rspb.2017.1278. PMC 5577490. PMID 28855367.
9. van der Geer, Alexandra A. E.; van den Bergh, Gerrit D.; Lyras, George A.; Prasetyo, Unggul W.; Due, Rokus Awe; Setiyabudi, Erick; Drinia, Hara (2016). "The effect of area and isolation on insular dwarf proboscideans". Journal of Biogeography. 43 (8): 1656–1666. doi:10.1111/jbi.12743.
10. Hooijer, D.A. (1974). "Quaternary Mammals West and East of Wallace's Line". Netherlands Journal of Zoology. 25: 46–56. doi:10.1163/002829675x00128.
11. Ong, Perry (1998). "The Philippine Menagerie". The Philippine Archipelago. Makati city, Philippines: Asia Publishing Co. Ltd. pp. 227–255.
12. Sutikna, Thomas; Tocheri, Matthew W.; Morwood, Michael J.; Saptomo, E. Wahyu; Jatmiko; Awe, Rokus Due; Wasisto, Sri; Westaway, Kira E.; Aubert, Maxime; Li, Bo; Zhao, Jian-xin (April 2016). "Revised stratigraphy and chronology for Homo floresiensis at Liang Bua in Indonesia". Nature. 532 (7599): 366–369. doi:10.1038/nature17179. ISSN 0028-0836. PMID 27027286. S2CID 4469009.
13. Van Den Bergh, G. D.; Rokhus Due Awe; Morwood, M. J.; Sutikna, T.; Jatmiko; Wahyu Saptomo, E. (May 2008). "The youngest Stegodon remains in Southeast Asia from the Late Pleistocene archaeological site Liang Bua, Flores, Indonesia". Quaternary International. 182 (1): 16–48. Bibcode:2008QuInt.182...16V. doi:10.1016/j.quaint.2007.02.001.
14. Diamond, Jared M. (1987). "Did Komodo dragons evolve to eat pygmy elephants?". Nature. 326 (6116): 832.
15. Zhang, Hanwen; Wang, Yuan; Janis, Christine M.; Goodall, Robert H.; Purnell, Mark A. (25 July 2017). "An examination of feeding ecology in Pleistocene proboscideans from southern China (Sinomastodon, Stegodon, Elephas), by means of dental microwear texture analysis". Quaternary International. VIth International Conference on Mammoths and their Relatives, Part 3. 445: 60–70. doi:10.1016/j.quaint.2016.07.011. ISSN 1040-6182.
16. Ma, Jiao; Wang, Yuan; Jin, Changzhu; Hu, Yaowu; Bocherens, Hervé (15 May 2019). "Ecological flexibility and differential survival of Pleistocene Stegodon orientalis and Elephas maximus in mainland southeast Asia revealed by stable isotope (C, O) analysis". Quaternary Science Reviews. 212: 33–44. doi:10.1016/j.quascirev.2019.03.021. ISSN 0277-3791.
17. Shoshani, J.; Tassy, P. (2005). "Advances in proboscidean taxonomy & classification, anatomy & physiology, and ecology & behavior". Quaternary International. 126–128: 5–20. Bibcode:2005QuInt.126....5S. doi:10.1016/j.quaint.2004.04.011.
18. Ben S. Roesch. . Archived from the original on 16 July 2012.
19. Norton, Charlie (14 October 2010). "In search of the Beast of Bardia". ISSN 0307-1235. Retrieved 21 January 2018.
20. Yoshikawa, S; Kawamura, Y.; Taruno, H. "Land bridge formation and proboscidean immigration into the Japanese Islands during the quaternary". Journal of Geosciences. Osaka City University. 50: 1–6.
21. Jukar, A. M.; Lyons, S. K.; Wagner, P. J.; Uhen, M. D. (15 January 2021). "Late Quaternary extinctions in the Indian Subcontinent". Palaeogeography, Palaeoclimatology, Palaeoecology. 562: 110137. doi:10.1016/j.palaeo.2020.110137. ISSN 0031-0182.
22. Samuel T. Turvey, Haowen Tong, Anthony J. Stuart and Adrian M. Lister (2013). "Holocene survival of Late Pleistocene megafauna in China: a critical review of the evidence". Quaternary Science Reviews. 76: 156–166. Bibcode:2013QSRv...76..156T. doi:10.1016/j.quascirev.2013.06.030.{{cite journal}}: CS1 maint: multiple names: authors list (link)
23. H. Saegusa, "Comparisons of Stegodon and Elephantid Abundances in the Late Pleistocene of Southern China" 2006-05-08 at the Wayback Machine, The World of Elephants – Second International Congress, (Rome, 2001), 345–349.

 

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