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Titlebook: Extinction Events in Earth History; Proceedings of the P Erle G. Kauffman,Otto H. Walliser Conference proceedings 1990 Springer-Verlag Berl

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發(fā)表于 2025-3-21 18:03:37 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Extinction Events in Earth History
副標(biāo)題Proceedings of the P
編輯Erle G. Kauffman,Otto H. Walliser
視頻videohttp://file.papertrans.cn/320/319917/319917.mp4
叢書名稱Lecture Notes in Earth Sciences
圖書封面Titlebook: Extinction Events in Earth History; Proceedings of the P Erle G. Kauffman,Otto H. Walliser Conference proceedings 1990 Springer-Verlag Berl
描述This volume is dedicated to the interdisciplinary study of dynamic biological changes through the Phanerozoic which are associated with mass extinction events and similar biotic crises, and their causal mechanisms. In particular, it documents in detail the complex nature of terrestrial and extraterrestrial feedback loops that are associated with many mass extinction intervals. Authors have been asked to represent most of the known mass extinction events through time, and to comment on the complex earthbound or extraterrestrial causes (or both) for global biotic crises. The reader is offered new perspectives of extinction boundaries, a more innovative and diverse approach to causal mechanisms and mass extinction theory, blended views of paleobiologists, oceanographers, geochemists, volcanologists, and sedimentologists by an international cast of authors. No other book on extinction presents such a broad spectrum of data and theories on the subject of mass extinction.
出版日期Conference proceedings 1990
關(guān)鍵詞Mass extinction; Massenaussterben; Oxide; Sediment; Trias; biological events; biologische Krisen; evolution
版次1
doihttps://doi.org/10.1007/BFb0011129
isbn_softcover978-3-540-52605-6
isbn_ebook978-3-540-47071-7Series ISSN 0930-0317 Series E-ISSN 1613-2580
issn_series 0930-0317
copyrightSpringer-Verlag Berlin Heidelberg 1990
The information of publication is updating

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發(fā)表于 2025-3-21 21:54:52 | 只看該作者
Biological selectivity of extinction,ion of causality. Heritable differences in characters may have predictable consequences in terms of differential species survival. Differences in magnitude and intensity of extinction are insufficient to distinguish background from mass extinction regimes. Biological adaptations may establish links
板凳
發(fā)表于 2025-3-22 03:48:16 | 只看該作者
地板
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Shock pressures in igneous processes: Implications for K/T events,sure of about 500 kbar. Such pressures fall off with distance from the magma chamber although jointing, fractures, etc. may act as stress concentrators to extend the radius of formation of shocked minerals as far as a kilometer. Shocked minerals are not to be expected from the magma itself as high t
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發(fā)表于 2025-3-22 11:58:58 | 只看該作者
Vertical advection from oxic or anoxic water from the main pycnocline as a cause of rapid extinction based on photosynthesis. Waters from the main pycnocline (100–1000 m) or deeper naturally contain decay products from sinking organic matter as a function of the oxidation state of the waters. Such products, in proper concentrations, can inhibit photosynthetic growth or are toxic or debilitating t
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發(fā)表于 2025-3-22 13:15:18 | 只看該作者
Evolutionary crisis within the Ordovician acrotretid inarticulate brachiopods of Poland,pt for three genera of the . line going up to the Silurian and of the . line going on to the Lower Devonian. In Poland, acrotretids are very diversified in Ordovician, especially in the Lower Ordovician/Upper Tremadocian-Llanvirnian), similarly as e.g. in Balto-Scandia (Sweden, Estonia, Leningrad en
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發(fā)表于 2025-3-22 21:13:37 | 只看該作者
Silurian and pre-Upper Devonian bio-events,ble with shelly benthos are bio-events in the C.–C. interval of the Upper Llandovery, in the early Wenlock, late Wenlock, late Ludlow, Silurian-Devonian boundary, near the base of the Emsian, near the end of the Eifelian, and near the end of the Givetian. The last two coincide in time with what may
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發(fā)表于 2025-3-23 09:12:33 | 只看該作者
The Middle Givetian ,-Events a tool for high time resolution and event-stratigraphical correlation,rica. Their exceptional character is not only based on the mass occurrence of “.” . (a small brachiopod), but also on additional biofacial and special sedimentological features. Due to their synchronous, extremely short-term deposition the . Horizons are excellent index horizons for a basin-wide cor
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