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Titlebook: Mass Extinction; Ashraf M.T. Elewa Book 2008 Springer-Verlag Berlin Heidelberg 2008 Devonian.Ice Age.Ordovician.Permian.Silurian.Triassic.

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發(fā)表于 2025-3-21 19:09:19 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱Mass Extinction
編輯Ashraf M.T. Elewa
視頻videohttp://file.papertrans.cn/626/625231/625231.mp4
概述Includes supplementary material:
圖書(shū)封面Titlebook: Mass Extinction;  Ashraf M.T. Elewa Book 2008 Springer-Verlag Berlin Heidelberg 2008 Devonian.Ice Age.Ordovician.Permian.Silurian.Triassic.
描述P. David Polly Department of Geological Sciences, Indiana University, Bloomington, IN 47405, USA, pdpolly@indiana.edu Only 200 years ago, extinction was a radical new idea. Fossils were known, but their identity as the remains of species that no longer lived on the face of the Earth was not yet firmly established in the scientific world. Arguments that these organic-looking objects from the rocks were merely bizarre mineralizations or that they were the remains of species still living th in unexplored regions of the world had dominated 18 Century interpretations of fossils. But the settling of North America and other colonial expeditions by Europeans were quickly making the world smaller. In 1796 Cuvier painstakingly demonstrated that the anatomy of the mastodon skeleton from Big Bone Lick in Kentucky could not possibly belong to a modern elephant, unlike the mammoth fossils found in Europe, which are so similar to the living African Elephant that many found plausible the explanation that they were bones of animals used by the Roman army. Any doubt that Cuvier’s mastodon still lived in the wilds of the western North American interior was crushed ten years later when the Lewis and C
出版日期Book 2008
關(guān)鍵詞Devonian; Ice Age; Ordovician; Permian; Silurian; Triassic; current mass extinction; desert; ecology; insects
版次1
doihttps://doi.org/10.1007/978-3-540-75916-4
isbn_softcover978-3-642-09504-7
isbn_ebook978-3-540-75916-4
copyrightSpringer-Verlag Berlin Heidelberg 2008
The information of publication is updating

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書(shū)目名稱Mass Extinction影響因子(影響力)學(xué)科排名




書(shū)目名稱Mass Extinction網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱Mass Extinction網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱Mass Extinction被引頻次




書(shū)目名稱Mass Extinction被引頻次學(xué)科排名




書(shū)目名稱Mass Extinction年度引用




書(shū)目名稱Mass Extinction年度引用學(xué)科排名




書(shū)目名稱Mass Extinction讀者反饋




書(shū)目名稱Mass Extinction讀者反饋學(xué)科排名




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ndiana.edu Only 200 years ago, extinction was a radical new idea. Fossils were known, but their identity as the remains of species that no longer lived on the face of the Earth was not yet firmly established in the scientific world. Arguments that these organic-looking objects from the rocks were me
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he nuclei 19F and 15N, subvolume III/35C contains the nucleus 1H, subvolume III/35D contains the nucleus 13C, subvolume III/35E contains the nucleus 17O, andsubvolume III/35G contains the nucleus 77Se. More nuclei will be presented later..978-3-540-31642-8Series ISSN 1615-1844 Series E-ISSN 1616-9522
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Mikael Calnerhe nuclei 19F and 15N, subvolume III/35C contains the nucleus 1H, subvolume III/35D contains the nucleus 13C, subvolume III/35E contains the nucleus 17O, andsubvolume III/35G contains the nucleus 77Se. More nuclei will be presented later..978-3-540-31642-8Series ISSN 1615-1844 Series E-ISSN 1616-9522
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Ashraf M. T. Elewahe nuclei 19F and 15N, subvolume III/35C contains the nucleus 1H, subvolume III/35D contains the nucleus 13C, subvolume III/35E contains the nucleus 17O, andsubvolume III/35G contains the nucleus 77Se. More nuclei will be presented later..978-3-540-31642-8Series ISSN 1615-1844 Series E-ISSN 1616-9522
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