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Titlebook: Biogeography, Time and Place: Distributions, Barriers and Islands; Willem Renema Book 2007 Springer Science+Business Media B.V. 2007 Biodi

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樓主: Encounter
41#
發(fā)表于 2025-3-28 18:19:57 | 只看該作者
978-90-481-7618-2Springer Science+Business Media B.V. 2007
42#
發(fā)表于 2025-3-28 21:45:27 | 只看該作者
43#
發(fā)表于 2025-3-29 00:17:21 | 只看該作者
44#
發(fā)表于 2025-3-29 06:51:22 | 只看該作者
https://doi.org/10.1007/978-3-319-43877-1ssed, with emphasis on the possible role of the break-up of Gondwana. All six families of butterflies (Hesperiidae, Papilionidae, Pieridae, Lycaenidae, Riodinidae, and Nymphalidae) and two families of wasps (Stephanidae and Braconidae) have been examined for obvious disjunct distributions. The evide
45#
發(fā)表于 2025-3-29 07:44:50 | 只看該作者
Kant’s Deduction , Apperceptiontarting in the Early Permian, or Middle Carboniferous (Odonata), making even the break-up of Gondwana (Late Jurassic) relevant to understanding present distributional patterns. The complex geological history of Southeast Asia is summarized, and geological area cladograms presented. Biogeographical s
46#
發(fā)表于 2025-3-29 13:03:53 | 只看該作者
47#
發(fā)表于 2025-3-29 17:21:28 | 只看該作者
A Working Model for Transcendental Argumentsudied. The interplay between the biological characteristics of the shrimps in the Atlantic/East Pacifi c area resulted in a biogeographical pattern best explained by a series of vicariance events. Distributional pattern in the Indo-West Pacifi c shows a centre of maximum diversity in eastern Indones
48#
發(fā)表于 2025-3-29 23:18:48 | 只看該作者
https://doi.org/10.1007/978-94-009-9700-4is centre includes Malaysia, the Philippines, Indonesia, and Papua New Guinea, it has been named the East Indies Triangle. Due to its dependence on the presence of coral reefs, it has recently been referred to as the Coral Triangle. Because these reefs are severely threatened by human activities, la
49#
發(fā)表于 2025-3-30 02:10:57 | 只看該作者
50#
發(fā)表于 2025-3-30 06:48:09 | 只看該作者
A Working Model for Transcendental Arguments Spain) during the Carboniferous is discussed, with an emphasis on the tectonically active Pennsylvanian (i.e., Late Carboniferous). The reef-bearing Valdeteja, San Emiliano, and Cuera formations are briefly described, and their brachiopod faunas are discussed with special emphasis on adaptations to
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