The first documented Sumatran rhinoceros was shot outside
Fort Marlborough, near the west coast of Sumatra, in 1793. Drawings of the animal, and a written description, were sent to the
naturalist Joseph Banks, then president of the
Royal Society of London, who published a paper on the specimen that year. In 1814, the species was given a scientific name by
Johann Fischer von Waldheim. The specific epithet
sumatrensis signifies "of Sumatra", the Indonesian island where the rhinos were first discovered.
Carl Linnaeus originally classified all rhinos in the genus,
Rhinoceros; therefore, the species was originally identified as
Rhinoceros sumatrensis or
sumatranus.
Joshua Brookes considered the Sumatran rhinoceros with its two horns a distinct genus from the one-horned
Rhinoceros, and gave it the name
Didermocerus in 1828.
Constantin Wilhelm Lambert Gloger proposed the name
Dicerorhinus in 1841. In 1868,
John Edward Gray proposed the name
Ceratorhinus. Normally, the oldest name would be used, but a 1977 ruling by the
International Commission on Zoological Nomenclature established the proper genus name as
Dicerorhinus.
Dicerorhinus comes from the
Greek terms '
(, meaning "two"), ' (, meaning "horn"), and '''' (, meaning "
nose"). The three
subspecies are:
D. s. sumatrensis, known as the
western Sumatran rhinoceros, which has only 75 to 85 rhinos remaining, mostly in the national parks of
Bukit Barisan Selatan and
Kerinci Seblat,
Gunung Leuser in Sumatra, but also in
Way Kambas National Park in small numbers. Three bulls and five cows currently live in captivity at the
Sumatran Rhino Sanctuary at Way Kambas, the youngest bull having been bred and born there in 2012. Another calf, a female, was born at the sanctuary in May 2016. The sanctuary's two bulls were born at the
Cincinnati Zoo and Botanical Garden. A third calf female was born in March 2022.
D. s. harrissoni, known as the
Bornean rhinoceros or
eastern Sumatran rhinoceros, which was once common throughout Borneo; now only about 15 individuals are estimated to survive. Reports of animals surviving in
Sarawak are unconfirmed. The Bornean subspecies is markedly smaller in body size than the other two subspecies.
D. s. lasiotis, known as the
northern Sumatran rhinoceros or
Chittagong rhinoceros, which once roamed India and Bangladesh, has been declared
extinct in these countries. Unconfirmed reports suggest a small population may still survive in Myanmar, but the political situation in that country has prevented verification. The extant family, the Rhinocerotidae, first appeared in the Late Eocene in
Eurasia, and the ancestors of the extant rhino species dispersed from Asia beginning in the
Miocene. Although the relationships of modern rhinoceros species to each other were long controversial, modern genetic evidence has placed the Sumatran rhinoceros as more closely related to the Asian one-horned rhinoceroses (the
Indian rhinoceros and
Javan rhinoceros) belonging to the genus
Rhinoceros than to living African rhinoceros species, with the split between
Rhinoceros and
Dicerorhinus estimated to have occurred around 14.8
million years ago, shortly after the split between the ancestors of
Dicerorhinus and
Rhinoceros and African rhinoceroses, which is placed around 15.6
million years ago.
Stephanorhinus species are well known in Europe from the Late Pliocene through the Pleistocene, and China from the Pleistocene, with two species,
Stephanorhinus kirchbergensis and the
Stephanorhinus hemitoechus surviving into the
last glacial period, until at least 40,000 years ago and possibly later.
today only two fossil species are confidently placed in the genus. These include Dicerorhinus fusuiensis
from the Early Pleistocene of South China, and Dicerorhinus gwebinensis'' from the
Pliocene-Early Pleistocene of Myanmar. Pairwise sequential
Markovian coalescent (PSMC) analysis of a complete nuclear genome of a Sumatran specimen suggested strong fluctuations in population size, with a general trend of decline over the course of the Middle to Late Pleistocene with an estimated peak effective population size of 57,800 individuals 950,000 years ago, declining to around 500–1,300 individuals at the start of the Holocene, with a slight rebound during the
Eemian Interglacial. This was likely due to climate change causing limiting suitable habitat for the Rhinoceros, causing severe population fluctuations as well as
population fragmentation due to the flooding of
Sundaland. Human induced habitat change and hunting may have played a role in the Late Pleistocene. The study was later criticised for not including DNA from extinct mainland populations, which would have provided a holistic account. A Bayesian skyline plot of complete Mitochondrial genomes from multiple individuals from across the range of the species suggested that the population had been relatively stable with an effective population size of 40,000 individuals over the last 400,000 years, with a sharp decline starting around 25,000 years ago.
Cladogram showing the relationships of recent and Late Pleistocene rhinoceros species (minus
Stephanorhinus hemitoechus) based on whole nuclear genomes, after Liu et al, 2021: |style=font-size:100%;line-height:80%}} == Description ==