Dinosaur reproduction

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Model of a dinosaur egg. NHM - Dinosaurier Eier 2.jpg
Model of a dinosaur egg.

Dinosaur reproduction shows correlation with archosaur physiology, with newborns hatching from eggs that were laid in nests. [1] [2] Dinosaurs did not nurture their offspring as mammals typically do, and because dinosaurs did not nurse, it is likely that most dinosaurs were capable of surviving on their own after hatching. [3] Although, parental care may have been required for some dinosaur species, as shown by fossil evidence. [4] [5] Dinosaur reproduction also required a mate; evidence of sexual dimorphism and courting displays have been found from fossil scrapings in sandstone and feathers on dinosaurs that lacked flight. [6] [7] [8]

Contents

Medullary bone

A discovery of features in a Tyrannosaurus rex skeleton provided more evidence that dinosaurs and birds evolved from a common ancestor and, for the first time, allowed paleontologists to establish the sex of a dinosaur. When laying eggs, female birds grow a special type of bone between the hard outer bone and the marrow of their limbs. This medullary bone, which is rich in calcium, is used to make eggshells. The presence of endosteally derived bone tissues lining the interior marrow cavities of portions of the Tyrannosaurus rex specimen's hind limb suggested that T. rex used similar reproductive strategies, and revealed the specimen to be female. [9] [10] Further research has found medullary bone in the theropod Allosaurus and the ornithopod Tenontosaurus . Because the line of dinosaurs that includes Allosaurus and Tyrannosaurus diverged from the line that led to Tenontosaurus very early in the evolution of dinosaurs, this suggests that dinosaurs in general produced medullary tissue. Medullary bone has been found in specimens of sub-adult size, which suggests that dinosaurs reached sexual maturity rather quickly for such large animals. [11]

Mating Displays

Sexual Dimorphism

Research and modern day birds suggest that dinosaurs had various methods of acquiring mates, ranging from biological traits such as sexual dimorphism, to mating displays such as dancing. [12] [13] [14] Some dinosaurs, like Ornithomimids , had feathered arms resembling wings but their bodies were too heavy for flight. [15] These wings were potentially used in mating displays, like some birds plumage does today. [15] Older studies also suggest that dinosaurs like the Lambeosaurus may have used their specialized hollow horn structures to create vocalizations specific to mating. [12] Both male and female fossils have been found, indicating these horn structures were not specific to one gender but these specialized hollow horns could have been brightly colored in order to distinguish males from females of the same species. [12] Stegosaurus fossils have potential sexual dimorphism in the shape of their back plates, with males having rounder and wider back plates while female's have taller more diamond shaped back plates. [13] These plates may have displayed colors and been a sign of health in males, while female's plates acted as defense, like a cow's horns. [13]

Mating Behavior

Large scrapes in the sandstone of Colorado suggests that dinosaurs may have danced in order to impress a potential mate, a behavior seen in their successors, birds. [14] The scrapings in the sandstone were interpreted to be evidence of mating displays areas or courtship sights, as there was no evidence of eggs in the area. [14]

Parental Care

Psittacosaurus nest Psittacosaurus nest.jpg
Psittacosaurus nest

Many dinosaurs fossils reflect instances of parental care and egg care. [16] [17] One fossil of the Pisttacosaurus sp. shows thirty-four juveniles of similar size buried along with an adult, a presumed care-taker. [16] The bone development of the juveniles suggests a slow growth rate, and the overall amount of young found together, indicates post-hatching growth that was dependent on extensive parental care. An assemblage of Protoceratops Andrewsi juveniles were found of similar size and age, suggesting that they were from the same nest. [17] These dinosaurs were found without the presence of egg shells in an oval-shaped nest, meaning that these animals grew together after hatching, potentially with some parental care. [17]

An Oviraptorosaurian nest, species unidentified. Oviraptorosaur nest.jpg
An Oviraptorosaurian nest, species unidentified.

Nest Building

Two main types of nest construction have been highlighted in fossils. [18] [19] Mound-nesting, as seen in modern archosaurs, were built-up nests made of mostly plant materials or soil. Eggs were then laid in the mound and covered to incubate through organic heat sources like decomposition of the plant material. These mound nests would allow the eggs to incubate without needing to be sat on and rotated. [18] Mound-nesting was the only option for larger dinosaurs, like sauropods, that were unable to sit on their eggs to provide warmth. The eggs of hadrosaurs have been associated with fine-grain pedogenic sediments, where eggs were left to incubate via microbial respiration. Early dinosaur eggs also lacked color, suggesting that the eggs did not need to blend in with the environment to avoid predation, as they were hidden in mounds while incubation occurred. [19] Other dinosaurs may have incubated their eggs using their body heat and feathers, [20] like oviraptors and troodontids which have been documented sitting over their eggs in semi-open nests that were at least partly exposed during incubation. [18]  

Ornithopod reproduction

Hadrosaur reproduction

In the Dinosaur Park Formation

The head of Gryposaurus notabilis. Gryposaurus BW.jpg
The head of Gryposaurus notabilis.

In a 2001 review of hadrosaur eggshell and hatchling material from Alberta's Dinosaur Park Formation, Darren Tanke and M. K. Brett-Surman concluded that hadrosaurs nested in both the ancient upland and lowlands of the formation's depositional environment. [21] The upland nesting grounds may have been preferred by the less common hadrosaurs, like Brachylophosaurus or Parasaurolophus . However, the authors were unable to determine what specific factors shaped nesting ground choice in the formation's hadrosaurs. They suggested that behavior, diet, soil condition, and competition between dinosaur species all potentially influenced where hadrosaurs nested. [21]

Sub-centimeter fragments of pebbly-textured hadrosaur eggshell have been reported from the Dinosaur Park Formation. This eggshell is similar to the hadrosaur eggshell of Devil's Coulee in southern Alberta as well as that of the Two Medicine and Judith River Formations in Montana, United States. [21] While present, dinosaur eggshell is very rare in the Dinosaur Park Formation and is only found in two different microfossil sites. [21] These sites are distinguished by large numbers of pisidiid clams and other less common shelled invertebrates like unionid clams and snails. This association is not a coincidence as the invertebrate shells would have slowly dissolved and released enough basic calcium carbonate to protect the eggshells from naturally occurring acids that otherwise would have dissolved them and prevented fossilization. [21]

In contrast with eggshell fossils, the remains of very young hadrosaurs are actually somewhat common. Tanke has observed that an experienced collector could actually discover multiple juvenile hadrosaur specimens in a single day. The most common remains of young hadrosaurs in the Dinosaur Park Formation are dentaries, bones from limbs and feet, as well as vertebral centra. The material showed little or none of the abrasion that would have resulted from transport, meaning the fossils were buried near their point of origin. [21] Bonebeds 23, 28, 47, and 50 are productive sources of young hadrosaur remains in the formation, especially bonebed 50. The bones of juvenile hadrosaurs and fossil eggshell fragments are not known to have preserved in association with each other, despite both being present in the formation. [21]

See also

Related Research Articles

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Gorgosaurus is a genus of tyrannosaurid theropod dinosaur that lived in western North America during the Late Cretaceous Period (Campanian), between about 76.5 and 75 million years ago. Fossil remains have been found in the Canadian province of Alberta and the U.S. state of Montana. Paleontologists recognize only the type species, G. libratus, although other species have been erroneously referred to the genus.

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

Hadrosaurids, or duck-billed dinosaurs, are members of the ornithischian family Hadrosauridae. This group is known as the duck-billed dinosaurs for the flat duck-bill appearance of the bones in their snouts. The ornithopod family, which includes genera such as Edmontosaurus and Parasaurolophus, was a common group of herbivores during the Late Cretaceous Period. Hadrosaurids are descendants of the Late Jurassic/Early Cretaceous iguanodontian dinosaurs and had a similar body layout. Hadrosaurs were among the most dominant herbivores during the Late Cretaceous in Asia and North America, and during the close of the Cretaceous several lineages dispersed into Europe, Africa, and South America.

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

Maiasaura is a large herbivorous saurolophine hadrosaurid ("duck-billed") dinosaur genus that lived in the area currently covered by the state of Montana and the province of Alberta, Canada, in the Upper Cretaceous Period, from 86.3 to 70.6 million years ago. Maiasaura peeblesorum is the state fossil of Montana.

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

Hypacrosaurus was a genus of duckbill dinosaur similar in appearance to Corythosaurus. Like Corythosaurus, it had a tall, hollow rounded crest, although not as large and straight. It is known from the remains of two species that spanned 75 to 67 million years ago, in the Late Cretaceous of Alberta, Canada, and Montana, United States, and is the latest hollow-crested duckbill known from good remains in North America. It was an obscure genus until the discovery in the 1990s of nests, eggs, and hatchlings belonging to H. stebingeri.

<span class="mw-page-title-main">Dinosaur Park Formation</span> Uppermost member of the Belly River Group geologic unit in Alberta, Canada

The Dinosaur Park Formation is the uppermost member of the Belly River Group, a major geologic unit in southern Alberta. It was deposited during the Campanian stage of the Late Cretaceous, between about 76.5 and 74.4 million years ago. It was deposited in alluvial and coastal plain environments, and it is bounded by the nonmarine Oldman Formation below it and the marine Bearpaw Formation above it.

<span class="mw-page-title-main">Two Medicine Formation</span> Geological formation in Montana, United States and Alberta, Canada

The Two Medicine Formation is a geological formation, or rock body, in northwestern Montana and southern Alberta that was deposited between 82.4 Ma and 74.4 Ma, during Campanian time. It crops out to the east of the Rocky Mountain Overthrust Belt, and the western portion of this formation is folded and faulted while the eastern part, which thins out into the Sweetgrass Arch, is mostly undeformed plains. Below the formation are the nearshore deposits of the Virgelle Sandstone, and above it is the marine Bearpaw Shale. Throughout the Campanian, the Two Medicine Formation was deposited between the western shoreline of the Late Cretaceous Interior Seaway and the eastward advancing margin of the Cordilleran Overthrust Belt. The Two Medicine Formation is mostly sandstone, deposited by rivers and deltas.

<i>Yamaceratops</i> Extinct genus of ceratopsian dinosaur

Yamaceratops is a genus of primitive ceratopsian that lived in Asia during the Late Cretaceous period in what is now the Javkhlant Formation. Initially, the rocks where it was found in were thought to be from the Early Cretaceous, but the age was reevaluated in 2009. It was a relatively small dinosaur, reaching 50 cm (1.6 ft) in length and 2 kg (4.4 lb) in body mass.

<i>Elongatoolithus</i> Fossil dinosaur eggs

Elongatoolithus is an oogenus of dinosaur eggs found in the Late Cretaceous formations of China and Mongolia. Like other elongatoolithids, they were laid by small theropods, and were cared for and incubated by their parents until hatching. They are often found in nests arranged in multiple layers of concentric rings. As its name suggests, Elongatoolithus was a highly elongated form of egg. It is historically significant for being among the first fossil eggs given a parataxonomic name.

<i>Macroelongatoolithus</i> Oogenus of dinosaur egg

Macroelongatoolithus is an oogenus of large theropod dinosaur eggs, representing the eggs of giant caenagnathid oviraptorosaurs. They are known from Asia and from North America. Historically, several oospecies have been assigned to Macroelongatoolithus, however they are all now considered to be a single oospecies: M. carlylensis.

<i>Macroolithus</i> Oogenus of dinosaur egg

Macroolithus is an oogenus of dinosaur egg belonging to the oofamily Elongatoolithidae. The type oospecies, M. rugustus, was originally described under the now-defunct oogenus name Oolithes. Three other oospecies are known: M. yaotunensis, M. mutabilis, and M. lashuyuanensis. They are relatively large, elongated eggs with a two-layered eggshell. Their nests consist of large, concentric rings of paired eggs. There is evidence of blue-green pigmentation in its shell, which may have helped camouflage the nests.

Continuoolithus is an oogenus of dinosaur egg found in the late Cretaceous of North America. It is most commonly known from the late Campanian of Alberta and Montana, but specimens have also been found dating to the older Santonian and the younger Maastrichtian. It was laid by an unknown type of theropod. These small eggs are similar to the eggs of oviraptorid dinosaurs, but have a distinctive type of ornamentation.

<span class="mw-page-title-main">Egg fossil</span> Fossilized remains of eggs laid by ancient animals

Egg fossils are the fossilized remains of eggs laid by ancient animals. As evidence of the physiological processes of an animal, egg fossils are considered a type of trace fossil. Under rare circumstances a fossil egg may preserve the remains of the once-developing embryo inside, in which case it also contains body fossils. A wide variety of different animal groups laid eggs that are now preserved in the fossil record beginning in the Paleozoic. Examples include invertebrates like ammonoids as well as vertebrates like fishes, possible amphibians, and reptiles. The latter group includes the many dinosaur eggs that have been recovered from Mesozoic strata. Since the organism responsible for laying any given egg fossil is frequently unknown, scientists classify eggs using a parallel system of taxonomy separate from but modeled after the Linnaean system. This "parataxonomy" is called veterovata.

<span class="mw-page-title-main">Timeline of hadrosaur research</span>

This timeline of hadrosaur research is a chronological listing of events in the history of paleontology focused on the hadrosauroids, a group of herbivorous ornithopod dinosaurs popularly known as the duck-billed dinosaurs. Scientific research on hadrosaurs began in the 1850s, when Joseph Leidy described the genera Thespesius and Trachodon based on scrappy fossils discovered in the western United States. Just two years later he published a description of the much better-preserved remains of an animal from New Jersey that he named Hadrosaurus.

Wendy Sloboda is a Canadian fossil hunter from Warner, Alberta. She has made fossil discoveries of dinosaurs and other extinct animals on several continents, with finds in Canada, Argentina, Mongolia, France, and Greenland. She is commemorated in name of the horned dinosaur Wendiceratops, remains of which she discovered in 2010, as well as the fossil footprint Barrosopus slobodai which she discovered in 2003.

<span class="mw-page-title-main">Elongatoolithidae</span> Oofamily of dinosaur eggs

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Incognitoolithus is an oogenus of medioolithid fossil bird egg. It is notable for bearing evidence of predation, possibly from a bird pecking the eggshell.

<span class="mw-page-title-main">Javkhlant Formation</span> Geological formation in Mongolia

The Javkhlant Formation is a geological formation in Mongolia whose strata date back to the Late Cretaceous possibly Santonian to Campanian. Ceratopsian, ornithopod and theropod remains been found in the formation. A prominent fossilized therizinosauroid nesting site is also known from the formation.

Darla K. Zelenitsky is a Canadian paleontologist most notable for her research on dinosaur reproductive biology and fossils. She was a part of a team that first found evidence of feathered dinosaurs in North America, and since then has co-authored over 50 different publications. Her research primarily focuses on paleobiology and paleoenvironments, with a key look on dinosaurs using extinct taxa to detect and infer the changes seen over time.

The Ohyamashimo Formation(大山下層) is an Early Cretaceous (Albian) geologic formation in Japan. It has been dated to the early-mid Albian, between 112.1 ± 0.4 Ma and 106.4 ± 0.4 Ma. Dinosaur remains have been discovered from this formation, including the sauropod Tambatitanis, the theropod Hypnovenator and the ceratopsian Sasayamagnomus. Other representative fossils from the formation include the monstersaurian lizard Morohasaurus and eutherian mammal Sasayamamylos. The depositional environment represents a fluvial system with a subhumid to semi-arid climate.

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