Septencoracias Temporal range: Eocene | |
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Holotype specimen | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Aves |
Order: | Coraciiformes |
Family: | † Primobucconidae |
Genus: | † Septencoracias Bourdon et al., 2016 |
Type species | |
†Septencoracias morsensis Bourdon et al., 2016 | |
Other species | |
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Septencoracias is an extinct genus of bird related to modern rollers and other Coraciiformes such as kingfishers, bee-eaters, motmots, and todies. It contains two species, Septencoracias morsensis described in 2016, [2] and S. simillimus, which was named in 2024. [1] It was found in the Fur Formation of Denmark, dating back to the Ypresian of the Lower Eocene Epoch, about 54 million years ago. Septencoracias is one of the earliest known members of Coraciiformes, lending insight into the earliest radiation of this group.
Septencoracias was a small bird the size of a Northern carmine bee-eater, Merops nubicus, about 25 cm in length. It had a large skull in comparison to its body, about twice the length of the humerus. It is much larger than modern day rollers and its sister taxon Primobucco , more similar in size and proportion to kingfishers, motmots, and bee-eaters. It had a stout, slightly curved beak, and the upper ridge of the beak curves gradually towards the tip of the bill like in living roller species. This is different from Primobucco which has stronger curvature on the anterior end of the beak. It had small, egg-shaped nasal openings, much different than any of its close extinct relatives or extant rollers, which have either elongated openings, slit-like openings, or large triangular nares. [2]
The only fossil specimen of Septencoracias does not preserve the sternum and shoulder girdle, except for the left scapula, which is not bifurcated as in Late Eocene and later rollers. Like in Primobucco, Septencoracias has a small claw on its alular digit, which is usually absent in modern birds. Septencoracias had a very wide pelvis, and had similar proportions in its hind limbs as modern rollers. Though most modern Coraciiformes show syndactyly, with three forward-pointing toes and toes three and four fused at the base, Septencoracias is not entirely certain to have this condition. The third and fourth digit do lie on top of each other in the fossil, with the second digit separated; however in the left foot the fourth digit is slightly separated from the third, and thus it cannot be said for certain if this condition is present in Septencoracias. [2]
The fossil remains show soft tissue preservation, mostly in the thoracic and abdominal cavities, though portions were also seen in the skull. Apart from remains of potential food material, these remains have not been thoroughly examined. [2]
Septencoracias is based on a single specimen, MGUH.VP 9509, consisting of most of the skeleton but lacking the sternum and portions of the shoulder girdle. The specimen was preserved in three dimensions, with the skull partly eroded due to it being exposed at the time of discovery. It was discovered in the Moclay Pit on the Island of Mors, in Jutland, Denmark, in the Fur Formation. This location dates to the Ypresian age of the Early Eocene, around 54 million years ago. It was found during a geology field course in an abandoned diatomite quarry. The genus name stems from 'septentrio', meaning north, and the genus name of many modern rollers, Coracias . The specific name stems from the Island of Mors. [2]
An additional specimen from the Tielt Formation in Egem, Belgium was referred to cf. Septencoracias sp. in 2019. The specimen only consists of an isolated tarsometatarsus, however it resembles that of Septencoracias in both size and shape more than any other fossil Coraciiformes, although it is slightly larger. [3]
A phylogenetic analysis in 2016 recovered Septencoracias as the sister taxon of Primobucco . The most parsimonious tree, based on 21 taxa, is shown below. [2]
Septencoracias is the oldest known member of the Coraciiformes, so it shows that this group was already fairly diversified by the Early Eocene, following the end-Cretaceous extinction. It already shows many of the derived characteristics of this group, as well as characteristics shared by its sister taxon, Primobucco. It was found with fish remains in its gut, of a very common taxon from the Fur Formation, argentinoids of about 10 cm in length. These may be the contents of the stomach, indicating that Septencoracias fed upon these fish prior to its death, and they were dissociated due to digestion and may have spread outside of the abdomen due to decay and breakage. This contributes to the idea that early roller and roller relatives had a much more varied diet than modern members of the group, which almost exclusively feed upon insects and small land vertebrates. However, Septencoracias probably mostly fed on insects and small land vertebrates, similar to its modern relatives, given that it was a terrestrial bird. [2]
Septencoracias was found in the Eastern Hemisphere, which is where all modern rollers are found, though they all occur in modern tropical and subtropical regions. Given the warmer climate of the Eocene, the finding of Septencoracias in Denmark indicates that the range of early Coraciiformes was much wider within the Northern Hemisphere during this time, due to the increased number of suitable habitats. As the globe cooled, the range of rollers was thus reduced to their present ranges. [2] This was part of a much broader trend in which many modern bird clades that were formerly found in higher latitudes during the Eocene are now restricted to the tropics and subtropics from cooling climates. [4]
The Coraciiformes are a group of usually colourful birds including the kingfishers, the bee-eaters, the rollers, the motmots, and the todies. They generally have syndactyly, with three forward-pointing toes, though in many kingfishers one of these is missing. The members of this order are linked by their “slamming” behaviour, thrashing their prey onto surfaces to disarm or incapacitate them.
Coraciidae is a family of Old World birds, which are known as rollers because of the aerial acrobatics some of these birds perform during courtship or territorial flights. Rollers resemble crows in size and build, and share the colourful appearance of kingfishers and bee-eaters, blues and pinkish or cinnamon browns predominating. The two inner front toes are connected, but not the outer one.
The todies are a family, Todidae, of tiny Caribbean birds in the order Coraciiformes, which also includes the kingfishers, bee-eaters and rollers. The family has one living genus, Todus, and one genus known from the fossil record, Palaeotodus.
Limnofregata is an extinct genus of primitive frigatebird. The two known species were described after fossils from the Early Eocene Green River Formation of Wyoming. A number of good complete and partial skeletons, some with feather impressions, are known of the type species, Limnofregata azygosternon, and L. hasegawai is known from two skulls and most of one torso.
Osteodontornis is an extinct seabird genus. It contains a single named species, Osteodontornis orri, which was described quite exactly one century after the first species of the Pelagornithidae was. O. orri was named after Santa Barbara Museum of Natural History paleontologist Phil C. Orr, for his recognition of the importance of the specimen.
The Fur Formation is a marine geological formation of Ypresian age which crops out in the Limfjord region of northern Denmark from Silstrup via Mors and Fur to Ertebølle, and can be seen in many cliffs and quarries in the area. The Diatomite Cliffs is on the Danish list of tentative candidates for World Heritage and may become a World Heritage site. Fossils found in the Fur Formation are primarily housed at the Fossil and Mo-clay Museum on Mors Island, the Fur Museum on Fur Island, and the Natural History Museum of Denmark in Copenhagen.
Dasornis is a genus of prehistoric pseudotooth birds. These were probably close relatives of either pelicans and storks or waterfowl; they are placed in the order Odontopterygiformes to account for this uncertainty.
Pseudodontornis is a rather disputed genus of the prehistoric pseudotooth birds. The pseudotooth birds or pelagornithids were probably rather close relatives of either pelicans and storks, or of waterfowl, and are here placed in the order Odontopterygiformes to account for this uncertainty. Up to five species are commonly recognized in this genus.
Lithornithidae is an extinct, possibly paraphyletic group of early paleognath birds. They are known from fossils dating to the Upper Paleocene through the Middle Eocene of North America and Europe, with possible Late Cretaceous representatives. All are extinct today; the youngest specimen is the currently unnamed SGPIMH MEV1 specimen from the mid-Eocene Messel Pit site.
Oligocolius is an unusual genus of extinct mousebird from the early to late Oligocene epoch of Germany. Oligocolius is known from two species, the type species O. brevitarsus and O. psittacocephalon. Oligocolius is a member of the family of modern mousebirds (Coliidae) and is broadly similar to them in shape. However, unlike modern mouse birds the skull and beak of Oligocolius closely resembles those of parrots, and appears to be specialised for a distinct lifestyle not found in living mousebirds.
Eocoracias is an extinct genus of bird related to modern rollers and other Coraciiformes such as kingfishers, bee-eaters, motmots, and todies. It contains one species, Eocoracias brachyptera, and it lived approximately 47 million years ago based on dating of the fossil site. It is known for a specimen having preserved non-iridescent structural coloration on its feathers, previously unknown in fossil birds. Fossils have been found at the Messel Pit in Germany.
Ueekenkcoracias is an extinct genus of primobucconid bird in the order Coraciiformes from the Huitrera Formation of Patagonia. A relatively large member of the stem-Coracii, Ueekenkcoracias possessed a robust femur and stout tibiotarsus, with a strongly projected facies articularis medialis.
Morsoravis is an extinct genus of neoavian bird from the Early Eocene Fur Formation of Denmark. It contains a single named species, Morsoravis sedilis. Fossils of Morsoravis have also been found in the Green River Formation of Wyoming and possibly the Nanjemoy Formation of Virginia.
Scaniacypselus is an extinct genus of basal swifts from the Eocene of Denmark, Germany and France. Many well preserved specimens still showing plumage were discovered in the Messel Pit near Darmstadt, Germany. Species of Scaniacypselus had relatively broader wings than modern swifts and hindlimbs better adapted to perching on tree-branches, indicating that the bird was not as aerial as its extant relatives and likely nested in trees like hummingbirds and treeswifts. Two species are recognized, S. wardi and S. szarskii.
Danielsraptor is an extinct genus of masillaraptorid bird from the Early Eocene (Ypresian) Walton Member of the London Clay Formation in Essex, United Kingdom. The genus contains a single species, D. phorusrhacoides, known from a partial skeleton.
Nasidytes is an extinct genus of loon (Gaviiformes) that lived during the early Eocene in what is now Great Britain. It contains a single species, N. ypresianus. Nasidytes is the earliest unambiguously identified loon in the fossil record.
Lutavis is an extinct genus of potentially afroavian bird from the Early Eocene London Clay Formation of Essex, United Kingdom. The genus contains a single species, L. platypelvis, known from a partial skeleton.
Minutornis is an extinct genus of parapasserine bird from the Early Eocene London Clay Formation of Essex, United Kingdom. The genus contains a single species, M. primoscenoides, known from a fragmentary skeleton.
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