Results 141 to 150 of about 1,109 (180)

Checklist of hosts, illustrated geographical range, and ecology of tick species from the genus Ixodes (Acari, Ixodidae) in Russia and other post-Soviet countries. [PDF]

Zookeys
Fedorov D, Hornok S.
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Delimitation of the widely distributed Palearctic Stenodema species (Hemiptera, Heteroptera, Miridae): insights from molecular and morphological data. [PDF]

Zookeys
Namyatova AA, Dzhelali PA, Konstantinov FV.   +2 more
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Annotated Checklist of Poroid Hymenochaetoid Fungi in Central Asia: Taxonomic Diversity, Ecological Roles, and Potential Distribution Patterns. [PDF]

J Fungi (Basel)
Gafforov Y, Yarasheva M, Wang XW, Rašeta M, Rakhimova Y, Kyzmetova L, Bavlankulova K, Rapior S, Chen JJ, Langer E, Munnavarov B, Aslonov Z, Bakokhoja B, Zhou LW.   +13 more
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Lithofacies and microbiofacies of the Upper Cretaceous rocks 〈Sadr unit〉 of Nakhlak area in Nottheastern NainCentral lran [PDF]

Kohansal, Ghadimvand Nader, Senowbari-Daryan, Baba, Vaziri, Seyed Hamid   +2 more
core  

Habitat potential modelling and the effect of climate change on the current and future distribution of three Thymus species in Iran using MaxEnt. [PDF]

Sci Rep
Hosseini N, Ghorbanpour M, Mostafavi H.
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DEPOSITIONAL HISTORY AND PALEOGEOGRAPHY OF THE LOWER PALEOCENE REDBEDS IN EASTERN KOPET-DAGH BASIN NORTHEASTERN IRAN [PDF]

Journal of Sciences, Islamic Republic of Iran, 1993
doaj  

Evolutionary history of an Irano-Turanian cushion-forming legume (Onobrychis cornuta). [PDF]

BMC Plant Biol
Tayebi Z, Moghaddam M, Mahmoodi M, Kazempour-Osaloo S.   +3 more
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Population status, habitat preferences and predictive current and future distributions of three endangered Silene species under changing climate. [PDF]

Front Plant Sci
Abdelaal M, Al-Huqail AA, Alghanem SMS, Alhaithloul HAS, Al-Robai SA, Abeed AHA, Dakhil MA, El-Barougy RF, Yahia AA.   +8 more
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Lower Cretaceous (Upper Barremian-Lower Albian) ammonite faunas of the Kopet Dagh Basin, NE Iran

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Kopet-Dagh Basin Evolution During Middle-late Jurassic

Proceedings, 2009
In this paper with the help of latest available data including field, well and seismic data, palaeoenvironments and depositional sequences of Kashafrud, Chaman Bid and Mozduran formations constructed in order to determine the basin evolution of the Kopet-Dagh during Middle-Late Jurassic.
M.A. Kavoosi, M. Sepehr, S. Sherkati
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