Stephanorhinus kirchbergensis, also known as Merck's rhinoceros (or the less commonly, the forest rhinoceros) is an extinct species of rhinoceros belonging to the genus Stephanorhinus that lived from the end of the Early Pleistocene (around 800,000 years ago) until its extinction in the Late Pleistocene (surviving until at least 40,000 years ago and possibly later) in Eurasia. Its range spanned from Western Europe to East Asia. Among the last members of the genus, it co-existed alongside Stephanorhinus hemitoechus (the narrow-nosed or steppe rhinoceros) in the western part of its range.
Comparison of the head angle of Merck's rhinoceros (top) with that of Stephanorhinus hemitoechus and the woolly rhinoceros (middle and bottom, respectively)
Merck's rhinoceros was a large rhinoceros, with a body mass in the range of 1,500–3,000 kilograms (3,300–6,600lb),[1] with a 2016 study estimating an average body weight of around 1,800–1,900 kilograms (4,000–4,200lb).[2] A particularly large specimen from Poland reached an estimated height at the withers of 1.82 metres (6.0ft).[3] It is one of the largest species of Stephanorhinus, exceeding S. hundsheimensis and S. hemitoechus in size.[4] The bones of the skeleton are robust and massive. The skull of Merck's rhinoceros is elongated, with the septum nasalis ossified only towards its anterior (front) end. The mandibular symphysis is relatively long and the mandible has a horizontal high, thick branch.[5]
Dental anatomy
The enamel of the teeth is very thick, and often bright coloured and smooth, with very thin or absent coronal cement. The buccal (cheek-facing) sides of the teeth often have sub-vertical bluish lines. Tooth dimensions are highly variable in comparison to other Stephanorhinus species. The upper teeth, especially the molars, are much higher towards the buccal side than to the lingual (towards the tongue) side. The ectolophs of the first and second upper molars have shallower folds, especially the fold between the paracone and mesostyle, than those of S. hemitoechus, resulting in a less pronounced undulation. In comparison to other species of Stephanorhinus, the premolars of S. kirchbergensis are mesially (towards the front of the tooth) broad and relatively lingually short. The upper premolar ectoloph folds are shallow, and have narrow anterior valleys. The ectoloph curves strongly mesially and often distally (towards the hind portion of the tooth) towards the inside of the tooth. In both upper molars and premolars, the metalophs and the protolophs are distinctly bulbous. The lower premolars and molars are similar and hard to distinguish.[5]
Merck's rhinoceros belongs to the genus Stephanorhinus, which first appeared in Europe during the Late Pliocene, around 3.5 million years ago, and is known from fossils across Eurasia. Mitochondrial and nuclear genomes obtained from Merck's rhinoceros suggest that its closest living relative is the Sumatran rhinoceros (Dicerorhinus sumatrensis), though it shares a closer common ancestry with the extinct woolly rhinoceros (Coelodonta antiquitatis), from which it suggested to have diverged around 5.5 million years ago.[8]
Relationships among Late Pleistocene and modern rhinoceros genera, based on nuclear DNA, after Liu et al., 2021:[8]
Stephanorhinus kirchbergensis (Merck's or forest rhinoceros)
Distribution and chronology
Distribution
Approximate time averaged range of Stephanorhinus kirchbergensis (red) and Stephanorhinus hemitoechus (blue), with overlapping range in purple
Its range spans from Europe to East Asia, but appears to be absent from the Iberian Peninsula.[10][11] It was predominantly present in Europe during interglacial periods where it formed part of the Palaeoloxodon antiquus assemblage, where it occurred alongside the straight-tusked elephant (Palaeoloxodon antiquus) and the narrow-nosed rhinoceros (Stephanorhinus hemitoechus).[12] In Europe its range extended northwards to Denmark[13] and southern Britain[10] (though it appears to have been absent from Britain during the Last Interglacial).[14] Its range extended into the Arctic Circle in Eastern Siberia, with a 70–48,000 year old skull known from arctic Yakutia in the Chondon River valley[15] and a late Middle Pleistocene aged lower jaw from the Yana River valley.[16] Teeth are known from caves in Primorsky Krai, suggested to date between 50,000 and 25,000 years ago based on dates of other bones found in the deposit, which are the easternmost known records,[17] along with records from the Middle Pleistocene of western and central Japan (which were previously attributed to the species Dicerorhinus nipponicus).[18][19] Remains are known from the Caucasus such as from Azokh Cave in Azerbaijan.[20] Previous claimed records from the Levant and North Africa are now thought to erroneous, and attributable to the narrow-nosed rhinoceros or other rhinoceros species.[10] A tooth of S. cf. kirchbergensis of an unknown age is known from the Lut Desert in northeastern Iran.[21] It is fairly common throughout the Pleistocene in North China,[22] but is a rarer component of South Chinese assemblages,[23] being known from around 30 localities in the region.[24] Its range was strongly controlled by glacial cycles, with the species experiencing repeated cycles of expansion and contraction as the ice sheets advanced, this accounts for the relative rarity of its remains in comparison to the woolly rhinoceros.[10]
Chronology
The earliest definitive records of the species are from Zhoukoudian Locality 13, near Beijing in northern China at around the Early-Middle Pleistocene transition approximately 800,000 years ago.[24]Stephanorhinus yunchuchenensis from Shanxi, China, likely represents a junior synonym of S. kirchbergensis, its precise age is uncertain, but it has been suggested to date to the late Early Pleistocene.[25]S. kirchbergensis appears in Europe during the early Middle Pleistocene between 700,000 and 600,000 years ago, where early on it coexisted with another Stephanorhinus species, S.hundsheimensis.[14]
During the Last Glacial Period, the species range contracted. The timing of its extinction in Europe is uncertain, thought it postdates the end of the Last Interglacial around 115,000 years ago.[26] Radiocarbon dated remains from the Altai Mountains date to around 40,000 years ago.[27] The youngest reliable records in China are from the Rhino Cave in Hubei, which is early Late Pleistocene in age.[23] Though less definitive remains are known from near Harbin in Heilongjiang, which are thought to be 20,000 years in age.[24] Records from Migong Cave just south of the Yangtze River in the Three Gorges area in northeastern Chongqing are suggested to date to MIS 2 (29,000-14,000 years ago).[28]
Ecology
Restoration of two Merck's rhinoceros in open wooded landscape with oak trees during the Eemian interglacial in Europe
Although the species has been referred to as the "forest rhinoceros", the species showed broad environmental tolerances, inhabiting across its range various environments[21] from open habitats like grassland as well as woodlands and forest.[14] Compared to the narrow-nosed rhinoceros, S. hemitoechus, the Merck's rhinoceros did nonetheless show a preference for denser, forested habitat.[29]
Merck's rhinoceros has been interpreted as a browser or a mixed feeder, consuming both browse such as branches and leaves of trees and shrubs, as well as low-lying vegetation. Its diet appears to have varied according to local conditions, though on average its diet included more browse than S. hemitoechus, which in Europe it often co-existed alongside.[30][31][14] Analysis of plant material embedded within teeth from the Neumark-Nord locality in Germany found remains of Populus (poplar or aspen) Quercus (oak), Crataegus (hawthorn), Pyracantha, Urtica (nettles) and Nymphaea (water lilies) as well as indeterminate remains of Betulaceae, Rosaceae, and Poaceae (grass).[1] Preserved plant remains found with the teeth on the arctic Chondon skull included twigs of Salix (willow), Betula (birch) and abundant Larix (larch) alongside fragments of Ericaceae (heather); sedges were notably absent.[15] A specimen from Eemian aged deposits in Gorzów Wielkopolski in Poland had twigs of Corylus (hazel), Carpinus (hornbeam), and Viscum (mistletoe), alongside fruit scales of birch, with hazel and birch dominating amongst the pollen.[30] The pollen from a specimen found at Spinadesco in Italy was dominated (~50%) by trees, particularly Alnus (alder) and Fagus (beech), with Hippophae rhamnoides (sea buckthorn), dominating amongst the shrubs, with around 30% of the total contribution being from a variety of herbaceous plants.[32]
Human exploitation
Evidence has been found at a number of sites for the exploitation and likely hunting of Merck's rhinoceros by archaic humans.
Cut marks are known on bones of S. kirchbergensis from the Guado San Nicola site in central Italy, which dates to the late Middle Pleistocene, around 400–345,000 years ago.[33] Remains of S. kirchbergensis with cut marks have also been reported from the Medzhibozh locality in western Ukraine, dating to MIS 11, around 425–375,000 years ago.[34] At the collapsed cave of Payre in southeast France, dating to the late Middle Pleistocene, numerous remains of rhinoceroses, primarily S. kirchbergensis and to a lesser exent S. hemitoechus have been found, which are suggested to have been accumulated by Neanderthals, and display marks indicative of butchery. Mortality profiles suggest that young and old individuals were preferentially targeted. The abundance of teeth found at the site (though other skull material is largely absent) suggests that the Neanderthals may have been using them as tools.[35] At the Grays Thurrock site in southern Britain, dating to MIS 9 around 300,000 years ago, both S. kirchbergensis and S. hemitoechus are suggested to have been butchered.[36] At the Taubach travertine site in Thuringia, Germany, which dates to the Eemian (approximately 130,000-115,000 years ago) abundant remains of Merck's rhinoceros with cut marks are known. The vast majority of remains were of young subadults, alongside a much smaller number of adults. It has been suggested that the rhinoceroses were killed and butchered on site by Neanderthals.[37]
Gallery
Partial skull in Stuttgart
300,000 year old dentary fragment from the United Kingdom in the NHM, London
Remains of Merck's rhinoceros from Germany
View of the top of the snout of a S. kirchbergensis skull, showing the rugose texture of the horn attachment area
↑ Georg Friedrich Jäger: Über die fossilen Säugetiere welche in Württemberg in verschiedenen Formationen aufgefunden worden sind, nebst geognostischen Bemerkungen über diese Formationen. C. Erhard Verlag, Stuttgart, 1835–39
↑ Johann Jakob Kaup: Akten der Urwelt oder Osteologie der urweltlichen Säugethiere und Amphibien. Darmstadt, Verlag des Herausgebers, 1841
↑ Billia, E.M.E., Zervanová, J., 2015. New Stephanorhinus kirchbergensis(Mammalia, Rhinocerotidae) records in Eurasia. Addenda to a previous work. Gortania.Geologia, Paleontologia, Paletnologia36, 55–68.
↑ Pushkina, Diana (July 2007). "The Pleistocene easternmost distribution in Eurasia of the species associated with the Eemian Palaeoloxodon antiquus assemblage". Mammal Review. 37 (3): 224–245. doi:10.1111/j.1365-2907.2007.00109.x. ISSN0305-1838.
↑ Billia, E.M.E. and Zervanovȧ, J., New Stephanorhinus kirchbergensis (Jäger, 1839) (Mammalia, Rhinocerotidae) records in Eurasia. Addenda to a previous work, Geol., Paleontol., Paletnol., 2015, vol. 36, pp. 55–68.
↑ Shpansky, A. V.; Boeskorov, G. G. (July 2018). "Northernmost Record of the Merck's Rhinoceros Stephanorhinus kirchbergensis (Jäger) and Taxonomic Status of Coelodonta jacuticus Russanov (Mammalia, Rhinocerotidae)". Paleontological Journal. 52 (4): 445–462. Bibcode:2018PalJ...52..445S. doi:10.1134/S003103011804010X. ISSN0031-0301. S2CID91447285.
↑ Kosintsev, P. A.; Zykov, S. V.; Tiunov, M. P.; Shpansky, A. V.; Gasilin, V. V.; Gimranov, D. O.; Devjashin, M. M. (March 2020). "The First Find of Merck's Rhinoceros (Mammalia, Perissodactyla, Rhinocerotidae, Stephanorhinus kirchbergensis Jäger, 1839) Remains in the Russian Far East". Doklady Biological Sciences. 491 (1): 47–49. doi:10.1134/S0012496620010032. ISSN0012-4966. PMID32483707. S2CID219156923.
This page is based on this Wikipedia article Text is available under the CC BY-SA 4.0 license; additional terms may apply. Images, videos and audio are available under their respective licenses.
