FAS Astronomers Blog, Volume 31, Number 12.
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As you look around, you might notice that there are no dinosaurs, or at least what we think of as dinosaurs. The dinosaurs ruled the Earth for millions of years before disappearing some 66 million years ago.
What is a Dinosaur?
Dinosaurs are reptiles that lived in the distant past (for the most part). Okay, non-avian dinosaurs lived in the past. Avian (flying) dinosaurs are still with us today we know them as birds. Dinosaurs are distinguished from other reptiles by their hip structure (more on this below). They also have legs underneath their body, unlike other reptiles (e.g., lizards and alligators) with legs off to the side.
Setting the stage for Dinosaurs
The Earth is thought to be around 4 ½ billion years old. Its history (Geologic Time) is broken into four eons (Hadean, Archean, Proterozoic, and Phanerozoic). The first three are often combined into the Precambrian supereon. The last, the Phanerozoic eon, started 539 million years ago, and is divided into the Paleozoic, Mesozoic, and Cenozoic eras. It was during the Paleozoic era that life in the form of complex plants and animals took hold. Then, during the Mesozoic, along came the dinosaurs.
The evolution of vertebrates during the Paleozoic era laid the foundation for dinosaurs. The Paleozoic extended for over 250 million years from the Cambrian period through to the Permian period. Fish became dominant during the Devonian period and evolved into the first four-limbed tetrapods that crawled onto the land. Tetrapods known as amniotes split into mammal ancestors (synapsids) and reptile ancestors (sauropsids/diapsids). Some of these mammal ancestors, such as therapsids, came to dominate the landscape during the Permian period. Then the Permian-Triassic (P-T) extinction hit. This is called the Great Dying, when life nearly came to an end. The larger therapsids eventually disappeared, leaving only small cynodonts to carry on.
Life slowly recovered from the Great Dying during the Triassic period. Archosaurs (ruling reptiles) took over and dominated much of the Triassic. They eventually led to the first dinosaurs, flying pterosaurs, and crocodylomorphs (ancestors of crocodiles).
The dinosaurs first appeared around 230 million years ago during the middle Triassic. Herrerasaurus and Stautikosaurus were once thought to be examples of these early dinosaurs. However, Eoraptor was discovered in and may have slightly predated the others. More recently, the fossilized remains of Nyasasaurus were found to be around 243 million years old. However, Nyasasaurus may be a dinosauriform, a group of reptiles that immediately preceded the dinosaurs, rather than a true dinosaur itself.
The Age of Dinosaurs
With the Triassic-Jurassic extinction, the true age of dinosaurs began. The dinosaurs ruled the Earth for around 150 million years, but really dominated the landscape during the Jurassic and Cretaceous periods. Many of the large plant eating sauropods were found during the Jurassic period. Most of the large meat eating therapods came along later during the Cretaceous period.
The reign of dinosaurs (and the dinosaurs themselves) ended with the Cretaceous-Paleogene (K-Pg) extinction around 66 million years ago. The K-Pg extinction was caused by a 6- to 9-mile-wide asteroid that hit the Earth near the present-day town of Chicxulub, Mexico in the Yucatan peninsula.
After the demise of the dinosaurs, mammals, which had been small and insignificant, began to flourish during the Cenozoic era eventually leading to humans and the world we know today.
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Discovery of the Dinosaurs
No one knew anything about dinosaurs until the first half of the 19th century when two paleontologists discovered fossils associated with three unidentified animals.
In , Richard Owen (Owen ) noticed similarities among the three. He concluded that they were large lizard like reptiles, which he classified as Dinosauria (Dinosaurs) meaning fearfully great lizards (or terrible lizards per many of todays references). Soon it became clear that an entire group of extinct creatures roamed the Earth sometime in the distant past.
A few years later, Harry Seeley (Seeley ) divided dinosaurs into two distinct groups based on their hip structure (lizard hipped Saurischians and bird hipped Ornithischians).
The Bone Wars
The hunt for dinosaurs soon made its way to America. One of the first repositories of dinosaur fossils was found in New Jersey. Othniel Charles Marsh and Edward Drinker Cope decided to cooperate and share the findings from this site. Marsh then bribed someone at the site to bypass Cope and send all the fossils only to him. This began a competition that lasted for the rest of their lives and then some.
Cope was well off financially and had the means to support his fossil hunting. Marsh was not, but he had a rich uncle named George Peabody, who built the Yale Peabody Museum. Peabody appointed Marsh to run the museum and Marsh eventually inherited a great deal of wealth when Peabody passed away.
Fossil sites were soon discovered in the west during the building of the Transcontinental Railroad. So, around , Cope headed out there in search of new sources for dinosaur bones. At the same time, Marsh, who stayed back east, sent students to prospect for fossils in his place. Well, they didnt play nice. They spied on each other. They paid people off attempting to acquire all the fossils for themselves. They went so far as to steal fossils from each other.
Early on, Marsh made sure to criticize every published mistake Cope made, including one where Cope placed the skull of a dinosaur at the end of its tail. Later Cope, during a Congressional investigation into the U.S. Geological Survey (headed by Marsh), organized Marshs employees to testify against him. Their war found its way into the public arena when they began attacking each other with a series of articles in the New York Herald. Because of this, Marsh eventually had to resign his Geological Survey position. Later Cope became head of the National Association for the Advancement of Science but had to sell off much of his fossil collection due to financial problems.
It isnt clear who won the Bone Wars. Marsh (80) discovered more species than Cope (56) including well know dinosaurs such as Stegosaurus and Allosaurus. Some say they wouldnt have come close to these numbers if they had cooperated, although competition clearly didnt bring out the best in either of them. They both ended up spending much of their financial resources. But they generated publicity, captured peoples attention, and made dinosaurs popular with the general public. So, maybe the two individuals lost, but the public and paleontology won.
Before Richard Owen introduced the term Dinosauria in , there was no concept of anything even like a dinosaur. Large fossilized bones quite probably had been observed long before that time, but there is little recordand no existing specimensof such findings much before . In any case, people could not have been expected to understand what dinosaurs were even if they found their remains. For example, some classical scholars now conclude that the Greco-Roman legends of griffins from the 7th century bce were inspired by discoveries of protoceratopsian dinosaurs in the Altai region of Mongolia. In Robert Plot of the University of Oxford included, in a work of natural history, a drawing of what was apparently the knee-end of the thighbone of a dinosaur, which he thought might have come from an elephant taken to Britain in Roman times. Fossil bones of what were undoubtedly dinosaurs were discovered in New Jersey in the late s and were probably discussed at the meetings of the American Philosophical Society in Philadelphia. Soon thereafter, Lewis and Clarks expedition encountered dinosaur fossils in the western United States.
The earliest verifiable published record of dinosaur remains that still exists is a note in the American Journal of Science and Arts by Nathan Smith. The bones described had been found in by Solomon Ellsworth, Jr., while he was digging a well at his homestead in Windsor, Connecticut. At the time, the bones were thought to be human, but much later they were identified as Anchisaurus. Even earlier (), large birdlike footprints had been noticed on sandstone slabs in Massachusetts. Pliny Moody, who discovered these tracks, attributed them to Noahs raven, and Edward Hitchcock of Amherst College, who began collecting them in , considered them to be those of some giant extinct bird. The tracks are now recognized as having been made by several different kinds of dinosaurs, and such tracks are still commonplace in the Connecticut River valley today.
Better known are the finds in southern England during the early s by William Buckland (a clergyman) and Gideon Mantell (a physician), who described Megalosaurus and Iguanodon, respectively. In Buckland published a description of Megalosaurus, fossils of which consisted mainly of a lower jawbone with a few teeth. The following year Mantell published his Notice on the Iguanodon, a Newly Discovered Fossil Reptile, from the Sandstone of Tilgate Forest, in Sussex, on the basis of several teeth and some leg bones. Both men collected fossils as an avocation and are credited with the earliest published announcements in England of what later would be recognized as dinosaurs. In both cases their finds were too fragmentary to permit a clear image of either animal. In a partial skeleton was found near Brighton that corresponded with Mantells fragments from Tilgate Forest. It became known as the Maidstone Iguanodon, after the village where it was discovered. The Maidstone skeleton provided the first glimpse of what these creatures might have looked like.
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