Journals / Bulletin of the mineral research and exploration / 2020 / Cilt: 0 - Sayı: 161

Drilling and core data from the Gulf of Gemlik (SE Sea of Marmara): Holocene fauna and flora assemblages

Pages
121–149
Publication Date
2022-10-12
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 mollusc shows the shallow marine community

📌 3 Key Takeaways

🎯
Objective & Hypothesis:This study was conducted to determine fauna and flora assemblages of Holocene sequences fromGemlik Gulf (SE Marmara Sea) and to obtaine their similarities and differences between theassemblages of Gemlik and İzmit Bays.
📊
Key Findings & Data:Total of 201 dark gray colored, fine to medium grainedsandy clay samples were studied.
💡
Conclusion & Impact:The mollusc shows the shallow marine community
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Abstract

This study was conducted to determine fauna and flora assemblages of Holocene sequences fromGemlik Gulf (SE Marmara Sea) and to obtaine their similarities and differences between theassemblages of Gemlik and İzmit Bays. Total of 201 dark gray colored, fine to medium grainedsandy clay samples were studied. In the drilled samples, 22 genera and 38 species were identifiedfrom the foraminifera characterizing the infralittoral zone. 40 genera and 58 species of foraminiferacharacterizing the upper circalittoral zone were identified. In addition, Black Sea originatedAmmonia parasovica was found for the first time in cores taken from Gemlik Gulf. Nannofossilspecies characterizing the open-shallow marine environment Emiliania huxleyi, Reticulofenestraparvula, Coronosphaera spp., Syracosphaera spp., Helicosphaera spp. beside Gephyrocapsaoceanica, small Gephyrocapsa spp., Scyphosphaera porosa were obtained. A total of 27 generaand 37 species from ostracods were defined in the samples from gulf. Moreover, the quite abundantmollusc assemblage characterizing the shallow marine environment and fewer genera and speciesof diatoms were identified. The studied sequence is represented by NN21 Emiliania huxleyi biozoneat the Holocene. Foraminifers and ostracods of the Gemlik Gulf are observed as MediterraneanAegean Sea originated assemblages. The mollusc shows the shallow marine community

🔖

Cite This Article

NAZİK, A., YÜMÜN, Z. Ü., YILDIZ, A., MERİÇ, E., SAGULAR, E. K., YOKEŞ, M. B., BÜYÜKMERİÇ, Y., YAVUZLAR, G. (2022). Drilling and core data from the Gulf of Gemlik (SE Sea of Marmara): Holocene fauna and flora assemblages. Bulletin of the mineral research and exploration, Cilt: 0 - Sayı: 161, 121–149. https://ajindex.com/articles/469365

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (8)

  1. Aksu, A.E., Hiscott, R.N., Yaşar, D. 1999. Oscillating Quaternary water levels of the Marmara Sea and vigorous out- £ow into the Aegean Sea from the Marmara Sea-Black Sea drainage corridor. Marine Geology 153, 275-302.
  2. Aksu, A.E., Hiscott, R.N., Kaminski, M.A., Mudie, P.J., Gillespie, H., Abrajano, T., Yaşar, D. 2002. Last Glacial-Holocene paleoceanography of the Black Sea and Marmara Sea: stable isotopic, foraminiferal and coccolith evidence. Marine Geology 190, 119-149.
  3. Athersuch J., Horne D.J., Whittaker J.E. 1989. Marine and brackish water ostracods. In Kermack D.M., Barnes R.S.K.(Ed.), Synopses of the British Fauna (New Series) 43, 345p. Breman, E. 1975. The distribution of ostracodes in the bottom sediments of the Adriatic Sea. Vrije Universiteit te Amsterdam, Krips Repro, Meppel, 165 p. Brückner, H., Kelterbaum, D., Marunchak, O., Porotov, A., Vott, A. 2010. The Holocene sea level story since 7500 BP - Lessons from the Eastern Mediterranean, the Black and the Azov Seas. Quaternary International 225, 160-179.
  4. Bonaduce G., Ciampo G., Masoli M. 1975. Distribution of Ostracoda in the Adriatic Sea. Pubblicazioni della Stazione Zoologica di Napoli 40, 304 p. Büyükmeriç, Y. 2016. Postglacial flooding of the Marmara Sea (Turkey): Molluscs and sediments tell the story. Geo-Marine Letters 36, 4, 307-321.
  5. Chepalyga, A.L. 2007. The Late Glacial great flood in the Ponto-Caspian basin. In:Yanko-Hombach, V., Gilbert, A.S., Panin, N., Dolukhanov, P.M. (Ed.), The Black Sea Flood Question. Springer, Dordrecht, 119-148.
  6. Cossignani, T., Ardovani, R., Micali, P., Tisselli, M., Cossignani, V., Cecalupo, A. 2011. Malacologia Mediterranea: Atlante delle Conchiglie del Mediterraneo. L’Informatore Piceno, Cupra Marittima, Italy, 536 p. Çağatay, M.N., Görür, N., Algan, O., Eastoe, C., Tchapalyga, A., Ongan, D., Kuhn, T., Kuşçu, I. 2000. Late Glacial-Holocene palaeoceanography of the Sea of Marmara: timing of connections with the Mediterranean and the Black Seas. Marine Geology 167, 191-206.
  7. Çağatay, M.N., Görür, N., Polonia, A., Demirbağ, E., Sakınç, M., Cormier, M.-H.,Capotondi, L., McHugh, C., Emre, Ö., Eriş, K. 2003. Sea level changes and depositional environments in the Izmit Gulf, eastern Marmara Sea, during thelate glacial- Holocene period. Marine Geology 202, 159-173.
  8. Çağatay, M.N., Eris¸, K., Ryan, W.B.F., Sancar, U., Polonia, A., Akcer, S., Biltekin, D., Gasperini, L., Görür, N., Lericolais, G., Bard, E. 2009. Late Pleistocene- Holocene evolution of the northern she