Titlebook: Recent Landform Evolution; The Carpatho-Balkan- Dénes Lóczy,Milo? Stankoviansky,Adam Kotarba Book 2012 Springer Science+Business Media B.V.

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書目名稱Recent Landform Evolution影響因子(影響力)




書目名稱Recent Landform Evolution影響因子(影響力)學科排名




書目名稱Recent Landform Evolution網(wǎng)絡公開度




書目名稱Recent Landform Evolution網(wǎng)絡公開度學科排名




書目名稱Recent Landform Evolution被引頻次




書目名稱Recent Landform Evolution被引頻次學科排名




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書目名稱Recent Landform Evolution年度引用學科排名




書目名稱Recent Landform Evolution讀者反饋




書目名稱Recent Landform Evolution讀者反饋學科排名

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Book 2012Group, promote networking between researchers and the exchange of research experience.?Following a brief introduction into the geology, climate, hydrology and land cover of the Carpatho-Balkan-Dinaric region, the book provides detailed information on research applying both traditional and innovative

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Ivan Kovalchuk,Yaroslav Kravchuk,Andriy Mykhnovych,Olha Pylypovychnary biology as well as in general invertebrate zoology..This second volume on ecdysozoans covers all animals commonly known as crustaceans. While “Crustacea” is currently n978-3-7091-1995-2978-3-7091-1853-5

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olutionary constrains during mid-embryogenesis compared with the less conserved early and late stages. These constraints may relate to morphological events, and/or the underlying gene regulatory networks, at the different stages of embryogenesis, as well as the requirement for embryogenesis to produ

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ance of mating among populations. This cessation of gene flow, coupled with further evolutionary change, could lead to the formation of nascent species. There is, then, a direct potential connection between local coadaptation of populations, speciation, and macroevolutionary diversification. Some of

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Ján Feranec,Tomá? Soukupkish, and marine environments. More than 15,000 fossil species that trace their origins back to the Ordovician period approximately 483 million years ago have been described. This period of origin is much later than that of many other animal phyla that arose during or before the Cambrian. Although o