| Dahalokely Temporal range: Turonian ~ | |
|---|---|
 | |
| Diagram showing known elements | |
Scientific classification  | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Dinosauria |
| Clade: | Saurischia |
| Clade: | Theropoda |
| Superfamily: | † Abelisauroidea |
| Genus: | † Dahalokely Farke & Sertich, 2013 |
| Type species | |
| †Dahalokely tokana Farke & Sertich, 2013 | |
Dahalokely is an extinct genus of carnivorous abelisauroid theropod dinosaur from the Late Cretaceous (Turonian) of Madagascar.
In 2007, during an expedition by Andrew Farke to the north of Madagascar, Joseph Sertich discovered near Antsiranana the remains of a theropod new to science. In 2010, these were completely excavated by Sertich and Liva Ratsimbaholison. The fossils were then transported to the United States of America to be prepared, repaired and scanned in the Stony Brook University. After casts had been made and stored in the Raymond M. Alf Museum of Paleontology with inventory number RAM 16010, the original fossils were returned to Madagascar and added to the collection of the University of Antananarivo. [1]
The type species Dahalokely tokana was named by Farke and Sertich in 2013. The generic name Dahalokely means "small thief" in Malagasy, deriving from its estimated length of 3.5 m (11.5 ft) smaller than those of known abelisaurids. The specific name tokana means "lonely" in the same language in reference to the isolation of the Madagascan subcontinent. During the Turonian, Madagascar and India were part of the same landmass that had separated from the rest of Gondwana. Dahalokely is the only dinosaur known from Madagascar when the island was separate from Gondwana but still connected with India, forming Indo-Madagascar. In the ZooBank the genus has the Life Science Identifier 8147803A-D4BE-4BA9-9701-D853E 37DE411 and the species the LSID AFAE32BB-123A-45D4-B931-4FF2A ABAF41C. [1]
The holotype, UA 9855, was uncovered in what is informally named the Ambolafotsy Formation, a Turonian-age deposit of the Diego Basin in northern Madagascar, about 93 million years old. [2] It consists of a partial skeleton lacking the skull, of a subadult individual, preserving vertebrae and ribs. These include the fifth neck vertebra, the first, second, sixth, seventh, eighth and ninth dorsal vertebrae, the left dorsal rib, the upper parts of two right ribs, the lower ends of two ribs and some rib fragments. The identification of the position of these elements is tentative. They were not found in articulation but were assumed to represent the same individual as they were discovered not a metre apart. [1]
Initial size estimates of Dahalokely, at 3.5 m (11.5 ft), were based on the assumption it was built like an abelisaurid. Should it have had the more elongated build of the noasaurids, it would have been 4.2–5.6 m (13.8–18.4 ft) long. [1] It was estimated as being 3.8 m (12.5 ft) in length in 2016. [3]
The describing authors established several unique derived traits, autapomorphies. The cervical vertebra has a lamina, bone sheet, between the front joint process, the prezygapophysis, and a rear process, the epipophysis, the edge of which lamina is markedly convex, the convex part being longer than the vertebral body and separated from both the prezygapophysis and the epipophysis by conspicuous notches. With the first and second dorsal vertebrae, the prezygapophysis and the lamina between it and the vertebral body are arranged on a vertical line, the joint facet of the prezygapophysis and the front vertebral body face being positioned in the same plane. With the second dorsal vertebra, the joint facets of the rear joint processes, the postzygapophyses, are strongly concave. From at least the sixth dorsal vertebra onwards, the fossa or hollowed out area, below the prezygapophysis is divided into two smaller depressions. [1]
In 2013 Dahalokely was assigned to the Abelisauroidea. The phylogenetic position of Dahalokely among abelisauroids is uncertain. Its vertebrae and ribs have features of both main groups of abelisauroids, the Noasauridae and the Abelisauridae. A phylogenetic analysis published along with its first description found Dahalokely to be a basal noasaurid, but this result was only weakly supported. The incompleteness of the remains and the lack of material that overlaps with known skeletal elements of other abelisauroid species means that the relationships of Dahalokely within the Abelisauroidea are hard to determine. [1] In 2014, Dahalokely was placed as a basal noasaurid. [4]
A phylogeny from 2018 recovered Dahalokely as forming a clade with the Indian abelisaurid Rahiolisaurus within majungasaurinae. [5] Only the phylogenies for Abelisauridae is depicted here.
In the 2021 description of Llukalkan both Rahiolisaurus and Dahalokely were recovered as basal brachyrostran carnotaurines. [6]
However, two separate studies from 2018 and 2022 instead recovered Dahalokely as a noasaurid based on their phylogenetic analyses. [7] [8]
Ceratosaurs are members of the clade Ceratosauria, a group of dinosaurs defined as all theropods sharing a more recent common ancestor with Ceratosaurus than with birds. The oldest known ceratosaur, Saltriovenator, dates to the earliest part of the Jurassic, around 199 million years ago. Ceratosauria includes three major clades: Ceratosauridae, Noasauridae, and Abelisauridae, found primarily in the Southern Hemisphere. Originally, Ceratosauria included the above dinosaurs plus the Late Triassic to Early Jurassic Coelophysoidea and Dilophosauridae, implying a much earlier divergence of ceratosaurs from other theropods. However, most recent studies have shown that coelophysoids and dilophosaurids do not form a natural group with other ceratosaurs, and are excluded from this group.
Rajasaurus is a genus of carnivorous abelisaurid theropod dinosaur from the Late Cretaceous of India, containing one species: Rajasaurus narmadensis. The bones were excavated from the Lameta Formation in the Gujarat state of Western India, probably inhabiting what is now the Narmada River Valley. It was formally described by palaeontologist Jeffrey A. Wilson and colleagues in 2003 based on a partial skeleton comprising the braincase, spine, hip bone, legs, and tail–a first for an Indian theropod. The dinosaur likely measured 6.6 metres (22 ft), and had a single horn on the forehead which was probably used for display and head-butting. Like other abelisaurids, Rajasaurus was probably an ambush predator.
Masiakasaurus is a genus of small predatory noasaurid theropod dinosaurs from the Late Cretaceous of Madagascar. In Malagasy, masiaka means "vicious"; thus, the genus name means "vicious lizard". The type species, Masiakasaurus knopfleri, was named after the musician Mark Knopfler, whose music inspired the expedition crew. It was named in 2001 by Scott D. Sampson, Matthew Carrano, and Catherine A. Forster. Unlike most theropods, the front teeth of M. knopfleri projected forward instead of straight down. This unique dentition suggests that they had a specialized diet, perhaps including fish and other small prey. Other bones of the skeleton indicate that Masiakasaurus were bipedal, with much shorter forelimbs than hindlimbs. M. knopfleri was a small theropod, reaching 1.8–2.1 m (5.9–6.9 ft) long and weighing 20 kg (44 lb).
Xenotarsosaurus is a genus of abelisaurid theropod dinosaur that lived during the Late Cretaceous of Argentina.
Abelisauridae is a family of ceratosaurian theropod dinosaurs. Abelisaurids thrived during the Cretaceous period, on the ancient southern supercontinent of Gondwana, and today their fossil remains are found on the modern continents of Africa and South America, as well as on the Indian subcontinent and the island of Madagascar. Isolated teeth were found in the Late Jurassic of Portugal, and the Late Cretaceous genera Tarascosaurus, Arcovenator and Caletodraco have been described in France. Abelisaurids possibly first appeared during the Jurassic period based on fossil records, and some genera survived until the end of the Mesozoic era, around 66 million years ago.
Aucasaurus is a genus of medium-sized abelisaurid theropod dinosaur from Argentina that lived during the Late Cretaceous of the Anacleto Formation. It was smaller than the related Carnotaurus, although more derived in some ways, such as its extremely reduced arms and almost total lack of fingers. The type skeleton is complete to the thirteenth caudal vertebra, and so is relatively well understood, and is the most complete abelisaurid yet described. However, the skull is damaged, causing some paleontologists to speculate that it was involved in a fight prior to death.
Tarascosaurus is a genus of abelisaurid theropod dinosaur from Late Cretaceous of France. It was a relatively small theropod measuring 2.5–3 metres (8.2–9.8 ft) long.
Ilokelesia is an extinct genus of abelisaurid theropod, preserved in the layers of the earliest Late Cretaceous of the Huincul Formation, Neuquén Group, located near Plaza Huincul, Neuquén Province, Argentina. The specimen, consisting of very fragmentary elements of the skull and the axial and appendicular skeleton, was described by Rodolfo Coria and Leonardo Salgado in late 1998.
Compsosuchus is a dubious genus of abelisauroid dinosaur from the Late Cretaceous Lameta Formation of India.
Majungasaurus is a genus of abelisaurid theropod dinosaur that lived in Madagascar from 70 to 66 million years ago, at the end of the Cretaceous Period, making it one of the last-known non-avian dinosaurs that went extinct during the Cretaceous–Paleogene extinction event. The genus contains a single species, Majungasaurus crenatissimus. This dinosaur is also called Majungatholus, a name which is considered a junior synonym of Majungasaurus.
Genusaurus is a genus of abelisauroid theropod from the Early Cretaceous. Its fossils were found in France. Genusaurus is believed to have lived during the Albian stage, around 112-100 million years ago.
Noasaurus is a genus of ceratosaurian theropod dinosaur genus from the late Campanian-Maastrichtian of Argentina. The type and only species is N. leali.
Spinostropheus is a genus of carnivorous neotheropod theropod dinosaur that lived in the Middle Jurassic period and has been found in the Tiouraren Formation, Niger. The type and only species is S. gautieri.
Noasauridae is an extinct family of theropod dinosaurs belonging to the group Ceratosauria. They were closely related to the short-armed abelisaurids, although most noasaurids had much more traditional body types generally similar to other theropods. Their heads, on the other hand, had unusual adaptations depending on the subfamily. 'Traditional' noasaurids, sometimes grouped in the subfamily Noasaurinae, had sharp teeth which splayed outwards from a downturned lower jaw.
Rahiolisaurus is a genus of abelisaurid theropod dinosaur which existed in India during the Late Cretaceous period. It was described in 2010, based on fossils recovered from the Lameta Formation in the Indian state of Gujarat. These fossils include elements from at least seven different individuals and are believed to have been from the Maastrichtian stage, sometime between 70 and 66 million years ago, making it one of the last non-avian dinosaurs known in the fossil record. Despite representing a variety of different growth stages, all recovered fossils from the locality indicate a single species, the type species Rahiolisaurus gujaratensis.
Eoabelisaurus is a genus of abelisauroid theropod dinosaur from the Lower Jurassic Cañadón Asfalto Formation of the Cañadón Asfalto Basin in Argentina, South America. The generic name combines a Greek ἠώς, (eos), "dawn", with the name Abelisaurus, in reference to the fact it represents an early relative of the latter. Only one species is currently recognized, E. mefi; the specific name honours the MEF, the Museo Paleontológico "Egidio Feruglio", where discoverer Diego Pol is active. It is characterized by reduced forelimb proportions that show primitive characteristics of the Abelisauridae family.
Arcovenator is an extinct genus of abelisaurid theropod dinosaurs hailing from the Late Cretaceous of France and possibly Spain. The type and only described species is Arcovenator escotae.
This timeline of ceratosaur research is a chronological listing of events in the history of paleontology focused on the ceratosaurs, a group of relatively primitive, often horned, predatory theropod dinosaurs that became the apex predators of the southern hemisphere during the Late Cretaceous. The nature and taxonomic composition of the Ceratosauria has been controversial since the group was first distinguished in the late 19th century. In 1884 Othniel Charles Marsh described the new genus and species Ceratosaurus nasicornis from the Late Jurassic Morrison Formation of the western United States. He felt that it belonged in a new family that he called the Ceratosauridae. He created the new taxon Ceratosauria to include both the Ceratosauridae and the ostrich-like ornithomimids. The idea of the Ceratosauria was soon contested, however. Later that same decade both Lydekker and Marsh's hated rival Edward Drinker Cope argued that the taxon was invalid.
Afromimus is a genus of theropod dinosaur from the Early Cretaceous Elrhaz Formation of Niger. It contains a single species, A. tenerensis, named in 2017 by Paul Sereno from parts of the right leg, vertebrae, and ribs found in the Ténéré Desert. It was originally classified as an ornithomimosaurian, but subsequently it was argued to be an abelisauroid.
Tralkasaurus is a genus of abelisaurid dinosaur from the Huincul Formation from Río Negro Province in Argentina. The type and only species is Tralkasaurus cuyi, named in 2020 by Mauricio Cerroni and colleagues based on an incomplete skeleton. A medium-sized abelisaurid, Tralkasaurus exhibits a conflicting blend of characteristics found among the early-diverging abelisauroids with others that characterize the highly specialized clade Brachyrostra, and thus its position within the clade is poorly-resolved.
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||
