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Etymologies
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Examples
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However, during different geological periods a number of other phytogeographical elements have penetrated the area, such as Irano-Turanian, Central European, West European, West Mediterranean and South Mediterranean.
Aegean and Western Turkey sclerophyllous and mixed forests 2008
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However, the structure's designation was later changed to the more Irano-Islamic sounding chihil sutun, literally the palace of forty pillars.
Connecting Histories in Afghanistan: Market Relations and State Formation on a Colonial Frontier 2008
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The overlapping of the Mediterranean and Irano-Turanian floristic zones here has also contributed to the evolution of unique species.
Southern Anatolian montane conifer and deciduous forests 2008
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It also includes areas of saltland vegetation enclosed within this zone (Zohary 1973), including: littoral saltland vegetation of Salicornietea europaeae, falling primarily in the northern part of this ecoregion; the Irano-Turanian saltland vegetation of Halocnemetea strobilacei; and the Saharo-Arabian saltland vegetation of Suadetea deserta.
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Due in large part to the influence of the Irano-Turanian phytogeographic realm, this ecoregion is rich in herbaceous plants and has a high proportion (30 %) of endemic species, the most in any Mediterranean region.
Southern Anatolian montane conifer and deciduous forests 2008
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In the southern reaches, this hotspot integrades with the Irano-Anatolian Hotspot.
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The lower slopes of Takhatu, Zarghun, Wam-Pilghar, and Toba Kakar, between 2,000 and 3,300 m, have dry alpine steppe 'of Irano-Turanian affinities.
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Smaller scattered areas of Irano-Turanian psammophilous vegetation, with Haloxylon persicum and Stipagrostis pennata (Zohary, 1973), are also included.
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Due to a drier climate and higher temperatures, and since it is highly affected by the Irano-Turanian phytogeographic realm, the southern maquis formation has many deciduous species.
Eastern Mediterranean conifer-sclerophyllous-broadleaf forests 2008
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In spring and autumn, the hot and dusty "khamsin" wind, blowing from the east and southeast, may cause temperatures to rise as high as 43-49 degrees C. Vegetation is reflective of the Mesopotamian province of the Irano-Turanian region.
Middle East steppe 2008
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