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<Article>
<Journal>
<PublisherName>OICC Press</PublisherName>
<JournalTitle>Geoconservation Research</JournalTitle>
<Issn>2588-7343</Issn>
<Volume>2</Volume>
<Issue>1</Issue>
<PubDate PubStatus="epublish">
<Year>2019</Year>
<Month>12</Month>
<Day>01</Day>
</PubDate>
</Journal>
<ArticleTitle>‘Canaralele din Portul Hârșova’- The paleontological importance of the most complete Oxfordian geosite in Central Dobrogea, Romania</ArticleTitle>
<VernacularTitle></VernacularTitle>
<FirstPage></FirstPage>
<LastPage></LastPage>
<ELocationID EIdType="doi">10.30486/gcr.2019.1878598.1014</ELocationID>
<Language>EN</Language>
<AuthorList>
<Author>
<FirstName>Delia-Georgeta</FirstName>
<LastName>Dumitraş</LastName>
<Affiliation>Geological Institute of Romania, 1st Caransebeş Street, Sector 1, 012271, Bucharest, Romania</Affiliation>
<Identifier Source="ORCID">https://orcid.org/0000-0001-9447-4183</Identifier>
</Author>
<Author>
<FirstName>Dan </FirstName>
<LastName>Grigore</LastName>
<Affiliation>Geological Institute of Romania, 1st Caransebeş Street, Sector 1, 012271, Bucharest, Romania</Affiliation>
<Identifier Source="ORCID"></Identifier>
</Author>
<Author>
<FirstName>Diana</FirstName>
<LastName>Perşa</LastName>
<Affiliation>Geological Institute of Romania, 1st Caransebeş Street, Sector 1, 012271, Bucharest, Romania</Affiliation>
<Identifier Source="ORCID"></Identifier>
</Author>
<Author>
<FirstName>Mohamed</FirstName>
<LastName>Abioui</LastName>
<Affiliation>Geology Department, Faculty of Sciences, Ibn Zohr University, Agadir, Morocco</Affiliation>
<Identifier Source="ORCID">0000-0002-6331-1442</Identifier>
</Author>
</AuthorList>
<PublicationType>Journal Article</PublicationType>
<History>
<PubDate PubStatus="received">
<Year>2019</Year>
<Month>12</Month>
<Day>01</Day>
</PubDate>
</History>
<Abstract>âCanaralele din Portul HÃ¢rÈovaâ geosite is integrated into âCanaralele Dunariiâ Natura 2000 site (ROSCI0022), and represents the northern part of the geologic profile in Jurassic deposits that is exposed along the Danube River valley between HÃ¢rÈova and Capidava. This sector exhibits Middle and Upper Jurassic deposits, developed in biohermal (in situ spongalgal, coralgal reefs and stromatolits) and biostromal facies. All around HÃ¢rÈova, on the right bank of the Danube, the landscape is dominated by ruiniform shapes of this spongalgal limestones, formed through differential dissolution. The Callovian and Oxfordian fossil fauna contents are of biostratigrafic and paleoecological importance.</Abstract>
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<Param Name="value">Bioherm</Param>
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<Object Type="keyword">
<Param Name="value">Biostratigraphy.</Param>
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<Object Type="keyword">
<Param Name="value">Canarale</Param>
</Object>
<Object Type="keyword">
<Param Name="value">Fossils</Param>
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<Object Type="keyword">
<Param Name="value">Geosite</Param>
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</Article>
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