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Dinosaur egg

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198: 237:, and eventually vomited out of the animal's system. These "stomach stones" tend to range in size from 1 to 6 centimeters. Larger sizes are known but very rare. Sometimes tiny dimples cover the surface of a stomach stone, which can fool observers into thinking they are the pores of an egg. Fossil egg expert Ken Carpenter has described stomach stones as the most egg-like natural objects, noting that they are "the trickiest objects to correctly identify". Calculi are so egg-like that on one occasion a detailed description of a stomach stone misidentified as a fossil egg was published in the scientific literature. Calculi can be distinguished from real egg fossils because when they are broken open, they show the layers of calcium phosphate and the foreign object at the core. Multiple layers of eggshell are known in 1264:, all putative embryos discovered using x-rays have been misidentifications. This is because the use of x-rays to find embryos is conceptually flawed. Embryo bones are incompletely developed and will generally lack their own mineral content, as such the only source of minerals for these bones is the sediment that fills the egg after burial. The fossilized bones will therefore have the same density as the sediment filling the interior of the egg which served as the source for their mineral content and will be poorly visible in an x-ray image. So far the only reliable method for examining embryonic fossils preserved in dinosaur eggs is to physically extract them through means such as acid dissolution. 1203:. Calcite is capable of acting as a polarizing light filter. When a microscopic thin section sample is rotated relative to polarized light it can eventually block all the light and seem opaque. This phenomenon is called extinction. Different varieties of dinosaur eggs with their different calcite crystal structures have different light extinction properties that can be used to identify and distinguish even eggs that seem very similar on the surface. To reconstruct the three-dimensional structures of the shell's pore channels scientists require a series of multiple radial sections. 1239:
gaseous eggshell molecules, which breaks down the molecules in the eggshell and imbues them with a positive charge. A magnetic field then sorts them by mass before they are detected by the spectrometer. One application of mass spectrometry has been to study the isotope ratios of dinosaur eggshell in order to ascertain their diets and living conditions. However this research is complicated by the fact that isotope ratios can be altered post mortem before or during fossilization. Bacterial decomposition can alter
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enough to have found a nest, the number and arrangement of the eggs must be estimated. Excavation must proceed to significant depth since many dinosaur nests include multiple layers of eggs. As the underside of the nest is excavated, it would be covered by material like newspaper, tin foil, or tissue. Afterwards, the entire block is covered in multiple layers of plaster-soaked strips of burlap. When the plaster is dried, the block is undercut the rest of the way and turned over.
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from being cracked. If the water table is high enough dissolved minerals like calcite can percolate through the pores of the eggshell. When the egg is completely filled it can become sturdy enough to withstand the weight of the overlying sediments. Not all fossil egg specimens are of complete specimens, however. Individual pieces of eggshell are much more robust than the entire egg and can be transported intact long distances from where they were originally laid.
3380: 1073:. Since the infilling sediment is their only source of minerals they will be preserved at basically the same density and therefore have poor visibility in the scan. The validity of this issue has been confirmed by performing Cat scans on fossil eggs known to have embryos inside and noting their poor visibility in the scan images. The only truly reliable way to discover a dinosaur embryo is to cut the egg open or dissolve some of its eggshell away. 1069:, all alleged embryos discovered using this method were actually false alarms. Variations in the type of infilling mineral or cement binding the infilling sediment into rock sometimes resemble bones in CAT scan images. Sometimes eggshell fragments that fell back into the egg when it hatched have been mistaken for embryonic bones. The use of CAT scans to search for embryonic remains is actually conceptually flawed since embryonic bones have not yet 266:
surface left by the insect during the burrow's original excavation. Fossil insect pupae can also resemble eggs. After death and burial, the decomposition of a deceased pupa would leave a gap in the sediment that could be filled with minerals carried by groundwater, forming an egg-like cast. These pseudo-eggs can be recognized by their small size (usually not much longer than a centimeter or two) and lack of an eggshell with its typical anatomy.
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fossils, which can break down amino acids. Another potential source of error is groundwater, which can leach away amino acids. These issues cast doubt as to whether the results these sorts of studies give are reliable as the actual composition of the eggshell's organic material in life. However, studies applying these techniques have made suggestive findings, including amino acid profiles in dinosaur eggs similar to those in modern birds.
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of dinosaurian eggs, proposed by the Soviet paleontologist A. Sochava, was based on grouping eggs by their pore systems. This system was abandoned when it was discovered that different eggs could have very similar pores, but pore systems do play an important role in modern eggshell parataxonomy. The density and width of the pores, combined with the eggshell's thickness can be used to predict the
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forms from crystals radiating outward from an organic core until they touch neighboring mammillae and grow upwards into the next layer. In spherulitic eggs, the eggs of non-theropod dinosaurs, the eggshell units grow upward from their organic cores; the base of each eggshell unit is rounded, but is not a true mammilla because it does not have a distinct ultrastructure from the top of the unit.
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like pores, mammillae, and prismatic or continuous layers, which are not present in concretions. Any given concretion is unlikely to be exactly the same size as any other, so associations of egg-like objects of different sizes are probably not real eggs at all. Concretions can also be far larger than any real egg so an apparently unnaturally large "egg" has probably been misidentified.
302:. Dinosaur eggs range in shape from spherical to highly elongated (some specimens three times longer than they are wide). Some elongated eggs are symmetrical, whereas others have one rounded end and one pointed end (similar to bird eggs). Most elongated eggs were laid by theropods and have an avian-like eggshell, whereas the spherical eggs typically represent non-theropod dinosaurs. 1288:
each species where compared with one another over the course of the study as well as against the fossilized eggs. The results that was retrieved from the experiment was that while sauropods laid smaller eggs in greater amounts each year, dinosaur of the theropod group was revealed to lay larger eggs less frequently over the years, similar to modern birds today.
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used together synergistically to provide a more complete understanding of the specimen under scrutiny. Eggshell specimens best suited for scanning electron microscopy are those recently broken because such a break will usually occur along the plane of the eggshell's calcite crystal lattice. First, a small specimen would be covered with a very thin layer of
241:, but these layers don't go all the way down to its core the way a stomach stone's do. Calculi are often suspiciously intact, unlike fossil eggs, which are usually damaged. Stomach stones also lack distinct shells with their attending structural components like continuous or prismatic layers, mammillae, and pores. 920:
others remain in solution. Generally, however, a fossilizing egg's shell keeps the same calcite it had in life, which allows scientists to study its original structure millions of years after the developing dinosaur hatched or died. However, eggs can also sometimes be altered after burial. This process is called
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can be used to infer the 3D structure of a fossil egg's interior by compiling images taken of slices through the egg in small regular increments. Scientists have tried to use CAT scans to look for embryo fossils contained inside the egg without having to damage the egg itself by physically extracting
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When the egg is buried deeply enough, the bacteria decomposing it no longer have access to oxygen and need to power their metabolisms with different substances. These physiological changes in the decomposers also alter the local environment in a way that allows certain minerals to be deposited, while
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The formation of fossil eggs begins with the original egg itself. Not all eggs that end up fossilizing experience the death of their embryo beforehand. Fossil eggs with open tops are common and could result from the preservation of eggs that hatched successfully. Dinosaur eggs whose embryos died were
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In all eggs, the embryo must breathe. In egg-laying amniotes (including dinosaurs), pore canals cutting through the eggshell allow gas exchange between the embryo and the outside world. Dinosaur eggshells exhibit a lot of diversity in pore size, density, and shape. One early attempt at classification
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The innermost layer, known as the mammillary layer or the cone layer, is only found in theropod eggs (the prismatic and ornithoid basic types). It is composed of cone-shaped structures called mammillae at the base of each shell unit. Mammillae are the first part of the eggshell to form. Each mammilla
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knives. Scientists must determine at what point to stop cleaning based on their own criteria. If eggs are fully extracted they can be more fully studied individually at the cost of information regarding the spatial relationships between eggs or if the eggs had hatched. Commercial fossil dealers tend
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of a dinosaur's egg. This can provide both information about nesting behavior and about the climate: eggs buried in sediment have higher rates of gas conductance than those laid in the open, and eggs laid in arid environments have lower gas conductance (to prevent water loss) than those laid in more
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Gel electrophoresis is not necessarily a perfect means of discovering the amino acid composition of dinosaur eggshell because sometimes the amount or type of amino acids present could be altered during or after preservation. One potential confounding factor would be the heating of deeply buried egg
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has been credited with groundbreaking work developing this technique. First, the paleontologist must submerge the egg in a very dilute phosphoric acid bath. Since the acid solution can penetrate the egg, every few days the specimen must be soaked in distilled water to prevent the acid from damaging
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Usually the first evidence of fossil dinosaur eggs to be discovered are shell fragments that have eroded away from the original eggs and been transported downhill by the elements. If the source eggs can be found the area must be examined for more unexposed eggs. If the paleontologists are fortunate
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Whether or not hatching was successful, burial would begin with sediments gradually entering any large openings in the shell. Even intact eggs are likely to fill with sediment once they crack under the strain of deep burial. Sometimes, though, fossilization can begin fast enough to prevent the eggs
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In order to test out how allosterics played a part in dinosaur egg size, scientists used modern day animal species such as birds, crocodiles, and tortoises in their experiment. They set the bird group as representing the theropods with the reptiles representing the sauropod group. The laid eggs of
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is used to view dinosaur eggshell under even greater magnification than is possible with light microscopy. However, this does not mean that scanning electron microscopy is necessarily the superior research method. Since both techniques provide differing amounts and types of information they can be
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pattern imposed on the eggshell by the pressure of being buried deeply. If the pressure gets severe enough, sometimes the eggshell's internal microscopic structure can be completely destroyed. Diagenesis can also happen chemically in addition to physically. The chemical conditions of a decomposing
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Sometimes the living or breeding chambers of an insect burrow are so perfectly egg-shaped that even a paleontologist can mistake a natural cast of these chambers for a fossil egg. Insect burrow fossils can sometimes be distinguished from real egg fossils by the presence of "scratch marks" on their
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out of solution. These minerals accumulate in a mass roughly shaped like the region of altered chemistry. Sometimes the mass produced is egg-shaped. Most egg-shaped concretions have uniform interiors, however some form through the accumulation of mineral in layers. These layered concretions can be
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X-ray equipment, like CAT scans, are used to study the interior of fossil eggs. Unlike CAT scans, x-ray imaging condenses the entire interior of the egg into a single two-dimensional image rather than a series of images documenting the interior in three dimensions. X-ray imaging in the context of
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to measure lenses but can also be used by paleontologists to estimate the life size of dinosaur eggs from shell fragments. The instrument can be used to help estimate the size of fossil eggshells by measuring their curved surfaces. Since most eggs aren't perfectly round measurements from multiple
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Unlike most modern eggs, many dinosaur eggs had a rough texture formed by nodes and ridges ornamenting the surface of their shell. This is predominant in Cretaceous dinosaur eggs, but very rare in eggs from the Jurassic or Triassic. Because of the lack of modern analogues, the purpose of eggshell
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Concretions also generally lack distinct shells, although sometimes they can appear to have them if their outside surfaces have been case-hardened. Since their interiors are softer, erosion can separate the two, creating eggshell pseudofossils. Real egg fossils should preserve eggshell structures
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The second layer is alternately called the prismatic layer, the columnar layer, the continuous layer, the crystalline layer, the cryptoprismatic layer, the palisade layer, the spongy layer, or the single layer. In this layer, the shell units can be distinct, partially fused together, or entirely
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The fine work of cleaning the egg fossils is performed in a laboratory. Preparation usually begins from the underside of the block, which tends to be the best preserved. Because of their fragility, cleaning fossil eggs requires patience and skill. Scientists use delicate instruments like dental
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is a method for determining eggshell composition that uses a device called a mass spectrometer. First, the eggshell sample must be powdered and placed in the mass spectrometer's vacuum chamber. The powder is vaporized by the heat of an intense laser beam. A stream of electrons then bombard the
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Prolatocanaliculate - Pores vary in width throughout their length. Gas exchange water loss rates are variable, so these eggs could have been laid in many different environments. This type is subdivided into foveocanaliculate with larger pore openings, and lagenocanaliculate with narrower pore
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parts of the egg with varying shell curvatures may be needed to get a full idea of the egg's size. Ideally an eggshell fragment being used to estimate the full size of an egg should be more than 3 cm long. Smaller eggshell fragments are better suited to other methods of study, like the
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ornamentation is unknown, but many functions have been proposed. Possibly, they provided extra strength to the eggshell without having pore canals too long for adequate gas exchange. They could also have helped keep substrate away from the pore openings of eggs that were buried, but modern
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The classification of dinosaur eggs is based on the structure of the egg shells viewed in thin section via microscope, although new techniques such as electron backscatter diffraction have been used. There are three main categories of dinosaur eggs: spherulitic (sauropods and
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the embryo before it is even exposed. If embryonic fossil bone is revealed after drying from the water bath, the exposed fossils must be delicately cleaned with fine instruments like needles and paint brushes. The exposed bone is then coated with plastic preservatives like
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crystal units. The basic arrangement and structure of these eggshell units (called the ultrastructure) is used to divide fossil eggs into several basic types, including the spherulitic, prismatic, and ornithoid basic types, which contain dinosaurs. Dinosaur eggs further
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Beach sands were a good place for dinosaurs to lay their eggs because the sand would be effective at absorbing and holding enough heat to incubate the eggs. One ancient beach deposit in northeastern Spain actually preserves about 300,000 fossil dinosaur eggs.
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can be used to expose the microstructure of shell that has been damaged by weathering. Acids are also used to extract embryo skeletons from the egg encasing them. Even fossilized soft tissue like muscle and cartilage as well as fat globules from the original
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is a method for determining eggshell composition that uses X-rays to directly bombard powdered eggshell. Upon impact some of the x-rays will be diffracted at different angles and intensities depending on the specific elements present in the eggshell.
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and has remained almost unchanged ever since. Horizontally cut thin sections are called tangential thin sections while vertically cut thin sections are called radial sections. Regardless of direction, the sample must be abraded by fine-grit
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to protect it from the acid when submerged for another round. The complete process can take months before the whole embryo is revealed. Even then only about 20% of the eggs subjected to the process reveal any embryo fossils at all.
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Fossil dinosaur eggshell fragments can be recognized based on three important traits. Their thickness should be roughly uniform, they are usually slightly curved, and their surface is covered in tiny pores. Less frequently, the
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X-rays can be used to chemically analyze dinosaur eggshell. This technique requires pure shell samples, so the fossil must be completely free of its surrounding rock matrix. The shell must then be further cleaned by an
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Norell, M. A.; Clark, J. M.; Dashzeveg, D.; Barsbold, T.; Chiappe, L. M.; Davidson, A. R.; McKenna, M. C.; Novacek, M. J. (1994). "A theropod dinosaur embryo, and the affinities of the Flaming Cliffs Dinosaur eggs".
233:. Calculus formation is a defense mechanism protecting the ruminant's stomach from damage if it swallows a foreign object while grazing. After ingestion, the object is covered by the same material composing bone, 365:
Tubocanaliculate - Large diameter pores with funnel-shaped openings on both inner and outer surfaces of the shell. These eggs would have a high gas exchange rate, and therefore were probably buried in humid
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Obliquicanaliculate - These canals cut diagonally through multiple eggshell units instead of going between them like in other pore systems. Obliquicanaliculate pores are only found in a single oogenus:
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is then used to dye the amino acids and make them visible. The bands of amino acids from the dinosaur eggs can then be compared with the banding of samples with known composition for identification.
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even harder to recognize than those with uniform interiors because the layers can resemble egg white and yolk. The yellow of the false yolk comes from minerals like limonite, siderite, and sulfur.
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present in the organic components of dinosaur eggshell. Contact with human skin can contaminate eggs with foreign amino acids, so only untouched eggs can be investigated using this technique.
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Dauphin, Y.; Jaeger, J.J. (1991). "Implications de l'analyse microstructurale et géochimique des œufs de dinosaures de la cairanne (Bassin d'Aix en Provence, France, Rognacien inférieur)".
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Multicanaliculate - Numerous large, branching, and closely spaced pore canals. They have a high gas exchange rate, so like tubocanaliculate eggs they were probably also buried humid mounds.
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Lawver, Daniel R.; Jin, Xingsheng; Jackson, Frankie D.; Wang, Qiongying (2016). "An Avian Egg from the Lower Cretaceous (Albian) Liangtoutang Formation of Zhejiang Province, China".
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Compactituberculate - The dome-shaped tops of the shell units form a dense covering of nodes on the surface of the eggshell. This type of ornamentation is most commonly seen in
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egg can make it easy for silica to be incorporated into eggshell and damage its structure. When iron-bearing substances alter eggshell it can be obvious because compounds like
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continuous. In some dinosaur eggs, the prismatic layer exhibits squamatic ultrastructure, where the prismatic structure is obscured by a rough texture resembling lizard skin.
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Giant Dinosaur (theropod) Eggs of the Oogenus Macroelongatoolithus (Elongatoolithidae) from Southeastern Idaho: Taxonomic, Paleobiogeographic, and Reproductive Implications.
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can be used to dissolve the calcite of the eggshell while leaving the shell's organic content intact. The resultant organic residue would be blended and then implanted into
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Angusticanaliculate - Long, narrow, straight pores with low pore density. These eggs would have a low gas exchange rate, and therefore they were typically laid in dry areas.
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Rimocanaliculate - Very narrow slitlike pore canals. This pore system is seen in modern ostriches, so these eggs were laid in open nests, similar to how ostriches do today.
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Since it varies from egg to egg, the texture of an eggshell's ornamentation is useful for classification. Six types of ornamentation were catalogued by Carpenter in 1999:
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Dauphin, Y. (1990). "Incidence de l'état diagénétique des coquilles d'oeufs de dinosaures sur la reconnaissance des morphotypes - exemple du Bassin d'Aix en Provence".
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Ramotuberculate - Irregular chains of nodes, typically found as a transition between the lineartuberculate midsection and dispersituberculate ends of elongated eggs.
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which bury their eggs have smooth eggshells, so this adaptation is not necessary for animals which bury their eggs. Another hypothesis, proposed by R. M. Mellon in
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Deeming, D. C. and M. W. J. Ferguson (eds.) 1991. Egg incubation: its effect on embryonic development in birds and reptiles. Cambridge University Press, UK. 448pp.
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Many dinosaur eggs have been recovered from sandstone deposits that formed in the ancient dune fields of what are now northern China and Mongolia. The presence of
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Though rare in non-avian dinosaurs, some theropod eggs and most bird eggs have a third layer (known as the external layer) made up of vertical calcite crystals.
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Mateus, I; Mateus, H; Antunes, MT; Mateus, O; Taquet, P; Ribeiro, V; Manuppella, G (1998). "Upper Jurassic theropod dinosaur embryos from Lourinhã (Portugal)".
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likely victims of similar causes to those that kill embryos in modern reptile and bird eggs. Typical causes of death include congenital problems, diseases,
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dinosaur research has generally been used to look for evidence of embryonic fossils contained inside the egg. However, as of Kenneth Carpenter's 1999 book
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to be seen. However, there are many kinds of naturally occurring objects which can resemble fossil eggs. These can fool even professional paleontologists.
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de Ricqlès, A.; Mateus, O.; Antunes, M. T.; Taquet, P. (2001). "Histomorphogenesis of embryos of Upper Jurassic theropods from Lourinhã (Portugal)".
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to expose only the bottom of the eggs since the topsides might be damaged by hatching and therefore less visually appealing to potential customers.
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Paleontologists' knowledge of the structure of dinosaur eggs is limited to the hard shell. However, it can be inferred that dinosaur eggs had an
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by the microstructural aspects of the crystalline structure of the eggshell units and by the type of their pores and their shell ornamentation.
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which must be converted to the radius in millimeters. Use of the Geneva Lens Measure to estimate the size of a fossil egg was first done by
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Dispersituberculate - Scattered nodes. This ornamentation is seen on the poles of elongated eggs, which may have allowed accumulations CO
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eggs. Egg discoveries continued to mount all over the world, leading to the development of multiple competing classification schemes.
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can be used to magnify the structure of dinosaur eggshell for scientific research. To do so an eggshell fragment must be embedded in
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are formed when decaying organisms change the chemistry of their immediate surroundings in a manner that is conducive to minerals
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Carpenter, Kenneth; Hirsch, Karl; Horner, John (1994). "Introduction". In Carpenter, Kenneth; Hirsch, Karl; Horner, John (eds.).
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preserved in their life brooding position suggests that the eggs, nests, and parents may have been rapidly buried by sandstorms.
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Moratalla, J.J.; Powell, J.E. (1994). "Dinosaur Nesting Patterns". In Carpenter, Kenneth; Hirsch, Karl; Horner, John (eds.).
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Moreno-Azanza, Miguel; Bauluz, Blanca; Canudo, José Ignacio; Gasca, José Manuel; Fernández-Baldor, Fidel Torcida (2016).
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embryo develops. When the first scientifically documented remains of non-avian dinosaurs were being described in
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Dauphin, Y. (1990). "Comparative microstructural studies of eggshells. 1. Dinosaurs of the Southern France".
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Lineartuberculate - Ridges, and chains of ridges and nodes form lines parallel to the long axis of the egg.
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are taxonomic names for types of eggshell. Nearly three dozen oogenera have been named for dinosaur eggs:
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In 1859, the first scientifically documented dinosaur egg fossils were discovered in southern France by a
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Sagenotuberculate - The nodes and ridges form a netlike pattern interspersed with pits and grooves.
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The first scientifically recognized non-avian dinosaur egg fossils were discovered in 1923 by an
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Anastomotuberculate - Ridges similar to lineartuberculate, but instead form wavy, branching, or
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Reisz, Robert R.; Scott, Diane; Sues, Hans-Dieter; Evans, David C.; Raath, Michael A. (2005).
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Paleontologist and fossil egg expert Kenneth Carpenter catalogued six types of pore systems:
3283: 2752: 2716: 2665: 2263: 2098: 1854: 1813: 1703: 1689:"Late Cretaceous Dinosaur Eggshells from the Tremp Basin, Southern Pyrenees, Lleida, Spain" 1116: 626: 413: 405: 2700: 1521: 1515: 1333: 1199:. The calcite crystal structure of dinosaur eggshell can be classified by their effect on 330:
Dinosaur eggshells are divided into one, two, or three layers of distinct ultrastructure.
8: 1465: 1459: 1269: 1100: 1081: 832: 717: 128: 2756: 2720: 2669: 2267: 2102: 1858: 1817: 1707: 3278: 3105: 2961: 2951: 2899: 2874: 2776: 2738:"Embryos of an Early Jurassic prosauropod dinosaur and their evolutionary significance" 2287: 2114: 1877: 1840: 1719: 1637: 787: 724: 703: 382: 238: 55:. In 1859, the first scientifically documented dinosaur egg fossils were discovered in 2737: 2728: 3338: 3082: 2768: 2639: 2612: 2279: 1882: 1801: 1742: 1723: 1641: 1629: 1525: 1469: 1275: 1235: 1089: 807:
Dinosaur embryos, the animal inside the eggs, are very rare but useful to understand
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in Mongolia. These eggs were mistakenly attributed to the locally abundant herbivore
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from being buried too deep, inimical temperatures, or too much or too little water.
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Eggs, Nests, and Baby Dinosaurs: A Look at Dinosaur Reproduction (Life of the Past)
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Eggs, Nests, and Baby Dinosaurs: A Look at Dinosaur Reproduction (Life of the Past)
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Eggs, Nests, and Baby Dinosaurs: A Look at Dinosaur Reproduction (Life of the Past)
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in fossil eggshell has been altered. Calcite in eggshell is either pure or rich in
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deposited at these sites are therefore excellent sources of dinosaur egg fossils.
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Fossil dinosaur eggshells, like modern bird and reptile eggshells, are made up of
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is the most important tool paleontologists have for revealing whether or not the
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Mikhailov, Konstantin (1996). "Bird Eggs in the Upper Cretaceous of Mongolia".
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The erosive effects of water can sometimes round rocks into egg-like shapes.
251: 163: 48: 2764: 2156:"A new type of dinosaur eggs from Early Cretaceous of Gansu Province, China" 3225: 3185: 3175: 3110: 3097: 2772: 2283: 1886: 1175: 1070: 1045: 938: 812: 654: 619: 598: 528: 513: 454: 158: 79: 183: 3365: 3360: 3355: 3190: 3180: 3145: 3130: 3125: 3047: 2977: 1908:"Basic Types Eggshell: Prismatic Basic Type," Carpenter (1999); page 137. 1741:. Trumpington Street, Cambridge: University of Cambridge. pp. 1–11. 1244: 1188: 1184: 1135:
is a device used to measure curved surfaces. It is most commonly used by
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Fossilized dinosaur egg from the Gobi desert, National Museum in Prague
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Xie, J.-F.; Zhang, S.-K.; Jin, X.-S.; Li, D.-Q.; Zhou, L.-Q. (2016).
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Dinosaur eggs are known from a variety of depositional environments.
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Laura E. Wilson, Karen Chin, Frankie D. Jackson, and Emily S. Bray.
1680: 1561:
Laura E. Wilson, Karen Chin, Frankie D. Jackson, and Emily S. Bray.
3313: 3170: 3165: 3160: 3078: 2982: 2913: 1845: 1220: 1145: 1032: 969: 930: 881: 808: 75: 52: 26: 2496:
https://embryo.asu.edu/pages/acid-dissolution-fossil-dinosaur-eggs
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them. However, as of Ken Carpenter's 1999 book on dinosaur eggs,
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underside of the eggshell fragment will preserve bumps known as
3318: 3288: 3195: 3150: 3052: 2997: 2987: 2848: 1005: 934: 397: 281: 218: 95: 56: 21: 1838: 3012: 2706: 2204: 2202: 1658:" (Doctoral dissertation, Montana State University, Bozeman). 1167: 1164: 1149: 230: 64: 59:
by Jean-Jacques Poech, although they were mistaken for giant
2252: 968:
Dinosaurs often laid their eggs on ancient floodplains. The
98:
inside. The oldest known dinosaur eggs and embryos are from
94:. Sometimes the egg preserves the remains of the developing 3068: 2390:"How to Fossilize an Egg," Carpenter (1999); pages 114–115. 1520:. Bloomington, Indiana: Indiana University Press. pp.  1464:. Bloomington, Indiana: Indiana University Press. pp.  1216: 1108: 1035:
can be uncovered using this method. Amateur paleontologist
1027: 1022:
Acids can be used to learn more about fossil eggs. Diluted
222: 91: 2789:"ROM Puts Oldest Dinosaur Eggs Ever Discovered on Display" 2199: 1686: 1314:"ROM Puts Oldest Dinosaur Eggs Ever Discovered on Display" 1174:. This basic method was invented by French paleontologist 47:
during the 1820s, it was presumed that dinosaurs had laid
3200: 2890: 2686: 1893: 1112: 502: 226: 2701:"Eggs with the Oldest Known Embryos of a Dinosaur Found" 1514:
Carpenter, Kenneth (1999). "How to Study a Fossil Egg".
1334:"Eggs with the Oldest Known Embryos of a Dinosaur Found" 2859: 2437: 213:
Calculi are egg-like objects formed in the stomachs of
2507:"Tools of the Trade," Carpenter (1999); pages 128–130. 2430: 2428: 2426: 2420:"How to Fossilize an Egg," Carpenter (1999); page 110. 2411:"How to Fossilize an Egg," Carpenter (1999); page 111. 2399:"How to Fossilize an Egg," Carpenter (1999); page 115. 2384: 2381:"How to Fossilize an Egg," Carpenter (1999); page 114. 2369:"How to Fossilize an Egg," Carpenter (1999); page 108. 2357:"How to Fossilize an Egg," Carpenter (1999); page 113. 2343:"How to Fossilize an Egg," Carpenter (1999); page 112. 1687:
Vianey-Liaud, Monique; Lopez-Martinez, Nieves (1997).
86:. The interior of a dinosaur egg can be studied using 2407: 2405: 2377: 2375: 2365: 2363: 2353: 2351: 2349: 2339: 2337: 1736: 1362: 1360: 2829: 2709:
Comptes Rendus de l'Académie des Sciences, Série IIA
2510: 2088: 2735: 2446: 2443:"Collecting Eggs," Carpenter (1999); pages 117–118. 2423: 1902: 457:
patterns resembling the water ripple marks in sand.
67:were not yet recognized as dinosaurs at the time). 2501: 2414: 2402: 2393: 2372: 2360: 2346: 2334: 1357: 1170:and sliced into a thin section with a thin-bladed 2595:"Tools of the Trade," Carpenter (1999); page 132. 2586:"Tools of the Trade," Carpenter (1999); page 131. 2577:"Tools of the Trade," Carpenter (1999); page 125. 2573: 2571: 2565:"Tools of the Trade," Carpenter (1999); page 124. 2556:"Tools of the Trade," Carpenter (1999); page 122. 2552: 2550: 2544:"Tools of the Trade," Carpenter (1999); page 134. 2540: 2538: 2532:"Tools of the Trade," Carpenter (1999); page 133. 2528: 2526: 2524: 2522: 2486:"Tools of the Trade," Carpenter (1999); page 130. 2482: 2480: 2478: 2476: 2470:"Tools of the Trade," Carpenter (1999); page 128. 2466: 2464: 2462: 2460: 2458: 2325: 2082: 1799: 1433: 1412: 3410: 2651: 1509: 1507: 1505: 1453: 1451: 1449: 1447: 1445: 1426: 1424: 2307: 1784: 1503: 1501: 1499: 1497: 1495: 1493: 1491: 1489: 1487: 1485: 1405: 1403: 1401: 1399: 1397: 1395: 1393: 1383: 1381: 1206: 423:and aiding the flow of oxygen and water vapor. 90:or by gradually dissolving away the shell with 2652:Horner, John R.; Weishampel, David B. (1996). 2589: 2580: 2568: 2559: 2547: 2535: 2519: 2473: 2455: 2452:"Collecting Eggs," Carpenter (1999); page 118. 2434:"Collecting Eggs," Carpenter (1999); page 117. 2147: 1366:"Collecting Eggs," Carpenter (1999); page 115. 1354:"First Discoveries," Carpenter (1999); page 4. 1345:"First Discoveries," Carpenter (1999); page 5. 1303:"First Discoveries," Carpenter (1999); page 1. 2875: 2153: 1611: 1442: 1439:"Fake Eggs," Carpenter (1999); pages 119–120. 1421: 1418:"Fake Eggs," Carpenter (1999); pages 120–121. 990: 941:can turn the shell blackish or rusty colors. 2298: 1800:Soto, M.; Perea, D.; Cambiaso, A.V. (2012). 1482: 1458:Carpenter, Kenneth (1999). "Making an Egg". 1390: 1378: 1369: 1223:. The specimen would then be bombarded with 944: 2689:Memórias da Academia das Ciências de Lisboa 2632:Dinosaurs: The Encyclopedia. 3rd Supplement 2316: 1348: 1339: 1297: 2882: 2868: 2322:"Abstract," Reisz et al. (2005); page 761. 1648: 1103:has been used in attempts to identify the 924:. One form of diagenesis is a microscopic 2677: 1954: 1876: 1866: 1667: 1513: 1457: 1326: 1144:. The Geneva Lens measure gives units in 444:at the poles to escape between the nodes. 1952: 1950: 1948: 1946: 1944: 1942: 1940: 1938: 1936: 1934: 1911: 1806:Journal of South American Earth Sciences 1780: 1778: 1776: 1774: 1430:"Fake Eggs," Carpenter (1999); page 119. 1409:"Fake Eggs," Carpenter (1999); page 120. 1387:"Fake Eggs," Carpenter (1999); page 121. 1375:"Fake Eggs," Carpenter (1999); page 118. 492: 304: 196: 121: 20: 2516:"Fig 7.11," Carpenter (1999); page 118. 1853:(5) (published May 4, 2016): e0153026. 1596: 1577: 1557: 1555: 1553: 1551: 1549: 1547: 1545: 1543: 1541: 3411: 1306: 1126: 1095: 1076: 1012: 78:. Dinosaur eggshell can be studied in 16:Vessel for dinosaur embryo development 2863: 1931: 1771: 1767:UCMP Online Exhibits: Fossil Eggshell 1755: 1730: 1661: 1567:UCMP Online Exhibits: Fossil Eggshell 1563:II. Eggshell morphology and structure 3391: 2807:University of Bristol Earth Sciences 2628:"Appendix: Dinosaur Tracks and Eggs" 2625: 1793: 1538: 1230: 1191:. Then the structure of the shell's 145:and amateur naturalist named Father 1155: 1017: 319: 157:crew while looking for evidence of 39:are the organic vessels in which a 13: 2091:Journal of Vertebrate Paleontology 309:Diagram of a two-layered eggshell. 155:American Museum of Natural History 133:egg with preserved embryo, at the 72:American Museum of Natural History 14: 3440: 2825: 2798:. insidetoronto.com. May 6, 2010. 1323:. insidetoronto.com. May 6, 2010. 1195:or pores can be examined under a 819:. Embryo fossils are known from: 461: 176: 3390: 3379: 3378: 2847: 2832: 390: 31:Indroda Dinosaur and Fossil Park 2489: 2246: 2235: 2224: 2213: 2188: 2136: 2125: 2071: 2060: 2049: 2038: 2027: 2016: 2005: 1994: 1983: 1972: 1961: 1832: 1605: 1590: 1571: 1262:Eggs, Nests, and Baby Dinosaurs 1067:Eggs, Nests, and Baby Dinosaurs 118:Timeline of egg fossil research 108:, about 190 million years ago. 2703:. BBC News. November 12, 2010. 1336:. BBC News. November 12, 2010. 344: 1: 2729:10.1016/s1251-8050(01)01580-4 2601: 2111:10.1080/02724634.2016.1100631 205: 2611:, Indiana University Press; 2276:10.1126/science.266.5186.779 1868:10.1371/journal.pone.0153026 1826:10.1016/j.jsames.2011.08.003 1614:Paläontologische Zeitschrift 1291: 1212:Scanning electron microscopy 1207:Scanning electron microscopy 1056: 896: 275: 7: 2607:Carpenter, Kenneth (1999). 482: 479:, including modern birds). 10: 3445: 2242:The Palaeobiology Database 2231:The Palaeobiology Database 2220:The Palaeobiology Database 2209:The Palaeobiology Database 2195:The Palaeobiology Database 2143:The Palaeobiology Database 2132:The Palaeobiology Database 2078:The Palaeobiology Database 2067:The Palaeobiology Database 2056:The Palaeobiology Database 2045:The Palaeobiology Database 2034:The Palaeobiology Database 2023:The Palaeobiology Database 2012:The Palaeobiology Database 2001:The Palaeobiology Database 1990:The Palaeobiology Database 1979:The Palaeobiology Database 1968:The Palaeobiology Database 991:Excavation and preparation 900: 802: 167:, but are now known to be 115: 111: 3374: 3249: 3096: 3061: 2970: 2932: 2906: 2897: 2803:"What are dinosaur eggs?" 2313:de Ricqles et al. (2001). 2169:(1): 1–10. Archived from 1716:10.1017/s002233600003609x 1254: 945:Depositional environments 325: 104:, which lived during the 2889: 2626:Glut, Donald F. (2003), 1787:Dinosaur Eggs and Babies 1763:V. Paleobiology and eggs 1739:Dinosaur Eggs and Babies 1601:. sér/ II, 310: 849–954. 1152:on fossil ostrich eggs. 2765:10.1126/science.1114942 1920:What are dinosaur eggs? 1696:Journal of Paleontology 1670:Paleontological Journal 1197:petrographic microscope 1142:Obrig radius dial gauge 3424:Dinosaur trace fossils 2163:Vertebrata PalAsiatica 1654:Simon, D. J. (2014). " 1599:C. R. Acad. Sci. Paris 1580:Revue de Paléobiologie 1000:picks, needles, small 522: 310: 202: 138: 33: 3429:Dinosaur reproduction 2794:May 10, 2010, at the 2304:Mateus et al. (1998). 1319:May 10, 2010, at the 1004:engraving tools, and 753:Spheruprismatoolithus 578:Dispersituberoolithus 496: 308: 263:Insect trace fossils: 200: 125: 24: 3284:Egg drop competition 2856:at Wikimedia Commons 1251:ratios of eggshell. 1117:Protein silver stain 627:Macroelongatoolithus 414:Princeton University 2813:on February 1, 2014 2757:2005Sci...309..761R 2721:2001CRASE.332..647D 2670:1996Natur.383..103H 2268:1994Sci...266..779N 2176:on January 29, 2016 2103:2016JVPal..36E0631L 1927:on February 1, 2014 1859:2016PLoSO..1153026M 1818:2012JSAES..33...68S 1708:1997JPal...71.1157V 1243:ratios in eggs and 1133:Geneva Lens Measure 1127:Geneva lens measure 1101:Gel electrophoresis 1096:Gel electrophoresis 1082:Cathodoluminescence 1077:Cathodoluminescence 1013:Research techniques 718:Protoceratopsidovum 147:Jean-Jacques Pouech 82:and viewed under a 3279:Egg-and-spoon race 3106:List of egg dishes 2919:Fish and amphibian 2900:List of egg topics 2699:Moskvitch, Katia. 1626:10.1007/bf02989853 1332:Moskvitch, Katia. 788:Tristraguloolithus 725:Pseudogeckoolithus 704:Preprismatoolithus 523: 383:Preprismatoolithus 355:humid conditions. 311: 203: 139: 51:because they were 34: 29:eggs displayed at 3406: 3405: 3339:Ovo vegetarianism 2852:Media related to 2751:(5735): 761–764. 2664:(6595): 256–257. 2645:978-0-7864-1166-5 2262:(5186): 779–782. 1748:978-0-521-44342-5 1531:978-0-253-33497-8 1475:978-0-253-33497-8 1276:X-ray diffraction 1236:Mass spectrometry 1231:Mass spectrometry 1090:calcium carbonate 690:Porituberoolithus 669:Paraspheroolithus 662:Pachycorioolithus 641:Nanshiungoolithus 475:, and ornithoid ( 315:calcium carbonate 239:pathological eggs 235:calcium phosphate 3436: 3394: 3393: 3382: 3381: 3136:Custard desserts 2884: 2877: 2870: 2861: 2860: 2851: 2842: 2840:Dinosaurs portal 2837: 2836: 2835: 2821: 2820: 2818: 2809:, archived from 2787:Skinner, Justin. 2784: 2742: 2732: 2696: 2683: 2681: 2679:10.1038/383103b0 2648: 2596: 2593: 2587: 2584: 2578: 2575: 2566: 2563: 2557: 2554: 2545: 2542: 2533: 2530: 2517: 2514: 2508: 2505: 2499: 2493: 2487: 2484: 2471: 2468: 2453: 2450: 2444: 2441: 2435: 2432: 2421: 2418: 2412: 2409: 2400: 2397: 2391: 2388: 2382: 2379: 2370: 2367: 2358: 2355: 2344: 2341: 2332: 2329: 2323: 2320: 2314: 2311: 2305: 2302: 2296: 2295: 2250: 2244: 2239: 2233: 2228: 2222: 2217: 2211: 2206: 2197: 2192: 2186: 2185: 2183: 2181: 2175: 2160: 2151: 2145: 2140: 2134: 2129: 2123: 2122: 2086: 2080: 2075: 2069: 2064: 2058: 2053: 2047: 2042: 2036: 2031: 2025: 2020: 2014: 2009: 2003: 1998: 1992: 1987: 1981: 1976: 1970: 1965: 1959: 1956: 1929: 1928: 1923:, archived from 1915: 1909: 1906: 1900: 1897: 1891: 1890: 1880: 1870: 1836: 1830: 1829: 1797: 1791: 1790: 1782: 1769: 1759: 1753: 1752: 1734: 1728: 1727: 1702:(6): 1157–1171. 1693: 1684: 1678: 1677: 1665: 1659: 1652: 1646: 1645: 1620:(3–4): 391–404. 1609: 1603: 1602: 1594: 1588: 1587: 1575: 1569: 1559: 1536: 1535: 1511: 1480: 1479: 1455: 1440: 1437: 1431: 1428: 1419: 1416: 1410: 1407: 1388: 1385: 1376: 1373: 1367: 1364: 1355: 1352: 1346: 1343: 1337: 1330: 1324: 1312:Skinner, Justin. 1310: 1304: 1301: 1193:calcite crystals 1161:Light microscopy 1156:Light microscopy 1018:Acid dissolution 861:Lourinhanosaurus 697:Polyclonoolithus 3444: 3443: 3439: 3438: 3437: 3435: 3434: 3433: 3409: 3408: 3407: 3402: 3370: 3245: 3092: 3057: 2993:Ichthyoplankton 2966: 2928: 2902: 2893: 2888: 2854:Dinosauria eggs 2838: 2833: 2831: 2828: 2816: 2814: 2801: 2796:Wayback Machine 2740: 2715:(10): 647–656. 2646: 2604: 2599: 2594: 2590: 2585: 2581: 2576: 2569: 2564: 2560: 2555: 2548: 2543: 2536: 2531: 2520: 2515: 2511: 2506: 2502: 2494: 2490: 2485: 2474: 2469: 2456: 2451: 2447: 2442: 2438: 2433: 2424: 2419: 2415: 2410: 2403: 2398: 2394: 2389: 2385: 2380: 2373: 2368: 2361: 2356: 2347: 2342: 2335: 2330: 2326: 2321: 2317: 2312: 2308: 2303: 2299: 2251: 2247: 2240: 2236: 2229: 2225: 2218: 2214: 2207: 2200: 2193: 2189: 2179: 2177: 2173: 2158: 2152: 2148: 2141: 2137: 2130: 2126: 2097:(3): e1100631. 2087: 2083: 2076: 2072: 2065: 2061: 2054: 2050: 2043: 2039: 2032: 2028: 2021: 2017: 2010: 2006: 1999: 1995: 1988: 1984: 1977: 1973: 1966: 1962: 1957: 1932: 1917: 1916: 1912: 1907: 1903: 1898: 1894: 1837: 1833: 1798: 1794: 1783: 1772: 1760: 1756: 1749: 1735: 1731: 1691: 1685: 1681: 1666: 1662: 1653: 1649: 1610: 1606: 1595: 1591: 1576: 1572: 1560: 1539: 1532: 1512: 1483: 1476: 1456: 1443: 1438: 1434: 1429: 1422: 1417: 1413: 1408: 1391: 1386: 1379: 1374: 1370: 1365: 1358: 1353: 1349: 1344: 1340: 1331: 1327: 1321:Wayback Machine 1311: 1307: 1302: 1298: 1294: 1270:ultrasonic bath 1257: 1233: 1209: 1201:polarized light 1158: 1129: 1098: 1079: 1059: 1020: 1015: 993: 947: 905: 899: 894: 815:, and dinosaur 805: 800: 760:Stromatoolithus 732:Shixingoolithus 711:Prismatoolithus 606:Heishanoolithus 592:Elongatoolithus 557:Continuoolithus 500:nest and eggs ( 485: 464: 443: 421: 393: 352:gas conductance 347: 328: 278: 208: 179: 151:serendipitously 143:Catholic priest 120: 114: 17: 12: 11: 5: 3442: 3432: 3431: 3426: 3421: 3404: 3403: 3401: 3400: 3388: 3375: 3372: 3371: 3369: 3368: 3363: 3358: 3353: 3352: 3351: 3349:Vegreville egg 3341: 3336: 3331: 3326: 3321: 3316: 3311: 3306: 3301: 3296: 3291: 3286: 3281: 3276: 3271: 3266: 3261: 3255: 3253: 3247: 3246: 3244: 3243: 3238: 3233: 3228: 3223: 3218: 3213: 3208: 3203: 3198: 3193: 3188: 3183: 3178: 3173: 3168: 3163: 3158: 3153: 3148: 3143: 3138: 3133: 3128: 3123: 3118: 3113: 3108: 3102: 3100: 3094: 3093: 3091: 3090: 3085: 3076: 3071: 3065: 3063: 3059: 3058: 3056: 3055: 3050: 3045: 3040: 3035: 3030: 3025: 3020: 3015: 3010: 3005: 3000: 2995: 2990: 2985: 2980: 2974: 2972: 2968: 2967: 2965: 2964: 2959: 2949: 2944: 2938: 2936: 2930: 2929: 2927: 2926: 2921: 2916: 2910: 2908: 2904: 2903: 2898: 2895: 2894: 2887: 2886: 2879: 2872: 2864: 2858: 2857: 2844: 2843: 2827: 2826:External links 2824: 2823: 2822: 2799: 2785: 2733: 2704: 2697: 2684: 2649: 2644: 2623: 2620: 2603: 2600: 2598: 2597: 2588: 2579: 2567: 2558: 2546: 2534: 2518: 2509: 2500: 2498:Last paragraph 2488: 2472: 2454: 2445: 2436: 2422: 2413: 2401: 2392: 2383: 2371: 2359: 2345: 2333: 2324: 2315: 2306: 2297: 2245: 2234: 2223: 2212: 2198: 2187: 2146: 2135: 2124: 2081: 2070: 2059: 2048: 2037: 2026: 2015: 2004: 1993: 1982: 1971: 1960: 1930: 1910: 1901: 1892: 1831: 1792: 1770: 1754: 1747: 1729: 1679: 1660: 1647: 1604: 1589: 1570: 1537: 1530: 1481: 1474: 1441: 1432: 1420: 1411: 1389: 1377: 1368: 1356: 1347: 1338: 1325: 1305: 1295: 1293: 1290: 1256: 1253: 1249:oxygen isotope 1247:can alter the 1241:carbon isotope 1232: 1229: 1208: 1205: 1157: 1154: 1128: 1125: 1097: 1094: 1078: 1075: 1058: 1055: 1019: 1016: 1014: 1011: 992: 989: 946: 943: 901:Main article: 898: 895: 893: 892: 885: 878: 871: 868:Massospondylus 864: 857: 850: 843: 836: 829: 821: 804: 801: 799: 798: 791: 784: 777: 770: 767:Subtiliolithus 763: 756: 749: 742: 735: 728: 721: 714: 707: 700: 693: 686: 679: 676:Phaceloolithus 672: 665: 658: 651: 648:Oblongoolithus 644: 637: 630: 623: 616: 613:Laevisoolithus 609: 602: 595: 588: 585:Ellipsoolithus 581: 574: 567: 560: 553: 550:Cairanoolithus 546: 543:Boletuoolithus 539: 532: 524: 484: 481: 463: 462:Classification 460: 459: 458: 451: 448: 445: 441: 438: 435: 432:megaloolithids 419: 392: 389: 388: 387: 377: 374: 370: 367: 363: 346: 343: 327: 324: 277: 274: 207: 204: 178: 177:Identification 175: 153:in 1923 by an 116:Main article: 113: 110: 106:Early Jurassic 101:Massospondylus 15: 9: 6: 4: 3: 2: 3441: 3430: 3427: 3425: 3422: 3420: 3417: 3416: 3414: 3399: 3398: 3389: 3387: 3386: 3377: 3376: 3373: 3367: 3364: 3362: 3359: 3357: 3354: 3350: 3347: 3346: 3345: 3342: 3340: 3337: 3335: 3334:Organizations 3332: 3330: 3327: 3325: 3322: 3320: 3317: 3315: 3312: 3310: 3309:Humpty Dumpty 3307: 3305: 3302: 3300: 3297: 3295: 3292: 3290: 3287: 3285: 3282: 3280: 3277: 3275: 3272: 3270: 3267: 3265: 3262: 3260: 3257: 3256: 3254: 3252: 3248: 3242: 3239: 3237: 3234: 3232: 3229: 3227: 3224: 3222: 3219: 3217: 3214: 3212: 3209: 3207: 3204: 3202: 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586: 582: 580: 579: 575: 573: 572: 571:Dictyoolithus 568: 566: 565: 564:Dendroolithus 561: 559: 558: 554: 552: 551: 547: 545: 544: 540: 538: 537: 536:Apheloolithus 533: 531: 530: 526: 525: 520: 516: 515: 510: 509: 505: 504: 499: 498:Therizinosaur 495: 491: 489: 480: 478: 474: 470: 456: 452: 449: 446: 439: 436: 433: 429: 428: 427: 424: 422: 415: 411: 410:senior thesis 407: 403: 399: 391:Ornamentation 385: 384: 378: 375: 371: 368: 364: 361: 360: 359: 356: 353: 342: 339: 335: 331: 323: 321: 316: 307: 303: 301: 300:elephant bird 297: 296: 295:Megaloolithus 291: 287: 283: 273: 271: 267: 264: 260: 256: 253: 252:precipitating 249: 246: 242: 240: 236: 232: 228: 224: 220: 216: 212: 199: 195: 193: 189: 185: 174: 172: 171: 166: 165: 164:Protoceratops 160: 156: 152: 148: 144: 136: 132: 130: 124: 119: 109: 107: 103: 102: 97: 93: 89: 85: 81: 77: 73: 68: 66: 62: 58: 54: 50: 46: 42: 38: 37:Dinosaur eggs 32: 28: 23: 19: 3395: 3383: 3176:Onsen tamago 2955: 2815:, retrieved 2811:the original 2806: 2748: 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Retrieved 2171:the original 2166: 2162: 2149: 2138: 2127: 2094: 2090: 2084: 2073: 2062: 2051: 2040: 2029: 2018: 2007: 1996: 1985: 1974: 1963: 1958:Glut (2003). 1925:the original 1919: 1913: 1904: 1895: 1850: 1844: 1834: 1812:(1): 68–79. 1809: 1805: 1795: 1786: 1766: 1757: 1738: 1732: 1699: 1695: 1682: 1673: 1669: 1663: 1650: 1617: 1613: 1607: 1598: 1592: 1583: 1579: 1573: 1566: 1516: 1460: 1435: 1414: 1371: 1350: 1341: 1328: 1308: 1299: 1286: 1282: 1281: 1274: 1266: 1261: 1258: 1234: 1210: 1187:until it is 1176:Paul Gervais 1159: 1130: 1121: 1099: 1080: 1066: 1060: 1046:Paraloid B72 1042:Acryloid B67 1021: 998: 994: 982: 975: 974: 962: 961: 952: 951: 948: 939:iron sulfide 918: 914: 906: 887: 873: 866: 859: 852: 838: 831: 824: 813:heterochrony 806: 793: 786: 779: 772: 765: 758: 751: 744: 737: 730: 723: 716: 709: 702: 695: 688: 683:Placoolithus 681: 674: 667: 660: 655:Ovaloolithus 653: 646: 639: 632: 625: 620:Macroolithus 618: 611: 604: 599:Faveoolithus 597: 590: 583: 576: 569: 562: 555: 548: 541: 534: 529:Ageroolithus 527: 514:Dinosaurland 512: 506: 501: 486: 465: 455:anastomosing 425: 402:crocodylians 394: 381: 357: 348: 340: 336: 332: 329: 312: 293: 279: 269: 268: 262: 261: 257: 245:Concretions: 244: 243: 210: 209: 180: 168: 162: 159:early humans 140: 127: 99: 80:thin section 69: 36: 35: 18: 3294:Fabergé egg 2180:January 11, 1283:Allosterics 1245:groundwater 1189:translucent 1185:emery paper 1105:amino acids 1071:mineralized 1024:acetic acid 964:Floodplains 954:Beach sands 910:suffocation 817:systematics 508:Segnosaurus 345:Pore canals 248:Concretions 25:Fossilized 3413:Categories 3304:HowToBasic 3299:Free range 3274:Easter egg 3269:Decorating 3251:In culture 3141:Deep fried 3062:Components 2942:Cephalopod 2695:: 101–110. 2602:References 1586:: 127–133. 977:Sand dunes 922:diagenesis 826:Beibeilong 739:Sphaerovum 521:, England. 519:Lyme Regis 511:) in from 469:hadrosaurs 320:classified 206:False eggs 192:microscope 84:microscope 3259:Balancing 3221:Scrambled 3033:Ovulation 3023:Oviparity 3003:Oogenesis 2962:Pathology 2924:Monotreme 1724:131405598 1642:129041143 1634:0031-0220 1292:Footnotes 1225:electrons 1137:opticians 1062:CAT scans 1057:CAT scans 1050:Vinac B15 1002:pneumatic 984:Oviraptor 970:mudstones 897:Taphonomy 875:Maiasaura 840:Heyuannia 477:theropods 473:prismatic 373:openings. 290:allantois 288:, and an 276:Structure 215:ruminants 211:Calculus: 188:mammillae 170:Oviraptor 131:osmolskae 88:CAT scans 61:bird eggs 3385:Category 3186:Powdered 3171:Omelette 3166:Meringue 3116:Benedict 3083:membrane 2983:Egg cell 2956:dinosaur 2817:June 20, 2792:Archived 2781:37548361 2773:16051793 2292:22333224 2284:17730398 2119:88169746 1887:27144767 1846:PLOS ONE 1317:Archived 1221:platinum 1172:rock saw 1146:diopters 1033:egg yolk 931:hematite 882:Qianlong 833:Citipati 809:ontogeny 488:Oogenera 483:Oogenera 217:such as 129:Citipati 76:Mongolia 74:crew in 53:reptiles 41:dinosaur 27:sauropod 3397:Commons 3366:Tossing 3361:Tapping 3356:Rolling 3344:Pysanka 3329:Organic 3324:Oomancy 3236:Soufflé 3226:Shirred 3191:Pickled 3181:Poached 3146:Deviled 3131:Coddled 3126:Century 3098:As food 3088:Chalaza 3048:Trophic 3018:Oviduct 3008:Ootheca 2978:Allergy 2971:Biology 2952:Reptile 2753:Bibcode 2745:Science 2717:Bibcode 2666:Bibcode 2636:613–652 2264:Bibcode 2256:Science 2099:Bibcode 1878:4856302 1855:Bibcode 1814:Bibcode 1704:Bibcode 1522:122–144 1086:calcium 889:Troodon 803:Embryos 408:in his 398:turtles 366:mounds. 286:chorion 270:Stones: 184:concave 112:History 45:England 3319:Oology 3289:Egging 3264:Carton 3231:Smoked 3216:Scotch 3211:Salted 3196:Quiche 3151:Eggnog 3121:Boiled 3053:Zygote 2998:Oogamy 2988:Embryo 2779:  2771:  2658:Nature 2642:  2615:  2290:  2282:  2117:  1885:  1875:  1745:  1722:  1640:  1632:  1528:  1472:  1466:85–107 1255:X rays 1006:X-Acto 937:, and 935:pyrite 326:Layers 282:amnion 229:, and 219:cattle 96:embryo 57:France 3206:Salad 3156:Fried 3111:Balut 3079:Shell 3074:White 3043:Tooth 3038:Spawn 3013:Ovary 2907:Types 2777:S2CID 2741:(PDF) 2288:S2CID 2174:(PDF) 2159:(PDF) 2115:S2CID 1720:S2CID 1692:(PDF) 1638:S2CID 1168:resin 1165:epoxy 1150:Sauer 1048:, or 231:goats 65:birds 3419:Eggs 3314:Hunt 3161:Iron 3081:and 3069:Yolk 2947:Fish 2914:Bird 2891:Eggs 2819:2013 2769:PMID 2640:ISBN 2613:ISBN 2280:PMID 2182:2016 1883:PMID 1743:ISBN 1630:ISSN 1526:ISBN 1470:ISBN 1217:gold 1181:sand 1131:The 1109:EDTA 1028:EDTA 406:1982 400:and 223:deer 135:AMNH 92:acid 49:eggs 3241:Tea 3201:Roe 2761:doi 2749:309 2725:doi 2713:332 2674:doi 2662:383 2272:doi 2260:266 2107:doi 1873:PMC 1863:doi 1822:doi 1712:doi 1622:doi 1219:or 1183:or 1113:gel 1026:or 517:in 503:cf. 471:), 412:at 227:elk 3415:: 2805:, 2775:. 2767:. 2759:. 2747:. 2743:. 2723:. 2711:. 2693:37 2691:. 2672:. 2660:. 2656:. 2638:, 2630:, 2570:^ 2549:^ 2537:^ 2521:^ 2475:^ 2457:^ 2425:^ 2404:^ 2374:^ 2362:^ 2348:^ 2336:^ 2286:. 2278:. 2270:. 2258:. 2201:^ 2167:54 2165:. 2161:. 2113:. 2105:. 2095:36 2093:. 1933:^ 1881:. 1871:. 1861:. 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Index


sauropod
Indroda Dinosaur and Fossil Park
dinosaur
England
eggs
reptiles
France
bird eggs
birds
American Museum of Natural History
Mongolia
thin section
microscope
CAT scans
acid
embryo
Massospondylus
Early Jurassic
Timeline of egg fossil research

Citipati
AMNH
Catholic priest
Jean-Jacques Pouech
serendipitously
American Museum of Natural History
early humans
Protoceratops
Oviraptor

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