Journals / Maden Tetkik ve Arama Dergisi / 2012 / Cilt: 145 - Sayı: 145

Ilıca Bay (Çeşme-İzmir) Benthic Forminifer-Ostracod Assemblages and Pacific Ocean - Red Sea Originated Foraminifera and Abnormal Individuals

Pages
62–78
Publication Date
2012-02-01
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)

Si, Mg and Mo concentrations of some of the colored Peneroplis planatus (Fichtel ve Moll) individuals are high but the concentration of rare earth elements, such as Tc, Pa, Ru and Mo were obtained from the shells in some of the sampling points.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:- In order to define contemporaneous benthic foraminifera series in surface sediments collected from the surroundings of hot spring locating at 2.50 m depth to the southeast of the Yıldız Cape, Ilıca Bay (Çeşme-İzmir), a total of 38 samples were collected from the three different transects.
📊
Key Findings & Data:The Pacific Ocean and Red Sea originated benthic foraminifera species found in this study are; Nodopthalmidium antillarum (Cushman), Spiroloculina antillarum d’Orbigny, Triloculina fichteliana d’Orbigny, Euthymonacha polita (Chapman), Coscinospira acicularis (Batsch), Peneroplis arietinus (Batsch), Amphisorus hemprichii Ehrenberg, Sorites orbiculus Ehrenberg, Cymbaloporetta plana (Cushman).
💡
Conclusion & Impact:Si, Mg and Mo concentrations of some of the colored Peneroplis planatus (Fichtel ve Moll) individuals are high but the concentration of rare earth elements, such as Tc, Pa, Ru and Mo were obtained from the shells in some of the sampling points.
🔬Design:Research Article
📍Scope:38 samples
⚙️Variables:Eastern Aegean Sea · Alien foraminifera · colored tests

Abstract

- In order to define contemporaneous benthic foraminifera series in surface sediments collected from the surroundings of hot spring locating at 2.50 m depth to the southeast of the Yıldız Cape, Ilıca Bay (Çeşme-İzmir), a total of 38 samples were collected from the three different transects. The Pacific Ocean and Red Sea originated benthic foraminifera species found in this study are; Nodopthalmidium antillarum (Cushman), Spiroloculina antillarum d’Orbigny, Triloculina fichteliana d’Orbigny, Euthymonacha polita (Chapman), Coscinospira acicularis (Batsch), Peneroplis arietinus (Batsch), Amphisorus hemprichii Ehrenberg, Sorites orbiculus Ehrenberg, Cymbaloporetta plana (Cushman). In addition to these species, Peneroplis arietinus (Batsch), Spiroloculina antillarum d’Orbigny, Triloculina cf. fichteliana d’Orbigny and Cymbaloporetta plana (Cushman) which were recorded on the southwest coasts of Antalya were also found in this region. Euthymonacha polita (Chapman) which was first recorded in Kuşadası Bay is also abundant in Ilıca Bay. This observation shows a northward distribution of this species. Coscinospira acicularis (Batsch) is a southwest Pacific originated species which is also found in Gulf of Aqaba, north of Red Sea. It is a typical alien species inhabiting the Ilıca Bay. This is the first record of this species both for the Mediterranean and Aegean Seas. Amphistegina lobifera Larsen was abundantly found around two submarine springs in Kuşadası Bay, situating at the south of Ilıca Bay. It was also recorded on the northwestern coasts of Karaburun Peninsula to the north of the study area. Meanwhile, the absence of Amphistegina lobifera Larsen in Ilıca Bay is the most striking feature of this study. Si, Mg and Mo concentrations of some of the colored Peneroplis planatus (Fichtel ve Moll) individuals are high but the concentration of rare earth elements, such as Tc, Pa, Ru and Mo were obtained from the shells in some of the sampling points.

🔖

Cite This Article

MERİÇ, E., AVŞAR, N., NAZİK, A., YOKEŞ, B., BARUT, İ. F., ERYILMAZ, M., KAM, E., TAŞKIN, H., BAŞSARI, A., DİNÇER, F., BİRCAN, C., KAYGUN, A. (2012). Ilıca Bay (Çeşme-İzmir) Benthic Forminifer-Ostracod Assemblages and Pacific Ocean - Red Sea Originated Foraminifera and Abnormal Individuals. Maden Tetkik ve Arama Dergisi, Cilt: 145 - Sayı: 145, 62–78. https://ajindex.com/articles/54077

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (13)

  1. Aitken, M.J., Michael, H.N., Betancourt, P.P., Warren, P.M., 1988, The Thera eruption: continuing discussion of the dating. Ar- chaeometry 30 (1): 165-181.
  2. Avşar, N. and Meriç, E., 2001, Çeşme-Ilıca Koyu (İzmir) bölgesi güncel bentik foraminifer- lerinin sistematik dağılımı. H. Ü. Yerbilim- leri, 24: 13-22, Ankara.,, Çevik, M.G. and Dinçer, F., 2009, Büyük Menderes Nehri önü (B Türkiye) kıta sahanlığı bölgesi güncel bentik foraminifer toplulukları. H. Ü. Yerbilimleri, 30 (2): 127- 144, Ankara.
  3. Babin, C. 1980. Elements of Palaeontology. John Wiley and Sons. Chichester. 446s. ISBN 0 471 27577 8 (56 Bab). Barut, I.F., Erdoğan (Yüzbaşıoğlu) N. and Başak, E., 2004, Hydrogeochemical evaluation of Western Anatolian mineralwaters. Environ- mental Geology, 45 (4), 494-503.
  4. Başkan, E. and Canik, B., 1983, Türkiye Sıcak ve Mineralli Sular Haritası, Ege Bölgesi. MTA Enstitüsü Yayınları, No.189, 80 s., Ankara.
  5. Bignot, G., 1985. Elements of micropaleontol- ogy. London: Graham and Trotman Ltd., 217s. Breman, E., 1975, The distribution of ostracodes in the bottom sediments of the Adriatic Sea. Vrije Universiteit te Amsterdam, Krips Repro, Meppel, 165 s. Çağlar, K.Ö., 1946, Türkiye Maden Suları ve Kaplıcaları. Maden Tetkik ve Arama En- stitüsü Yayınları,
  6. Seri B, No. 11, 791 s., Ankara.
  7. Çakmakoğlu, A. and Bilgin, Z.R., 2006, Karabu- run Yarımadası’nın Neojen öncesi strati- grafisi. Maden Tetkik ve Arama Dergisi (in Turkish), 132, 33-62,
  8. Ankara.
  9. Erişen, B., Akkuş, İ., Uygur, N. and Koçak, A., 1996, Türkiye Jeotermal Envanteri. MTA Genel Müdürlüğü, 480 s., Ankara.
  10. Greaves, A.M., 2003, Miletos Bir Tarih. Çev: Çınar Öztürk. Homer Kitabevi, İstanbul.10-1l0. Guillaume, M.C., Peypouquet, J.P. and Tetart, J., 1985, Quaternaire et actuel. Atlas des Os- tracodes de France, Ed: H.J. Oertli. Bull. Centres Rech. Explor. Prod. Elf-Aquitaine. Mém.9, 337-377.
  11. Hartman, G. and Puri, H., 1974, Summary of Neontological and Paleontological Classi- fication of Ostracod. Mitt. Hamburg Zool. Must. Inst., 20, 7-73.
  12. Hottinger, L., Halicz, E. and Reiss, Z., 1993, Re- cent foraminifera from the Gulf of Aqaba, Red Sea. Slovenska Akademija Znanosti in Umetnosti, 179 p. (pl. 1-230),
  13. Ljubljana. Joachim, C. and Langer, M.R. 2008, The 80 most common Ostracods from the Bay of Fe- tovaia Elba Island (Mediterranean Sea), Universität Bonn, 29p. Koukousioura O. and Dimiza M.D., Triantaphyllou M.V., 2010, Alien foraminifers from Greek coastal areas (Aegean Sea, Eastern Medi- terranean). Mediterranean Marine Sci