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someone who studies "ancient organisms" |
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the study of ancient life |
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teh first proper name given to a dinosaur |
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Fossil fanatic
Founding fther of paleontology |
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40-foot sea monster
not a dinosaur, but a seaa going relative of todays monitor lizard (e.g. komodo dragon) |
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- studied giant sloth fossils from South America
- theorized that dinosaurs died long ago
- considered a genius, peple for the first time gave serious consideration that animals can and have gone extinct
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Reverend William Buckland |
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credited with describing the first scientifically valid dinosaur |
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- "big reptile"
- Buckland's dinosaur
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found the teeth and bones of an animal, Iguanadon |
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- named by Mantell
- first described herbivorous dinosaur
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tried to categorize the giant fossil animals of europe as scaled-up members of living reptile groups |
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scaly-skinned, terrestrialized animals, that lay hard-shelled eggs |
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- named by Sir Richard Owen
- "fearfully great reptiles"
Characterized as
- giant
- possessing upright stances
- non-aquatic
- having more than two sacral vertebrae(backbones fused in the hip region)
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include crocodillians and pterosuars(extinct flying reptiles) and dinosauromorphs(extinct dinosaur-like reptiles) |
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- (crocodiles, pterosaurs, dinosaurs, and other archosaurians such as "dinosauromorphs")
- teeth in socket: replaced throughout life
- hingelike ankles
- erect posture
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- three or more sacral vertebrae: fused backbones
- hands with three main fingers
- perforate acetabulae: the hole where the thighbone attached goes all the way through the hip
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- "bird hips"
- pelvic bones shaped like those of birds
- (e.g. Iguanadon)
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pelves like lizards
(e.g. Megalosaurus) |
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Othniel Charles Marsh and Edward Drinker Cope |
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the first person that we call a dinosaur paleobiologist |
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"terrible claw" a velociraptor like those in Jurassic Park |
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made dinosaur research popular again with crazy ideas |
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Mesozoic Era (238 million years ago) |
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Major divisions of the Mesozoic Era |
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- Triassic Period
- Jurassic Period
- Cretaceous Period
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- occurred 251-200 million years ago
- the oldest dinosaurs show up midway through this period
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this was the time of the very largest dinosaurs |
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the dinosaurs went extinct 65.4 million years ago at the end of the cretaceous period |
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Best isotopes for dating rocks |
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Potassium 40 which breaks down into Argon 40 |
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the amount of time it takes for half of the original material to break down |
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Climate at the time of dinosaurs |
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arid in equatorial regions (e.g. like florida)
Closer to the poles it was cool, wet and rainy (e.g. like Seattle) |
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One super continent during the triassic period |
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the continentsl movements are driven by the volcanic seafloor spreading in the oceans |
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suc as pine trees, conifers, cypress trees, cycads, ginkgo trees and others dominated the worldd's dryer ecosystems |
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showed up midway through the Cretaceous Period |
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32 foot long
"terror crocodiles" |
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reptiles that looked and swam like dolphins |
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- the supposed Loch Ness Monster
- bodies like sea turtles but necks long and snake-like
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- the animal Cuvier used in support of his extinction theory
- sea-going relatives of the living monitor lizard like the Komodo Dragon
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close relatives of dinosaurs with bat-like wings |
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largest known pterosaurs
had a 36-wing wingspan |
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- appeared in the late triassic period
- initially rat or weasl like and mouse to opossum sized
- remained so throughout the entire 173 million year tenure of the dinosaurs
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- "traces of ancient life"
- tracks, eggs, skin impressions
- gastroliths: stomach stones
- bite marks
- coprolites: fossilized feces
- the primary means by which paleontologists learn about dinosaur biology
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rocks formed from sandstones and shales including organic derivatives |
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rocks that form from volcanoes (such as ash tuffs) |
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sedimentary or igneous rocks that have been deformed by the pressures of the earth |
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places where rocks of these types are exposed and ideally where there is little vegetation so one can see lot of exposures |
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characterized by lizard-like hip bones
- includes meat-eaters like T-Rex and herbivorous long neck sauropod giants
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hips shaped like those of living birds
includes the herbivorous armored dinosaurs, the horned dinosaurs, the duck-bills, the bizarre head ramming pachycephalosaurus |
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Attributes of Ornithischia |
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- Bird-shaped hips
- a beak to crop plants
- a nutcracker jaw joint that allowed all teeth to come together at once and aided the processing of plants
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Sheild Bearers
Distiguishing features
- armor in their skins referred to as osteoderms
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Two major groups of thyreophora |
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Ankylosaurs: the dinosaur "tanks"
Stegosaurs: the "plated lizards" |
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Distinguishing Attribute of Stegosaurs |
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plates and spikes along or beside the backbone |
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"fused lizards"
quadrapedal, herbivorous |
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Diagnostic feature of ankylosaurs |
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an extensive armor extending over the sides of the body and neck |
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include the spike-thumbed iguanodonts, the duck bills, the bone heads, and the horned dinosaurs |
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Distinguishing Characteristics of the Cerapodans |
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Diastema: a gap between the front and back teeth |
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- gregarious: herding animals
- herbivorous
- bipedal or facultatively quadrapedal
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Distinguishing feature of Ornithopodans |
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front teeth well below the cheek teeth ( the gum line for the teeth at the front of the skull is at a different level than for the back teeth) |
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- early ornithopod group
- "different sized-teeth lizards"
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considerable size difference between the sexes of dinosaurs |
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Key features of advanced ornithopods |
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- criss crossed back and tail tendons
- forward forward prong on the pubis
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Diagnostic feature of extremely advanced ornithopods |
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flared out snout with no front teeth |
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extremely advanced ornithopods that did not have a grinding dentition but were unique in their possession of thumb spikes |
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- replaced the iguanodonts
- grinding dentitions
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- very broad, duck-like bills
- dental batteries composed of hundreds of tightly adjoining teeth
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naming more species than really exists |
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