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	<Article> 

	<Journal> 

	<PublisherName>International Science Community Association</PublisherName>

	<JournalTitle>International Research Journal of Biological Sciences</JournalTitle> 

	<Issn>2278 - 3202</Issn>

	<Volume>5</Volume>

	<Issue>9</Issue>

	<PubDate PubStatus="ppublish"> 

	<Year>2016</Year> 

	<Month>09</Month> 

	<Day>10</Day> 

	</PubDate>

	</Journal>



	<ArticleTitle>Plant Remains from the Holocene of Sheikh El-Obeiyid Area (Farafra Oasis, Egypt), 7730-5360 b.p.</ArticleTitle> 


	<FirstPage>22</FirstPage>

	<LastPage>31</LastPage>



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	<Language>EN</Language> 
	<AuthorList>

	
		<Author> 

		<FirstName>Subhadra</FirstName>

		<MiddleName> </MiddleName>

		<LastName>Subhadarsini</LastName>

		<Suffix>1</Suffix>

		<Affiliation>P.G. Department of Botany, Utkal University, Vani vihar, Bhubaneswar, Odisha, India</Affiliation>

		</Author>
		<Author> 

		<FirstName>Sandeep Kumar</FirstName>

		<MiddleName> </MiddleName>

		<LastName>Nayak</LastName>

		<Suffix>2</Suffix>

		<Affiliation> P.G. Department of Botany, Utkal University, Vani vihar, Bhubaneswar, Odisha, India</Affiliation>

		</Author>
		<Author> 

		<FirstName>Kunja Bihari </FirstName>

		<MiddleName> </MiddleName>

		<LastName>Satapathy*</LastName>

		<Suffix>3</Suffix>

		<Affiliation> P.G. Department of Botany, Utkal University, Vani vihar, Bhubaneswar, Odisha, India</Affiliation>

		</Author>
		<Author> 

		<FirstName>M. </FirstName>

		<MiddleName> </MiddleName>

		<LastName>Udayakumar </LastName>

		<Suffix>1</Suffix>

		<Affiliation> Department of Botany, Pachaiyappa’s College, Chennai – 600 030, Tamil Nadu, India</Affiliation>

		</Author>
		<Author> 

		<FirstName>T.* </FirstName>

		<MiddleName> </MiddleName>

		<LastName>Sekar</LastName>

		<Suffix>2</Suffix>

		<Affiliation> Department of Botany, Pachaiyappa’s College, Chennai – 600 030, Tamil Nadu, India</Affiliation>

		</Author>
		<Author> 

		<FirstName>Analyn*</FirstName>

		<MiddleName> </MiddleName>

		<LastName> Anzano Cabras* </LastName>

		<Suffix>1</Suffix>

		<Affiliation>College of Arts and Sciences, University of Mindanao, Davao City, Philippines</Affiliation>

		</Author>
		<Author> 

		<FirstName>Jürgen </FirstName>

		<MiddleName> </MiddleName>

		<LastName>Wiesner</LastName>

		<Suffix>2</Suffix>

		<Affiliation>Dresdener Ring 11, D-38444 Wolfsburg, Germany</Affiliation>

		</Author>
		<Author> 

		<FirstName>Mohamed </FirstName>

		<MiddleName> </MiddleName>

		<LastName> Ahmed Fadl</LastName>

		<Suffix>1</Suffix>

		<Affiliation> Botany and Microbiology Department, Faculty of Science, Beni-Suef University, Beni-Suef, Egypt and Biology Department, Faculty of Science, Taif University, Taif, KSA</Affiliation>

		</Author>

	<Author>

	<CollectiveName></CollectiveName>>

	</Author>

	</AuthorList>


	<PublicationType>Research Article</PublicationType>


	<History>  
	<PubDate PubStatus="received">
	<Year>2016</Year>
	<Month>8</Month>
	<Day>29</Day>
	</PubDate>
	<PubDate PubStatus="accepted">										
	<Year>2016</Year> 
	<Month>09</Month>									
	<Day>10</Day> 
	</PubDate>

	</History>
	<Abstract>Egypt is a hyperarid region of the Eastern Sahara of Africa, the oases of the Western Desert form green patches. In the Holocene of Farafra Oasis (7730-5360b.p.) humid climate with dense vegetation and herding animals were recorded. Archaeobotanical and Archaeological evidences of the Sheikh El-Obeiyid area in the westnorth of Farafra Oasis, three active occupation periods in Sheikh El-Obeiyid Neolithic site were identified, the first period extended from 7530–6166 b.p. in El-Bahr Playa, and the second period extended from 6320–6170 b.p. in Valley 1 and Bir El-Obeiyid Playa and the third period from 5790–5360 b.p. in Valley 1 and Valley 3. Identified plant species indicated a moist conditions of small lakes with their surrounding Tamarix nilotica, Juncus sp., Cyperus sp, and Samolus valerandii; in the Wadi El-Obeiyid and its tributaries Acacia, Tamarix aphylla and Ficus trees forms a desert savanna vegetation. The recorded types of vegetation proved that there are obvious effects of monsoon summer and Mediterranean winter climate on the vegetation of the Holocene in Sheikh El-Obeiyid area. There is a similarity of archaeological features between the Sheikh El-Obeiyid and the nearby Hidden Valley basin, both of them were active in the seventh millennium b.p.</Abstract>

	<CopyrightInformation>Copyright@ International Science Community Association</CopyrightInformation>

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