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The Late Devonian and Permian-Triassic intervals are among the most dynamic episodes of Earth history, marked by large secular changes;
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. The book includes chapters updating varied topics, like the Permian and Triassic chronostratigraphic scales, palaeogeographic reconstructions;
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; Ordovician - Mature stage of Caledonian and initial stage of development of Hercynian mobile belts; Silurian-Early Devonian. Completion;
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of the late Paleozoic - early Mesozoic and Cenozoic periods in North Vietnam. The Permian - Triassic and Paleogene volcano-plutonic and plutonic;
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of the late Paleozoic - early Mesozoic and Cenozoic periods in North Vietnam. The Permian - Triassic and Paleogene volcano-plutonic and plutonic;
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species of Triassic animals and plants, suggesting that faunal and floral changes already began in the Middle Triassic and were more protracted;
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The warm climate and floods of the Devonian period produced fishes, ammonoids, and reefs but it also accommodated two of the biggest mass;
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equatorial record, at the boundary between Tethys and Panthalassa. After the end-Permian extinction, ammonoids reached their first major diversity;
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paleoceanography, palynology, mammalian paleontology, and paleoanthropology-address the relationship between climatic and biotic evolution, presenting and;
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of the Paleozoic Era. These include the Cambrian; the early, mid-, and late Ordovician; the Silurian and Devonian with their numerous marine;
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the profound evolutionary consequences of the Late Devonian extinctions and the various theories proposed to explain their occurrence. Only;
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the profound evolutionary consequences of the Late Devonian extinctions and the various theories proposed to explain their occurrence. Only;
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Mesozoic, the Permian mass extinction, the late Paleozoic glaciation, and the origin of the first trees and land plants in the Devonian-Ordovician;
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interpretation of ancient dune fields and sand flats in fluvial basins in Buntsandstein (Lower Triassic), Rotliegend (Lower Permian) and Keuper (Upper;
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Based on two decades of research, The Late Devonian Mass Extinction reviews the many theories that have been presented to explain the;
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Based on two decades of research, The Late Devonian Mass Extinction reviews the many theories that have been presented to explain the;
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of Earth's earliest land life emerged from the water and stood poised to develop into mammal form, only to be obliterated during the PermianTriassic;
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of Earth's earliest land life emerged from the water and stood poised to develop into mammal form, only to be obliterated during the PermianTriassic;
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occurrences were recorded against a precisely controlled stratigraphical record in post-Lochkovian Devonian sediments * Includes 16 plates and 23 text;
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history, when the warmest climatic episode of the Cenozoic era occurred. This sudden global warming resulted in major turnovers among marine and;
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educators will find this book informative for understanding biotic and biogeochemical responses to changing climatic conditions. Scientists from a;
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comprehensive portrait of the effects of ancient climate change on global ecology. Carboniferous Giants and Mass Extinction examines the climatic;
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comprehensive portrait of the effects of ancient climate change on global ecology. Carboniferous Giants and Mass Extinction examines the climatic;
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and immediately after glacial episodes is paramount to accurate palaeoclimatic reconstructions and for our understanding of global climatic;
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Ice Age Earth provides the first detailed review of global environmental change in the Late Quaternary. Significant geological and climatic;
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Part of a monograph series on fossils The publication,New Middle and Late Anisian (Middle Triassic) Ammonoid Faunas from Northwestern;
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