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・ Mesotype
・ Mesotype didymata
・ Mesotype parallelolineata
・ Mesotype verberata
・ Mesovarium
・ Mesovortices
・ Mesovouni
・ Mesovouni, Karditsa
・ Mesovouno
・ Mesovouno massacres
・ Mesowear
・ Mesowest
・ Mesoxalic acid
・ Mesoxantha
・ Mesozoa
Mesozoic
・ Mesozoic mammals of Madagascar
・ Mesozoic Marine Revolution
・ Mesozoic–Cenozoic Radiation
・ Mesozygiella dunlopi
・ MESP1
・ MESP2
・ Mespaul
・ Mespeatches
・ Mespelbrunn
・ Mespelbrunn Castle
・ Mespil
・ Mespilus
・ Mespilus canescens
・ Mespilus germanica


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Mesozoic : ウィキペディア英語版
Mesozoic

The Mesozoic Era is an interval of geological time from about . It is also called the Age of Reptiles, a phrase introduced by the 19th century paleontologist Gideon Mantell who viewed it as dominated by reptiles such as ''Iguanodon'', ''Megalosaurus'', ''Plesiosaurus'' and what are now called Pseudosuchia.
''Mesozoic'' means "middle life", deriving from the Greek prefix ''meso-''/''μεσο-'' for "between" and ''zōon''/''ζῷον'' meaning "animal" or "living being".〔(【引用サイトリンク】url=http://www.etymonline.com/index.php?term=Mesozoic&allowed_in_frame=0 )〕 It is one of three geologic eras of the Phanerozoic Eon, preceded by the Paleozoic ("ancient life") and succeeded by the Cenozoic ("new life"). The era is subdivided into three major periods: the Triassic, Jurassic, and Cretaceous, which are further subdivided into a number of epochs and stages.
The era began in the wake of the Permian–Triassic extinction event, the largest well-documented mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction which is known for having killed off non-avian dinosaurs, as well as other plant and animal species. The Mesozoic was a time of significant tectonic, climate and evolutionary activity. The era witnessed the gradual rifting of the supercontinent Pangaea into separate landmasses that would eventually move into their current positions. The climate of the Mesozoic was varied, alternating between warming and cooling periods. Overall, however, the Earth was hotter than it is today. Non-avian dinosaurs appeared in the Late Triassic and became the dominant terrestrial vertebrates early in the Jurassic, occupying this position for about 135 million years until their demise at the end of the Cretaceous. Birds first appeared in the Jurassic, having evolved from a branch of theropod dinosaurs. The first mammals also appeared during the Mesozoic, but would remain small—less than 15 kg (33 lb)—until the Cenozoic.
==Geologic periods==
Following the Paleozoic, the Mesozoic extended roughly 186 million years, from when the Cenozoic Era began. This time frame is separated into three geologic periods. From oldest to youngest:
* Triassic ()
* Jurassic ()
* Cretaceous ()
The lower (Triassic) boundary is set by the Permian–Triassic extinction event, during which approximately 90% to 96% of marine species and 70% of terrestrial vertebrates became extinct. It is also known as the "Great Dying" because it is considered the largest mass extinction in the Earth's history. The upper (Cretaceous) boundary is set at the Cretaceous–Tertiary (KT) extinction event (now more accurately called the Cretaceous–Paleogene (or K–Pg) extinction event), which may have been caused by the impactor that created Chicxulub Crater on the Yucatán Peninsula. Towards the Late Cretaceous large volcanic eruptions are also believed to have contributed to the Cretaceous–Paleogene extinction event. Approximately 50% of all genera became extinct, including all of the non-avian dinosaurs.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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