Biogeography of paravian dinosaurs

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Fig. 1. Mounted skeleton cast of Deinonychus, Field Museum. FMNH Deinonychus.JPG
Fig. 1. Mounted skeleton cast of Deinonychus , Field Museum.

The biogeography of Paravian dinosaurs is the study of the global distribution of Paraves through geological history. Paraves is a clade that includes all of the Theropoda that are more closely related to birds than to oviraptorosaurs. [1] These include Dromaeosauridae and Troodontidae (historically grouped under Deinonychosauria) and Avialae (including crown group birds, i.e. modern birds). [2] The distribution of paraves is closely related to the evolution of the clade. Understanding the changes in their distributions may shed light on problems like how and why paraves evolve, eventually gaining the ability to fly.

Contents

Paraves first appeared in the fossil record in early Late Jurassic (163–145 million years ago), [3] [4] then rapidly diversified and dispersed during Cretaceous (145–66 million years ago). [5] They emerged during the breakup of Pangea (since Early-Middle Jurassic), [6] which influenced the biogeographic processes such as speciation, geodispersal and extinction. By the Late Cretaceous, Paraves reached global distribution with fossils found in modern Asia, Europe, Australia, Antarctica etc. [7] Almost all Paravian dinosaurs died out before or during the end-Cretaceous mass extinction (~66 million years ago), also called the Cretaceous-Paleogene (K-Pg) mass extinction. [8] [9] [10]

As a result of this extinction event, only a small group of avialans – neornithines  – were able to survive. [8] [11] This group of Avialae continued to flourish in Cenozoic and later evolved into all modern birds. [9]

There are limitations to be considered when studying the paleobiogeography of Paraves. Firstly, the fossil record may not represent the actual distribution of the three clades mainly due to taphonomic bias. [12] Also, the fossil record may be incomplete, which may lead to misinterpretations. [12]

Vicariance and geodispersal

Fig. 3. The figure shows two maps viewed from the North Pole at early and mid-Late Cretaceous. It illustrates the concept of geodispersal through the formation of the Bering Land Bridge between Asia and North America. Modified from Wen et al. (2016). Geodispersal at Bering Land Bridge.png
Fig. 3. The figure shows two maps viewed from the North Pole at early and mid-Late Cretaceous. It illustrates the concept of geodispersal through the formation of the Bering Land Bridge between Asia and North America. Modified from Wen et al. (2016).

Vicariance is a biogeographic process that occurs when a population is forced to separate into two or more groups due to geographic constraints. [14] [15] It is a key process in the biogeographic history of Paraves and one of the main hypotheses on the global distribution of dromaeosauridae in Late Mesozoic. [16] Pangea broke up into Laurasia and Gondwana, creating an oceanic barrier in between the two landmasses where terrestrial faunal exchange was near impossible. In a regional scale, the collapse of land bridges can also cause vicariance. [7]

Geodispersal is the process where populations migrate from their origins to other areas due to the removal of geophysical barriers like mountains and seas, connecting areas that are previously isolated. Unlike vicariance, geodispersal opens up gene flow by allowing populations that had never been in contact before to interact. [17]

In reality, vicariance and geodispersal often occur together in repeated intervals. For example, the Bering Strait (Fig. 2) between North America and Asia acts as an oceanic barrier preventing terrestrial animals from crossing from one continent to another. [18] Nonetheless, the channel was not present throughout the history of Earth. During Late Jurassic and Early Cretaceous, there were multiple occasions where the Bering Land Bridge formed between the two continents. [19] The land bridge was made by tectonic movements in Late Mesozoic, [18] and by lowering of global sea level due to climatic changes in Pleistocene. [20] It acted as an overpass for land-dwellers to move from Asia to North America, and vice versa. Evidence for this was in the speciation of troodontids in Asia and North America respectively after the Bering Land Bridge broke off in the early Late Cretaceous. [7] The land bridge was then repeatedly inundated and exposed since the breakup of Laurasia, contributing to the episodic exchange of fauna involving dinosaurs and mammals alike. [18]

Paleobiogeography

During the Early Mesozoic, the supercontinent Pangea just finished its assembly and almost immediately started breaking apart. [6] The rifting began to take place during Early to Middle Jurassic (201–163 million years ago), and gradually formed two extensive landmasses – Laurasia and Gondwana. [21] The continents then continued to be ripped apart into smaller land that resembled modern continents throughout late Mesozoic and Cenozoic. [6] The breakup of continents did not happen uniformly, and modern continents were formed at different speeds while experiencing repeated collision and rifting. [22] [21] This phenomenon is closely related to the dispersal and evolution of Paraves. [7]

Middle Jurassic

Reconstruction of Anchiornis huxleyi Anchiornis martyniuk.png
Reconstruction of Anchiornis huxleyi

There was a consensus among paleontologists that Paraves first appeared in Middle to Late Jurassic (174–145 million years ago). However, it was fairly recent when the clade Avialae was grouped under Paraves. [5] With the discovery of Anchiornis (earliest feathered dinosaur with four wings) in Tiaojishan Formation in China, [4] scientists were able to identify the appearance of Paraves within the Middle Jurassic. Anchiornis is a feathered dinosaur with anatomical features similar to that of Archaeopteryx , historically the oldest known avialan. Initially considered a basal troodontid, many paleontologists have also considered it an early avialan. Feathered dinosaurs have helped to confirm that the dinosaur-to-bird hypothesis is almost certainly true. [2] [3]

Anchiornis is seen as one of the first paravian dinosaurs to have ever existed, [4] along with several other genera from the same family (Anchiornithidae) such as Aurornis [5] and Caihong. [23] Their fossils were found in the same rock formation in China, suggesting that Paraves likely originated from Asia. [4] [23]

Following the appearance of Anchiornis and other basal paravians, a series of vicariance events were inferred to have taken place. The widespread distribution and speciation of Dromaeosauridae and Troodontidae in Late Mesozoic coincided with the timing of the Pangean breakup, thus giving rise to the hypothesis of allopatric speciation initiated by continental fragmentation. [7]

Late Jurassic

Fig. 5. A map showing the distribution of dromaeosauridae, troodontidae and avialae respectively at the end of Late Jurassic. The red line indicates the separation of Laurasia and Gondwana (no faunal exchange on land). Abbreviations: N, North America; S, South America; A, Asia; E, Europe; F, Africa; T, Antarctica; U, Australia; I, India; M, Madagascar. Modified from Ding et al. (2019). The distribution of paraves in Late Jurassic.png
Fig. 5. A map showing the distribution of dromaeosauridae, troodontidae and avialae respectively at the end of Late Jurassic. The red line indicates the separation of Laurasia and Gondwana (no faunal exchange on land). Abbreviations: N, North America; S, South America; A, Asia; E, Europe; F, Africa; T, Antarctica; U, Australia; I, India; M, Madagascar. Modified from Ding et al. (2019).

During Late Jurassic (163–145 million years ago), the land was mostly separated into Laurasia (north) and Gondwana (south). [6] In addition to that, the North Atlantic Ocean was ripped open by the separation of North America and Eurasia. In terms of biodiversity, Paraves began to speciate into three distinct clades: Dromaeosauridae, Troodontidae and Avialae. [7]

Table 1. Distribution of each clade in Late Jurassic
ContinentDromaeosauriadeTroodontidaeAvialae
Asia✓ [4]
Europe✓ [24] ✓ [25] ✓ [26]
Africa
North America✓ [27] ✓ [28]
South America
Antarctica
Australia

The oldest Archaeopteryx (Avialae) was found in the Solnhofen Limestone in Germany, [26] while the oldest evidence of Dromaeosauridae was unearthed in the Morrison Formation in North America. [27] Troodontidae continued to diversify and can be found in Asia, Europe and North America. [29] [4] [7] [25] [28] They were most probably dispersed from Asia to other continents on land. [7]

Around the same time, Avialae began to obtain the ability to fly. [30] This may contribute to the rapid diversification and dispersal of avialans in later stages. [7] [30]

Cretaceous

Fig. 6. A map showing the distribution of Paraves in Early Cretaceous. The red line indicates the separation of South America and Africa. The dotted lines indicate the position of the continents at the end of Jurassic. Abbreviations: N, North America; S, South America; A, Asia; E, Europe; F, Africa; T, Antarctica; U, Australia; I, India; M, Madagascar. Modified from Ding et al. (2019). The distribution of paraves in Early Cretaceous.png
Fig. 6. A map showing the distribution of Paraves in Early Cretaceous. The red line indicates the separation of South America and Africa. The dotted lines indicate the position of the continents at the end of Jurassic. Abbreviations: N, North America; S, South America; A, Asia; E, Europe; F, Africa; T, Antarctica; U, Australia; I, India; M, Madagascar. Modified from Ding et al. (2019).

In Early Cretaceous (145–100 million years ago), the opening of the South Atlantic Ocean commenced and South America became fully detached from Africa at approximately 100 Ma. [21] Despite the fragmentation of land, terrestrial animals can still cross from continent to continent, facilitated by the land bridges and shallow seas. [15]

Table 2. Distribution of each clade in Early Cretaceous
ContinentDromaeosauridaeTroodontidaeAvialae
Asia✓ [31] ✓✓ [32]
Europe✓
Africa✓ [1]
North America✓✓
South America✓ [33]
Antarctica
Australia✓ [34]

Apart from Troodontidae, Dromaeosauridae and Avialae began spreading to other continents. Dromaeosauridae dispersed to Asia and Africa, [7] likely made possible by the Apulian Route connecting Eurasia and Africa, [35] and the Bering Land Bridge linking North America and Asia. [18] The Apulian Route was established in early Late Jurassic and broke off towards the end of Jurassic. [35] At this stage, paravian distribution concentrated mostly on the northern hemisphere, with exceptions of avialae found in South America and Australia. [7]

The iconic Jehol Biota found in Yixian Formation and Jiufotang Formation in Inner Mongolia yielded fossils of early avialans including enantiornithes (a subclass of birds) [36] and small dromaeosaurids (i.e. microraptorians). [37] During the paravians' rapid diversification, some of the better-known dinosaurs came into existence, including the troodontid Mei. [38]

Fig. 7. A map showing the distribution of Paraves in Late Cretaceous. The dotted lines indicate the position of the continents at the end of Early Cretaceous. Abbreviations: N, North America; S, South America; A, Asia; E, Europe; F, Africa; T, Antarctica; U, Australia; I, India; M, Madagascar. Modified from Ding et al. (2019). The distribution of paraves in Late Cretaceous.png
Fig. 7. A map showing the distribution of Paraves in Late Cretaceous. The dotted lines indicate the position of the continents at the end of Early Cretaceous. Abbreviations: N, North America; S, South America; A, Asia; E, Europe; F, Africa; T, Antarctica; U, Australia; I, India; M, Madagascar. Modified from Ding et al. (2019).
Table 3. Distribution of each clade in Late Cretaceous
ContinentDromaeosauridaeTroodontidaeAvialae
Asia✓✓✓
Europe✓ [39] ✓
Africa✓✓ [40]
North America✓✓✓ [41]
South America✓ [42] ✓
Antarctica✓ [43] ✓ [44]
Australia

In Late Cretaceous (100–66 million years ago), both Dromaeosauridae and Avialae had reached global distribution, while Troodontidae remained found only in Asia (including India) and North America. [7] There were many more avialan records in Antarctica and Australia in Early Cretaceous compared to that of Late Cretaceous. [7]

Paleontologists also deduced a slight change in diet in avialans during Cretaceous. [30] While most Paraves in Late Jurassic were carnivorous (meat-eater), some avialans were found to be seed-eating in this period. This change in diet and the sudden avian diversification coincided with the spread of angiosperms (flowering plants), implying that there may have been coevolution taking place where the avialans and the flowering plants impact each other's evolution. [30]

End-Cretaceous mass extinction

The Cretaceous-Paleogene mass extinction (~66 million years ago) is one of the most-studied extinction events. While not being the largest known mass extinction event, it is famous for its impact on dinosaurs. [45] Like all other dinosaurian species, almost all Paraves died out sometime between the latest Cretaceous (Maastrichtian) and the start of Paleogene  – with one exception. Given the title "the most successful dinosaurs" by paleontologists, neornithines managed to survive the mass extinction and continued to flourish in present days. [8] [30]

The reason as to why only neornithines lived was still a very much debated topic among vertebrate paleontologists. Some believed that it was related to their global distribution and the cause of mass extinction. [8] [11] The fossil record of late Cretaceous neornithines concentrated in the southern hemisphere where Gondwana once was. [11] It is then hypothesised that life in the southern hemisphere suffered less [8] because the impact of the meteor at Chicxulub was northward-facing. [46]

Another hypothesis suggested that the extinction of non-neornithines was unlikely a result of mass extinction but was instead caused by a change in vegetation pattern. [30] It is found that a portion of non-neornithines was already extinct before the impact event. [30] This can be accounted for by the regional scale vegetation loss that occurred in North America, [47] which largely affected the atmospheric composition [48] and disrupted the food chain. [30]

Both hypotheses, along with any other possibilities, have yet to be proven with definitive evidence. One certain thing is that neornithines did not diversify much in Cretaceous compared to that in the early Cenozoic, unlike other groups of birds. [10] [49] The fossil record for neornithines in Late Cretaceous was sparse, but there was an explosive increase in fossils in Early Cenozoic. [10] As the radiation of neornithines happened together with the rise of mammals, it seems logical that the two events were related.

Paleogene-present

Fig. 8. A diagram showing the diversification of avialans before and after the K-Pg mass extinction event. The size roughly represents the number of species in that group. Basal birds diversified into different groups in the Cretaceous, while neornithines only began their rapid diversification in Paleocene. Modified from Feduccia (2014). K-Pg boundary and Radiation of Neornithines.png
Fig. 8. A diagram showing the diversification of avialans before and after the K-Pg mass extinction event. The size roughly represents the number of species in that group. Basal birds diversified into different groups in the Cretaceous, while neornithines only began their rapid diversification in Paleocene. Modified from Feduccia (2014).

As the Earth entered a new era, the continents started to move into their modern positions. [50] Australia and South America finally separated from Antarctica [51] while the Indian subplate began its collision into Asia, creating the world's largest mountain range the Himalayas. [52] At the same time, the global average temperature cooled down [53] [54] since Late Cretaceous with a Thermal Maximum at Paleocene-Eocene boundary and Middle Miocene Climatic Optimum. [55] Between these warm episodes were periods of cooling (Oligocene global cooling), [30] where seawater level fell and land bridges between Africa and Eurasia (i.e. Gomphotherium landbridge), [56] and Eurasia and North America (i.e. Bering Land Bridge) [20] were formed.

Vegetation patterns underwent drastic changes in Cenozoic. With long periods of global warming, grasslands spread to regions of higher latitudes. [57] This phenomenon facilitated the dispersal of avialans that lived in non-arboreal environments, [30] examples found in Green River Formation (USA) and Messel Oil Shale (Germany). Neornithines underwent a rapid increase in number in Paleogene in a relatively short time, though crown group birds were still sparse. [10]

Since the continents were almost entirely separated from each other, [50] neornithines began to speciate independently. [30] Most of the mutations occurred in birds without long-distance flight abilities, and the most prominent changes were found in birds living on isolated islands like New Zealand and Australia. [30] [58] It is hypothesised that due to the lack of large carnivorous (meat-eating) predators on these islands due to the extinction of dinosaurs, birds were able to evolve and adapt to the new environments. [30] Such mutations include an increase in body sizes but reduced wings and development of flightlessness, as found in birds like moas (completely extinct by the year 1440 [59] ), kiwis and ostriches. [30] Though they were not closely related to one another, this evolution pattern indicates that birds evolve similarly in isolated environments without major threats of predators. [58]

Summary of paleobiogeography

Table 4. Summary
ContinentMiddle Jurassic

(170-166Ma)

Late Jurassic

(166-145Ma)

Early Cretaceous

(145-100Ma)

Late Cretaceous

(100-66Ma)

Post K-Pg Mass Extinction

(66Ma-present)

DTADTADTADTADTA
Asia⧠⧠★⧠⚫︎★⧠⚫︎⚫︎
Europe⧠⚫︎⚫︎★⚫︎⚫︎
Africa★★⚫︎⚫︎
North America★⧠★⧠★⧠⚫︎⚫︎
South America⚫︎★⚫︎⚫︎
Antarctica★⚫︎⚫︎
Australia⚫︎⚫︎

D – Dromaeosauridae (★)

T – Troodontidae (⧠)

A – Avialae (⚫︎)

Table 5. Distribution of Dromaeosauridae through time
ContinentMiddle JurassicLate JurassicEarly CretaceousLate CretaceousPost K-Pg Mass Extinction
Asia✓✓
Europe✓
Africa✓✓
North America✓✓✓
South America✓
Antarctica✓
Australia
Table 6. Distribution of Troodontidae through time
ContinentMiddle JurassicLate JurassicEarly CretaceousLate CretaceousPost K-Pg Mass Extinction
Asia✓✓✓✓
Europe✓
Africa
North America✓✓✓
South America
Antarctica
Australia
Table 7. Distribution of Avialae through time
ContinentMiddle JurassicLate JurassicEarly CretaceousLate CretaceousPost K-Pg Mass Extinction
Asia✓✓✓
Europe✓✓✓✓
Africa✓✓
North America✓✓
South America✓✓✓
Antarctica✓✓
Australia✓✓

Limitations

Flight capabilities

There are some limitations in studying the biogeography of Paraves, including their development of flight. Flight capabilities in Paraves were developed since the Late Jurassic. [30] While only several groups of paravian dinosaurs have such abilities, it is certainly a possibility that it contributed to their dispersal in late Mesozoic. [25] In these cases, the biogeographic record of Paraves cannot be interpreted solely by whether the land was connected or not. Modern migratory birds can travel covering long distances without relying much on land. This means that the development of long-distance flight occurred at some point between the first appearance of bird-like dinosaurs and present day. [30] It is found that, at least until Early Cretaceous, Paraves can only glide between trees instead of flying like modern birds. [60] Thus, their flight abilities do not affect the dispersal of Paraves. [7] In Cenozoic, avian flight abilities were more or less developed in neornithines, though there are exceptions that are flightless birds mainly found in isolated islands. [58] Since then, flight in avians had become a major factor contributing to the dispersal of birds. [30]

Taphonomic bias

Taphonomic bias is caused by the difference in how organisms decay and fossilise. It is another challenge faced by paleontologists as the fossil records are often incomplete. [61] Moreover, some localities have better-preserved record due to their geological history than the others, leading to misinterpretations in biogeography. [62] This is especially true for dinosaurian fossil records since localities in North America and China had a much higher abundance of fossils preserved in sedimentary rocks. [7] [30] In fact, there is only one known rock formation that holds a relatively complete and dated record of the latest Cretaceous (Maastrichtian), named the Hell Creek Formation in western North America. [45] The fossils for birds (including basal avialans) in Late Cretaceous are incomplete as well, given the sparse record discovered in Australia and Antarctica. [49]

Other possible types of taphonomic bias include collecting bias. Fossils of species that lived in a specific environment can also be poorly preserved. An example being fossils of arboreal neornithines (birds that live in trees) are rarely found in the late Mesozoic and earliest Paleocene. [30] This may lead to the conclusion that they did not diversify in that period due to underrepresentation, which may or may not be true. [30]

See also

Related Research Articles

<span class="mw-page-title-main">Troodontidae</span> Extinct family of bird-like dinosaurs

Troodontidae is a clade of bird-like theropod dinosaurs. During most of the 20th century, troodontid fossils were few and incomplete and they have therefore been allied, at various times, with many dinosaurian lineages. More recent fossil discoveries of complete and articulated specimens, have helped to increase understanding about this group. Anatomical studies, particularly studies of the most primitive troodontids, like Sinovenator, demonstrate striking anatomical similarities with Archaeopteryx and primitive dromaeosaurids, and demonstrate that they are relatives comprising a clade called Paraves.

<span class="mw-page-title-main">Deinonychosauria</span> Extinct clade of dinosaurs

Deinonychosauria is a clade of paravian dinosaurs which lived from the Late Jurassic to the Late Cretaceous periods. Fossils have been found across the globe in North America, Europe, Africa, Asia, South America, and Antarctica, with fossilized teeth giving credence to the possibility that they inhabited Australia as well. This group of dinosaurs are known for their sickle-shaped toe claws and features in the shoulder bones.

<span class="mw-page-title-main">Maniraptora</span> Clade of dinosaurs

Maniraptora is a clade of coelurosaurian dinosaurs which includes the birds and the non-avian dinosaurs that were more closely related to them than to Ornithomimus velox. It contains the major subgroups Avialae, Dromaeosauridae, Troodontidae, Oviraptorosauria, and Therizinosauria. Ornitholestes and the Alvarezsauroidea are also often included. Together with the next closest sister group, the Ornithomimosauria, Maniraptora comprises the more inclusive clade Maniraptoriformes. Maniraptorans first appear in the fossil record during the Jurassic Period, and survive today as living birds.

<i>Buitreraptor</i> Dromaeosaurid dinosaur genus from the Late Cretaceous

Buitreraptor is a genus of dromaeosaurid dinosaurs that lived during the Late Cretaceous of Argentina at the Candeleros Formation. Buitreraptor was described in 2005 and the type species is Buitreraptor gonzalezorum. It was rooster-sized and had a very elongated head with many small teeth.

<i>Rahonavis</i> Extinct genus of dinosaurs

Rahonavis is a genus of bird-like theropods from the Late Cretaceous of what is now northwestern Madagascar. It is known from a partial skeleton found by Catherine Forster and colleagues in Maevarano Formation rocks at a quarry near Berivotra, Mahajanga Province. Rahonavis was a small predator, at about 70 centimetres (2.3 ft) long and 0.45-2.27 kg, with the typical Velociraptor-like raised sickle claw on the second toe. It was originally the first African coelurosaur until the Nqwebasaurus was discovered in 2000.

<span class="mw-page-title-main">Scansoriopterygidae</span> Extinct family of dinosaurs

Scansoriopterygidae is an extinct family of climbing and gliding maniraptoran dinosaurs. Scansoriopterygids are known from five well-preserved fossils, representing four species, unearthed in the Tiaojishan Formation fossil beds of Liaoning and Hebei, China.

<span class="mw-page-title-main">Archaeopterygidae</span> Family of dinosaurs

Archaeopterygidae is a group of maniraptoran dinosaurs, known from the latest Jurassic and earliest Cretaceous of Europe. In most current classifications, it contains only the genera Archaeopteryx and Wellnhoferia. As its name suggests, Protarchaeopteryx was also once referred to this group, but most paleontologists now consider it an oviraptorosaur. Other referred genera, like Jurapteryx, Wellnhoferia, and "Proornis", are probably synonymous with Archaeopteryx or do not belong into this group. Jinfengopteryx was originally described as an archaeopterygid, though it was later shown to be a troodontid. A few studies have recovered Anchiornis and Xiaotingia to also be members of the Archaeopterygidae, though most subsequent analyses have failed to arrive at the same result. Uncertainties still exist, however, and it may not be possible to confidently state whether archaeopterygids are more closely related to modern birds or to deinonychosaurs barring new and better specimens of relevant species. Teeth attributable to archaeopterygids are known from the earliest Cretaceous (Berriasian) Cherves-de-Cognac locality and the Angeac-Charente bonebed of France.

<span class="mw-page-title-main">Avialae</span> Clade including all birds and their ancestors

Avialae is a clade containing the only living dinosaurs, the birds. It is usually defined as all theropod dinosaurs more closely related to birds (Aves) than to deinonychosaurs, though alternative definitions are occasionally used.

<span class="mw-page-title-main">Alan Feduccia</span> American academic

John Alan Feduccia is a paleornithologist specializing in the origins and phylogeny of birds. He is S. K. Heninger Distinguished Professor Emeritus at the University of North Carolina. Feduccia's authored works include three major books, The Age of Birds, The Origin and Evolution of Birds, Riddle of the Feathered Dragons, and many peer-reviewed papers in ornithological and biological journals.

<span class="mw-page-title-main">Paraves</span> Clade of all dinosaurs that are more closely related to birds than to oviraptorosaurs

Paraves are a widespread group of theropod dinosaurs that originated in the Middle Jurassic period. In addition to the extinct dromaeosaurids, troodontids, anchiornithids, and possibly the scansoriopterygids, the group also contains the avialans, which include diverse extinct taxa as well as the over 10,000 species of living birds. Basal members of Paraves are well known for the possession of an enlarged claw on the second digit of the foot, which was held off the ground when walking in some species. A number of differing scientific interpretations of the relationships between paravian taxa exist. New fossil discoveries and analyses make the classification of Paraves an active subject of research.

<i>Epidexipteryx</i> Extinct genus of dinosaurs

Epidexipteryx is a genus of small paravian dinosaurs, known from one fossil specimen in the collection of the Institute of Vertebrate Paleontology and Paleoanthropology in Beijing. Epidexipteryx represents the earliest known example of ornamental feathers in the fossil record.

<i>Anchiornis</i> Extinct genus of birds

Anchiornis is a genus of small, four-winged paravian dinosaurs, with only one known species, the type species Anchiornis huxleyi, named for its similarity to modern birds. The Latin name Anchiornis derives from a Greek word meaning "near bird", and huxleyi refers to Thomas Henry Huxley, a contemporary of Charles Darwin.

<i>Xiaotingia</i> Genus of dinosaur

Xiaotingia is a genus of anchiornithid theropod dinosaur from Middle Jurassic or early Late Jurassic deposits of western Liaoning, China, containing a single species, Xiaotingia zhengi.

<span class="mw-page-title-main">Jinfengopteryginae</span> Extinct subfamily of dinosaurs

Jinfengopteryginae is a subfamily of bird-like theropod dinosaurs known from the Cretaceous of Eurasia. This group includes relatively few genera, with members discovered in 2005 but the name erected in 2012. Like other troodontids, this group of dinosaurs resided in the Paraves potentially close to the Avialae.

<span class="mw-page-title-main">Unenlagiidae</span> Extinct family of dinosaurs

Unenlagiidae is a proposed family of eumaniraptoran paravians that includes the subfamilies Unenlagiinae and possibly Halszkaraptorinae. Fossils of both subfamilies have been found in both Gondwanan and Laurasian deposits. The biology of the group suggests that some members were semiaquatic specialists.

<span class="mw-page-title-main">Anchiornithidae</span> Extinct family of reptiles

Anchiornithidae is a family of eumaniraptorans which could be the basalmost family of birds in the clade Avialae. Anchiornithids have been classified at varying positions in the maniraptoran tree, with some scientists classifying them as a distinct family, a basal subfamily of Troodontidae, members of Archaeopterygidae, or an assemblage of dinosaurs that are an evolutionary grade within Avialae or Paraves.

<i>Imperobator</i> Extinct genus of dinosaurs

Imperobator is a genus of paravian theropod, a group of large, three-toed carnivorous dinosaurs, that lived during the Maastrichtian stage of the Late Cretaceous period in what is now James Ross Island in Antarctica. Imperobator is one of only two non-avian theropods known from Antarctica, crossing over to the landmass when it was part of Gondwana. The only described specimen was found in 2003 by an expedition launched by the University of California Museum of Paleontology and initially described as a dromaeosaur in 2007. However, later searches reported more fossils from the site including teeth and skull bones. The fossils were formally described as a new genus of giant paravian in 2019.

<i>Oculudentavis</i> Extinct genus of reptiles

Oculudentavis is an extinct genus of lizard of uncertain taxonomic placement, originally identified as an avialan dinosaur. It contains two known species, O. khaungraae and O. naga. Each species is known from one partial fossil specimen in Burmese amber, which differ in several proportions. Their skulls measure 1.4–1.7 centimetres (0.55–0.67 in) in length, indicating that Oculudentavis would have been comparable in size with the modern bee hummingbird if it were an avialan. Both specimens were retrieved from 99-million-year-old deposits of the Hukawng Basin in Kachin State, northern Myanmar. The type specimen of O. khaungraae is embroiled in controversy regarding its identity and the ethical issues surrounding the acquisition and study of Burmese amber. The original description advocating for an avialan identity was published in Nature, but has since then been retracted from the journal.

<i>Overoraptor</i> Extinct genus of dinosaurs

Overoraptor is a genus of paravian theropod dinosaurs, which was closely related to Rahonavis, from the Late Cretaceous (Cenomanian) Huincul Formation of Gondwana, present-day Argentina. It includes one species, Overoraptor chimentoi.

References

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