問題一覧
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"Age of Reptiles"
Mesozoic Era
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was a pivotal period in the Earth's history that spanned approximately 252 to 66 million years ag
Mesozoic
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contributed to significant changes in atmospheric composition and global temperature, often leading to mass extinction events.
Volcanic Activity
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The Mesozoic Era was punctuated by periodic episodes of
Volcanic Activity
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led to the creation of diverse geological features,
Tectonic Activity
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the Siberian Traps eruptions during what extinction
Triassic - Jurassic
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Massive, Long-necked dinosaur
Sauropods
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Agile, Carnivorous Dinosaur
Theropods
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the first vertebrates to evolve true powered flight
Pterosaur
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occupied a range of ecological niches and played crucial roles in their respective ecosystems.
Pterosaurs
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First True Mammals
Morganucodon and Sinoconodon
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This contributed to the proliferation of lush, tropical environments that were well-suited for the flourishing of dinosaurs and other reptilian life forms.
Greenhouse Effect
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The Mesozoic Era was characterized by a prolonged "greenhouse" climate, with significantly higher levels of atmospheric _ and _compared to the present day.
Carbon Dioxide and Global Temperature
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The Mesozoic Era came to a dramatic end with the _ extinction event
Cretaceous - Paleogene
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(145-66 million years ago)
Cretaceous
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252 to 66 million years ago.
Mesozoic
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(252-201 million years ago)
Triassic
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(201-145 million years ago)
Jurassic
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saw the first appearance of dinosaurs and the rise of many other reptilian species.
Triassic Period
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witnessed the final chapter of the dinosaur era, including the emergence of feathered and avian dinosaurs
Cretaceous
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was marked by the dominance of large, iconic dinosaurs such as Tyrannosaurus rex and Brachiosaurus
Jurassic
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(252 million to 247 million years ago)
Early Triassic
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(about 247 million to 235 million years ago)
Middle Triassic
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(about 235 million to 201 million years ago)
Late Triassic
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consists of dolomite, shales or clay stones, and evaporites that were deposited during the middle and late Triassic epochs.
Keuper
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sequence of sedimentary rock strata, consists of limestone and dolomite beds and represents the marine part of the middle Triassic
Muschelkalk
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consists of sandstone layers of the lower Triassic series and is part of the Germanic Trias supergroup.
Bunter Buntsandstein
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have naked seeds, meaning they are not enclosed within a fruit.
Gymnosperms
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seed-bearing plants, were the dominant group of plants during the Triassic
Gymnosperms
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characterized by their needle-like or scale-like leaves and cone-bearing reproductive structures.
Conifers
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include trees such as Araucaria, Voltzia, and Walchia.
Conifers
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palm-like plants with large compound leaves and reproductive structures in the form of cones.
Cycads
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distinctive fan- shaped leaves and were likely an important part of the Triassic flora.
Ginkgoes
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(flowering plants)
Angiosperms
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Early forms of beetles, dragonflies, and other insect groups can be found in the Triassic fossil record.
Insects
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had segmented bodies, jointed appendages, and exoskeletons.
Crustacean
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sea scorpions
Eurypterid
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lizard-like appearance and diverse body forms. "stem reptiles,
Cotylosaurs
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They are often referred to as "mammal-like reptiles"
Therapsids
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were small and lizard-like in appearance.
Eosuchians
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They were characterized by their teeth being set in sockets (thecodont dentition), which is a feature shared with some modern reptiles and mammals
Thecondontians
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They were small to medium-sized reptiles with elongated bodies and long necks.
Protorosaurs
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THE GOLDEN AGE OF DINOSAURS
Jurassic
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derived from creta, Latin for “chalk,” and was first proposed by J.B.J. Omalius d’Halloy in 1822.
Cretaceous