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Dergiler / Turkish Journal of Earth Sciences / 2012 / Cilt: 21 - Sayı: 3

Ichnology of the Miocene Güneyce Formation (Southwest Turkey): Oxygenation and Sedimentation Dynamics

JAN KRESTEN NIELSEN
MUHİTTİN GÖRMÜŞ
KUBİLAY UYSAL & SÜVEYLA KANBUR
Süveyla KANBUR
Sayfa
391–405
Yayın Tarihi
2012-03-01
DOI
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⚡ TL;DR(1 Cümlede Hızlı Çıkarım)

Ophiomorpha rudis ichnosubfacies, Paleodictyon ichnosubfacies of the Nereites ichnofacies and Zoophycos ichnofacies were identified.

📌 3 Maddede Bu Makale

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Amaç & Hipotez:The Güneyce Formation is well exposed in the Lake District of southwestern Turkey.
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Temel Bulgular & Veri:It was deposited in the early Miocene in the Neotethys ocean and contains a large variety of trace fossils.
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Sonuç & Katkı:Ophiomorpha rudis ichnosubfacies, Paleodictyon ichnosubfacies of the Nereites ichnofacies and Zoophycos ichnofacies were identified.
🔬Tür:Araştırma Makalesi
📍Kapsam:Genişletilmiş Akademik Örneklem
⚙️Değişkenler:trace fossils · turbidites · ichnofacies

Özet

The Güneyce 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.

Abstract

The Güneyce 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.

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Bu Makaleye Atıf Yap

NIELSEN, J. K., GÖRMÜŞ, M., KANBUR, K. U. &. S., KANBUR, S. (2012). Ichnology of the Miocene Güneyce Formation (Southwest Turkey): Oxygenation and Sedimentation Dynamics. Turkish Journal of Earth Sciences, Cilt: 21 - Sayı: 3, 391–405. https://ajindex.com/articles/220755

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Kaynakça (9)

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