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Titlebook: Biogeography and Ecology of Turkmenistan; Victor Fet,Khabibulla I. Atamuradov Book 1994 Springer Science+Business Media Dordrecht 1994 Fau

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發(fā)表于 2025-3-21 18:24:17 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱Biogeography and Ecology of Turkmenistan
影響因子2023Victor Fet,Khabibulla I. Atamuradov
視頻videohttp://file.papertrans.cn/188/187067/187067.mp4
學(xué)科分類Monographiae Biologicae
圖書封面Titlebook: Biogeography and Ecology of Turkmenistan;  Victor Fet,Khabibulla I. Atamuradov Book 1994 Springer Science+Business Media Dordrecht 1994 Fau
影響因子remnants of gene pools of these species. Badghyz Natural Reserve, established in 1941, became a refuge for the last existing population of the Turkmen onager (Equus hemionus onager) and a unique pistachio woodland. A new generation oflocal Turkmen scientists, many of whom were trained by the Russian researchers in the graduate schools of Moscow and Leningrad arose from the 1930s through the 1950s. The Turkmen Academy of Sciences and its journal, Proceedings (including the monthly biological series), served to record the results of diverse biological studies in the republic. While basic science in the Middle Asian republics rather gained from the Russian "colonial" influence, natural resources, in contrast, were severely damaged by the Soviet way of handling the economy and social issues. Severe environmental problems have been inherited by the now independent Turkmenistan, including overgrazed desert pastures, deforested mountains, depleted water resources, accumulated pesticides in cotton fields, declining populations of endangered species of animals and plants, and - worst of al- progressing, human-caused desertification (Kharin this volume). In order to approach a solution to th
Pindex Book 1994
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發(fā)表于 2025-3-21 23:46:19 | 只看該作者
Landscapes of Turkmenistan,h their northern submontane plain, the isolated Bolshoi Balkhan and Maly Balkhan Mountains, the Ustyurt Plateau (its part within Turkmenistan), the Krasnovodsk Peninsula, the Cis-Caspian Lowland, western sands of Chilmamed and Uchtagan, the Sarykamysh-Khwarazm Lowland, the Uzboi dry valley, the Kara
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Climate of Turkmenistan,elements throughout the republic of Turkmenistan, and climatic features of seasonality. Turkmenistan has a very continental and exceptionally dry climate. It is determined by the low latitude position of this area, its significant distance from the oceans, features of atmospheric circulation, charac
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Paleogeography of Turkmenistan,ota. In the Cretaceous, climate become more differentiated; seasonal temperature changes and latitudinal zonality of vegetation appeared; and the desert climatic regime was established. In the Paleogene, the remnants of the Tethys Sea covered only the lowest portions of lowlands; in the early Eocene
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發(fā)表于 2025-3-22 11:46:45 | 只看該作者
Desertification of the Arid Lands of Turkmenistan,criteria of desertification characterizing this process can include, e.g., data on species composition, vegetation, and productivity in specific plant communities. Such criteria were used for map construction, including the desertification map of Turkmenistan on the scale 1:4,000,000. The basic type
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Flora of Kopetdagh, dicotyledons. A prominent position in this flora is occupied by the typical Ancient Mediterranean families of Asteraceae, Poaceae, Fabaceae, Brassicaceae, and Chenopodiaceae. The desert and low arid mountain character of the flora is expressed by the diversity of Chenopodiaceae, Brassicaceae, and B
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Trees, Shrubs, and Semishrubs in the Mountains of Turkmenistan,ished forest and savannoid communities and transformed them into sparse xerophitic woodlands. In the historical period, the anthropogenic factor has increasingly affected vegetation, especially woodlands comprised of junipers . and pistachio . Structure and current condition of these woodlands are d
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