Journals / Türkiye Jeoloji Bülteni / 2010 / Cilt: 53 - Sayı: 1

Salyan formasyonu’undaki (Üst Burdigaliyen-Alt Langiyen) Crassostrea gryphoides (Schlotheim, 1813) kavkıları üzerinde biyoerozyon yapıları, K. Maraş, Güneydoğu Türkiye

Bioerosion structures on the Crassostrea gryphoides (Schlotheim, 1813) shells from the Salyan formation (Upper Burdigalian-Lower Langhian), K. Maraş, Southeastern Turkey

Pages
45–62
Publication Date
2022-11-05
DOI
—
🏛️Bibliographic metadata and full text access for this article are provided via DergiPark.
DergiPark Record ↗
✨

AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

The activity of Clionid sponges, Polychaete worms and vermetid gastropods have also been observed.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:The Salyan Formation (Upper Burdigalian-Lower Langhian) of K.
📊
Key Findings & Data:Bioerosion structures found on the Early-Middle Miocene oyster specimens Crassostrea gyrphoides (Schlotheim, 1813) from the Northwestern K.
💡
Conclusion & Impact:The activity of Clionid sponges, Polychaete worms and vermetid gastropods have also been observed.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Abstract

The Salyan Formation (Upper Burdigalian-Lower Langhian) of K. Maraş, Turkey contains thick-bedded deposits of oysters. Bioerosion structures found on the Early-Middle Miocene oyster specimens Crassostrea gyrphoides (Schlotheim, 1813) from the Northwestern K. Maraş Basin area are much affected by the boring of micro-organisms. The borings, represented by three ichnogenera, are assigned to Renichnus isp., Caulostrepsis isp., and Entobia isp. The activity of Clionid sponges, Polychaete worms and vermetid gastropods have also been observed.

Özet

K. Maraş’da Salyan Formasyonu (Üst Burdigaliyen-Alt Langiyen) kalın oyster depoları içermektedir. Kahramanmaraş Miyosen Havza’sının kuzeybatısında, oyucu/delici mikro-organizmalar tarafından oluşturulan biyoerozyon yapıları Crassostrea gryphoides (Schlotheim, 1813) oyster türü üzerinde bulunmuştur. Bu oyuk/delikler üç iz fosil cinsini; Renichnus isp., Caulostrepsis isp., ve Entobia isp., işaret etmektedir. Bu yapılar Klionid süngerler, Polychaete kurtlar ve vermetid gastropodların aktiviteleri olarak gözlemlenmşitir.

🔖

Cite This Article

OKAN, Y., HOŞGÖR, İ. (2022). Salyan formasyonu’undaki (Üst Burdigaliyen-Alt Langiyen) Crassostrea gryphoides (Schlotheim, 1813) kavkıları üzerinde biyoerozyon yapıları, K. Maraş, Güneydoğu Türkiye. Türkiye Jeoloji Bülteni, Cilt: 53 - Sayı: 1, 45–62. https://ajindex.com/articles/629695

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (14)

  1. Aigner, T., 1984. Dynamic stratigraphy of epicontinental carbonates, Upper Muschelkalk (M. Triassic), South- German Basin. Neus Jahrbuch für Geologie und Palaontologie Abhandlungen, 169, 127-159.
  2. Baluk, W., 2006. Middle Miocene (Badenian) gastropods from Korytnica, Poland; Part V, Addenda et Corrigenda ad Prosobranchia. Acta Geologica Polonica, 56, 177-220.
  3. Barrier, P. and D’Alessandro, A., 1985. Structures biogeniques et physiques dans les sables de Pavigliana Reggio Calabra (Italie). Rivista Italiana di Paleontologia e Stratigrafia, 91, 379- 408. Brett, C.E. and Baird, G.C., 1986. Comparative taphonomy: A key to paleoenvironmental interpretation based on fossil preservation. Palaios, 1, 207-227.
  4. Bromley, R.G., 1970. Borings as trace fossils and Entobia cretacea PORTLOCK, as an example. In: Crimes T.P and Harper J.G. (eds.), Trace Fossils. Liverpool, Seel House Pres, 49-90.
  5. Bromley, R.G., 1978. Bioerosion of Bermuda reefs. Palaeogeography, Palaeoclimatology, Palaeoecology, 23, 169-197.
  6. Bromley, R.G., 1981. Concepts in ichnotaxonomy illustrated by small round holes in shells. Acta Geologica Hispanica, 16, 55-64.
  7. Bromley, R.G., 1992. Bioerosion: eating rocks for fun and profit. In: Maples, C.G. and West, R.R. (eds.), Trace Fossils: Short Courses in Paleontology, 5, 121-129.
  8. Paleontological Society, Knoxville, Tennessee. Bromley, R.G., 1994. The palaeoecology of bioeorosion. In. S.K.Donovan (ed.), The palaeobiology of Trace Fossils, John Willey and Soons, Chichester, 134-154.
  9. Bromley, R.G. and D’Alessandro, A., 1983. Bioerosion of the Pleistocene of southern Italy: ichnogenera Caulostrepsis and Maeandroplydora. Rivista İtaliana di Paleontologia e Stratigrafia, 89, 283-309.
  10. Bromley, R.G. and D’Alessandro, A., 1984. The ichnogenus Entobia from the Miocene, Pliocene and Pleistocene of southern Italy. Rivista İtaliana di Paleontologia e Stratigrafia, 90, 227-296.
  11. Bromley, R.G. and D’Alessandro, A., 1989. Ichnological study of shallow marine endolithic sponges from the Italian coast. Rivista İtaliana di Paleontologia e Stratigrafia, 95, 279-314.
  12. Bromley, R.G. and Heinberg, C., 2006. Attachment strategies of organisms on hard substrates: A palaeontological view. Palaeogeography, Palaeoclimatology, Palaeoecology, 232, 429-453.
  13. Bromley, R.G. and Martinell, J., 1991. Centrichnus, new ichnogenus for centrically patterned attachment scars on skeletal substrates. Bulletin of the Geological Society of Denmark, 38, 243-252.
  14. Bronn, H. G., 1837. Lethaea Geognostica, oder Ab