Metaxytherium

The first remains of Metaxytherium were described in 1822 by Anselme-Gaëtan Demarest as a species of Hippo, H. medius before the genus name Metaxytherium was coined in 1840 by De Christol. Although the type species was initially designated to be M. cuvieri, later publications argued that the two species are synonymous and M. medium thus holds precedence. The grammatical changes of the species name were made to match the rules of the International Code of Zoological Nomenclature (ICZN). M. serresii was introduced by Gervais in 1847 to encompass the Metaxytherium finds made in Montpellier, France from the Early Pliocene. Although he later described and figured multiple specimens, no type specimen was ever introduced. M. floridanum was named in 1922 by Oliver P. Hay based on a piece of a right maxilla discovered 11 years prior near Mulberry, Florida. The genus Thalattosiren, described by Sickenberg in 1928, was erected from remains previously named M. pettersi, however, further research concluded that it should not only be synonymous with Metaxytherium on a genus level, but is also indistinguishable from M. medium as a species. M. arctodites was named in 1994 by Aranda-Manteca, Domning and Barnes based on three specimens found in California and Baja California, constituting the first valid record of this genus from the north-eastern Pacific. There are several genera that are now synonymous with Metaxytherium, including Thalattosiren, Halianassa, Felsinoitherium, Cheirotherium and Hesperosiren. Several species previously considered distinct have likewise been synonymized with already established Metaxytherium species. ==Species==

• M. albifontanum :Described in 2014, this species inhabited what is now Florida and South Carolina during the late Oligocene. The species name "albifontanum" is a composite of the Latin "albus" (=white) and "fontanus" (=of a spring), a name chosen due to the holotype being discovered near White Springs, Florida. More specifically, M. albifontanum was discovered in the Porters Landing Member of the Parachucla Formation and the Chandler Bridge Formation of South Carolina (25.7-23.6 Ma). It is the stratigraphically oldest species of Metaxytherium and relatively small, with a body size of 2 to 3 meters. • M. crataegense :A West-Atlantic species found in the early to middle Miocene Montera Formation of Peru as well as the Hawthorne and Calvert formations of the United States, extending its range from western South America to the north-east of the United States. The two species M. calvertense and M. riveroi from Cuba have both been sunk into this species as well. belonging to the Lower Bone Valley Formation. M. floridanum remains specifically date to the Late Barstovian to Early Hemphillian age (14-7 Ma). It reached a length of approximately 3 meters. • M. krahuletzi :M. krahuletzi is the oldest species of Metaxytherium known from Europe, The Metaxytherium bonebeds of Eggenburg Bay have been suggested to represent mass death sites, possibly the result of reduced food supply following heavy storm events known to have occurred in this part of the Paratethys. The species was named in honor of Austrian geologist Johann Krahuletz. • M. medium :The type species, M. medium is known from the Middle Miocene (Langhian) Greece and presumably Northern Africa. The most recent records of M. medium stem from late Miocene (Tortonian) Tuscany (10.5 to 8.14 Ma). • M. serresii :A species originally described to include Pliocene (Early Zanclean) specimen from Montpellier, France, later discoveries extended its range to late Miocene (latest Tortonian) Italy as well as Sahabi, Libya. M. serresii is notably smaller than any of the European species before or after it across its range, while the size of the tusks had relatively increased. It was named by Paul Gervais after Marcel de Serres. • M. subapenninum :M. subapenninum, the last species of Metaxytherium in the fossil record, lived in the early and late Pliocene of Italy and Spain. It is the only species of sirenians that lived in the northwestern coasts of the Mediterranean Sea in the Pliocene and disappeared from the Mediterranean around 3 million years ago because of the progressive climate cooling. Fossils of these dugongs have been found in various parts of Italy, Spain and possibly on the island of Mallorca. M. subapenninum marks a return to greater body size in European Metaxytherium (4-5 meters) and possesses the largest tusk of this particular lineage. ImageSize = width:1000px height:auto barincrement:15px PlotArea = left:10px bottom:50px top:10px right:10px Period = from:-33.9 till:-2.588 TimeAxis = orientation:horizontal ScaleMajor = unit:year increment:5 start:-33.9 ScaleMinor = unit:year increment:1 start:-33.9 TimeAxis = orientation:hor AlignBars = justify Colors = #legends id:EU value:green id:AM value:blue id:black value:black id:white value:white id:cenozoic value:rgb(0.54,0.54,0.258) id:paleogene value:rgb(0.99,0.6,0.32) id:oligocene value:rgb(0.99,0.75,0.48) id:neogene value:rgb(0.999999,0.9,0.1) id:miocene value:rgb(0.999999,0.999999,0) id:pliocene value:rgb(0.97,0.98,0.68) BarData= bar:eratop bar:space bar:periodtop bar:space bar:NAM1 bar:NAM2 bar:NAM3 bar:NAM4 bar:NAM5 bar:NAM6 bar:NAM7 bar:NAM8 bar:space bar:period bar:space bar:era PlotData= align:center textcolor:black fontsize:M mark:(line,black) width:25 shift:(-7,-4) bar:periodtop from: -33.9 till: -23.03 color:oligocene text:Oligocene from: -23.03 till: -5.332 color:miocene text:Miocene from: -5.332 till: -2.588 color:pliocene text:Plio. bar:eratop from: -33.9 till: -23.03 color:paleogene text:Paleogene from: -23.03 till: -2.588 color:neogene text:Neogene PlotData= align:left fontsize:M mark:(line,white) width:5 anchor:from align:right color:AM bar:NAM1 from:-25.7 till:-23.6 text:M. albifontanum color:AM bar:NAM2 from:-20.44 till:-13.6 text:M. crataegense color:AM bar:NAM3 from:-15 till:-14 text:M. arctodites color:AM bar:NAM4 from:-14 till:-7 text:M. floridanum color:EU bar:NAM5 from:-20.8 till:-16.5 text:M. krahuletzi color:EU bar:NAM6 from:-15.97 till:-8.14 text:M. medium color:EU bar:NAM7 from:-7.3 till:-4.5 text:M. serresii color:EU bar:NAM8 from:-5.3 till:-3 text:M. subapenninum PlotData= align:center textcolor:black fontsize:M mark:(line,black) width:25 bar:period from: -33.9 till: -23.03 color:oligocene text:Oligocene from: -23.03 till: -5.332 color:miocene text:Miocene from: -5.332 till: -2.588 color:pliocene text:Plio. bar:era from: -33.9 till: -23.03 color:paleogene text:Paleogene from: -23.03 till: -2.588 color:neogene text:Neogene ==Evolution==

The exact origins of Metaxytherium are complicated and not entirely understood, with the two basal-most species being known from opposite sides of the Atlantic. Jorge Vélez-Juarbe and Daryl P. Domning propose in their 2014 paper that the closest relatives to the clade comprising dugongs, Metaxytherium and hydrodamalines are native to the Caribbean, suggesting a West-Atlantic Caribbean origin of the genus. This would place Caribosiren or a related genus as a potential ancestor of Metaxytherium. They further suggest that the genus must have originated during the middle Oligocene, due to the two basal most taxa likely having already diverged from one another prior to the Chattian. However, the large distance between these basal species, M. albifontanum and M. krahuletzi, may indicate that their origin is more complex than currently understood. The drastic increase in tusk size would also support this hypothesis, suggesting that when faced with declining resources, the European Metaxytherium adapted to better exploit what was available, including the rhizomes of seagrasses. However, more recent discoveries from Italy suggest that M. serresii already existed by the time of the Messinian Salinity Crisis, and the dwarfing may instead be a result of the Tortonian Salinity Crisis (7.8 - 7.3 Ma). The presence of Metaxytherium species on the western coast of the Americas, in addition to their close phylogenetic ties with the Hydrodamalinae, has been suggested to represent a second anagenetic lineage starting with M. crataegense entering Peru via the Central American Seaway. M. arctodites has been hypothesized to be a direct descendant of this species found further north along the Mexican and Californian coastline. The hypothesis also suggests that this northern lineage would further give rise to Dusisiren and eventually culminate in the algae specialist Hydrodamalis, which persisted until historic times. Unlike the European forms, which continuously evolved larger tusks to deal with the environmental changes of the Late Miocene Mediterranean, the American lineage took a different approach, gradually shrinking their tusks until losing their teeth entirely in Hydrodamalinae. ==Phylogeny==

Phylogenetic analysis suggests that Metaxytherium is a paraphyletic genus with close ties to the Hydrodamalinae, sea cows native to the colder waters of the northern Pacific, including the giant Steller's Sea Cow. Generally, analysis consistently recover hydrodamaline sea cows to be a direct off-shoot of the American lineage. M. subapenninum and M. serresii are generally accepted to be sister taxa and M. krahuletzi appears as the most basal most member of the genus. Vélez-Juarbe & Domning recover the following tree in their description of M. albifontanum: In their phylogeny Sirenia is limited to manatees and dugongs. == Paleobiology ==

Diet Unlike modern sirenians, Metaxytherium is known from a multitude of environments that it shared with other species of sea cows. M. albifontanum for instance coexisted with both Crenatosiren olseni and Dioplotherium manigaulti. In a 2004 publication MacFadden and colleagues attempted to determine diet and habitat of the extinct sirenians of Florida using isotopic values. Concerning Metaxytherium, both M. crataegense and M. floridanum were analyzed. In modern taxa, dugongs show a sharply downturned upper jaw, generally associated with its grazing lifestyle, while manatees have comparably shallow rostral deflection. Although not thoroughly researched, it's hypothesized that the downturned snout helps with grazing by keeping the mouth close to the ground while maintaining a horizontal posture for the rest of the body. Both types of skull morphology can be seen in the two analyzed taxa, with M. crataegense having a relatively straight upper jaw while M. floridanum shows a strong downturn similar to the dugong. Despite the more manatee-like morphology of M. crataegense, both species were recovered with mean carbon isotopic values that would indicate a specialized seagrass diet. There are some outliers however. Three of the seven M. floridanum specimens from the Clarendonian/early Hemphillian later Bone Valley sequence show carbon isotopic values indicative of a diet consisting of C3 plants (which plants in particular however could not be determined). Oxygen values generally support a marine lifestyle, but 3 isolated specimens may have lived in freshwater. There was however no overlap between the freshwater specimens and those not specialised in seagrass. The diet of the European lineage meanwhile followed a clearly observable trend from the Miocene to the Pliocene. Early taxa such as M. krahuletzi and M. medium had small tusks and likely fed on the leaves of seagrasses as well as small to medium-sized rhizomes. The Tortonian and Messinian Salinity Crisis may have caused shifts in the seagrass flora of the Mediterranean Basin, leading to a greater percentage of rhizomes in the diet of Metaxytherium and causing the "medium" sized tusk-condition seen in M. serresii. As conditions in the Mediterranean stabilized, previously dominant seagrasses such as Posidonia oceanica recolonized the area and become a key component in the sirenian's diet. M. subapenninum could have developed its larger tusks to specifically feed on the thick and nutrient rich rhizomes of Posidonia rather than returning to their previous diet. This would have been furthermore beneficial as Posidonia provided a relatively stable food source compared to some of the other seagrass species, which fluctuate in availability between seasons. Another paper from the same year describes fossils of M. subapenninum that bear toothmarks similar to those of extant juvenile Bluntnose sixgill sharks. Although adults are known to inhabit deeper waters, whereas sirenians prefer the shallows, juvenile hexanchid sharks have been observed feeding in shallower waters at night. == See also ==