Lavanify is a mammalian genus from the late Cretaceous (probably Maastrichtian, about 71 to 66 million years ago) of Madagascar. The only species, L. miolaka, is known from two isolated teeth, one of which is damaged. The teeth were collected in 1995–1996 and described in 1997. The animal is classified as a member of Gondwanatheria, an enigmatic extinct group with unclear phylogeny relationships, and within Gondwanatheria as a member of the family Sudamericidae. Lavanify is most closely related to the Indian Bharattherium; the South American Sudamerica and Gondwanatherium are more distantly related. Gondwanatheres probably ate hard plant material.
Lavanify had high-crowned, curved teeth. One of the two teeth is 11.2 mm high and shows a deep furrow and, is centered laterally in the crown, a V-shaped area that consists of dentine. The other, damaged, tooth is 9.8 mm high and has at least one deep cavity (infundibulum). Characters shared by the teeth of Lavanify and Bharattherium include the presence of an infundibulum and a furrow; they both also have large, continuous bands of matrix (unbundled hydroxyapatite crystals) between the prisms (bundles of hydroxyapatite crystals) of the tooth enamel, and perikymata—wave-like ridges and grooves in the enamel surface.
Gondwanatheres are a small group of mammals of uncertain phylogeny affinities known from the late Cretaceous to the Eocene (~56–34 mya) of the Gondwanan continents, known only from teeth and a few lower jaws. Upon their discovery in the 1980s, gondwanatheres were initially thought to be —part of the same group as living , , and —but later workers have favored affinities with (a diverse group of fossil mammals) or left the relationships of the gondwanatheres open. The group comprises two families. The family Ferugliotheriidae, whose members had low-crowned teeth, occurs in the Campanian (~84–71 mya) to Maastrichtian of Argentina. All other gondwanatheres, including Lavanify, are placed in the Sudamericidae, which have high-crowned (hypsodont) teeth. These include Gondwanatherium from the Campanian and Maastrichtian of Argentina; Sudamerica from the Paleocene (~66–56 mya) of Argentina; Lavanify; at least one species from the Maastrichtian of India; an unnamed species related to Sudamerica from the Eocene of Antarctica; and an unnamed possible gondwanathere, TNM 02067, from the Cretaceous of Tanzania.Wilson et al., 2007, p. 521 In 2007, teams led by G.P. Wilson and G.V.R. Prasad independently described this animal as Dakshina and Bharattherium respectively; as the latter name was published first, it is the correct name for this genus according to the Principle of Priority.Prasad, 2008, p. 91 Gondwanatheres have been interpreted as feeding on roots, bark, and abrasive vegetation or as the earliest grass-eating mammals.Gurovich and Beck, 2009, p. 37; Wilson et al., 2007, p. 521
Several other mammals have been recorded from the late Cretaceous of Madagascar, mostly on the basis of isolated teeth. A possible second gondwanathere is represented by a tooth that is larger and lower-crowned than those of Lavanify, and a yet lower-crowned tooth may also be of a gondwanathere. A lower molar, UA 8699, may be of a marsupial or a placental and a molar fragment is referable to Multituberculata. Finally, an as-yet-undescribed mammal is known from a fairly complete skeleton. None of these mammals is related to the living mammals of the island, many of which belong to unique groups (see List of mammals of Madagascar).Krause et al., 2006, pp. 186–188 The fauna also contains , , and other animals.Krause et al., 2006, p. 178
UA 8653, the holotype, is hypsodont and curved. It is 11.2 mm high, of which the crown makes up about 85%, and the dimensions of its crown are 3.4 x 3.2 mm. The occlusal (chewing) surface is worn flat and contains a V-shaped island of dentine surrounded by tooth enamel. One side of the crown lacks enamel. Between the two arms of the V, at the lingual (inner) side of the tooth,Wilson et al., 2007, p. 526 is a furrow filled with cementum, which extends all the way through the tooth; the presence of such a long furrow distinguishes it from Gondwanatherium. The enamel is made up of small, round prisms (bundles of hydroxyapatite crystals) that are separated by large, continuous bands of interprismatic matrix (IPM; the material between the enamel prisms).
FMNH PM 59520 is 9.8 mm high. It is similar in many respects to UA 8653, but is less curved and its occlusal surface contains a large (funnel-shaped cavity), filled with cementum and surrounded by enamel that penetrates deeply into the tooth. There is also either a second infundibulum or a cementum-filled furrow. The differences in degree of curvature and occlusal morphology suggest that this tooth represents a different tooth position than UA 8653. Krause and colleagues tentatively placed this tooth in Lavanify in view of the considerable variation among other gondwanathere teeth of a single species and in the absence of evidence to the contrary.Krause et al., 1997, p. 505
Relationships
Literature cited
|
|