| dc.creator | NIELSEN, Jan Kresten | |
| dc.creator | GÖRMÜŞ, Muhittin | |
| dc.creator | UYSAL, Kubilay | |
| dc.creator | Kanbur, Süheyla | |
| dc.date | 2012-04-30T21:00:00Z | |
| dc.date.accessioned | 2020-10-06T09:30:24Z | |
| dc.date.available | 2020-10-06T09:30:24Z | |
| dc.identifier | 22f16832-3f25-455a-9c06-178ac6d59402 | |
| dc.identifier | 10.3906/yer-1011-40 | |
| dc.identifier | https://avesis.sdu.edu.tr/publication/details/22f16832-3f25-455a-9c06-178ac6d59402/oai | |
| dc.identifier.uri | http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/55360 | |
| dc.description | The Guneyce Formation is well exposed in the Lake District of southwestern Turkey. It was deposited in the early Miocene in the Neotethys ocean and contains a large variety of trace fossils. The following ichnotaxa were recognized: Chondrites intricatus, C. targionii, ?Cosmorhaphe isp., Helminthopsis isp., Helminthorhaphe flexuosa, Lorenzinia isp., Naviculichnium marginatum, ?Nereites isp., Ophiomorpha rudis, ?Phycosiphon incertum, Planolites beverleyensis, cf. Rhizocorallium isp. and Thalassinoides suevicus. There is a lateral trend from proximal turbiditic successions to distal low-oxygen shaly mudstone. Ophiomorpha rudis ichnosubfacies, Paleodictyon ichnosubfacies of the Nereites ichnofacies and Zoophycos ichnofacies were identified. | |
| dc.language | eng | |
| dc.rights | info:eu-repo/semantics/closedAccess | |
| dc.title | Ichnology of the Miocene Guneyce Formation (Southwest Turkey): Oxygenation and Sedimentation Dynamics | |
| dc.type | info:eu-repo/semantics/article |
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