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Year 2010, Volume: 140 Issue: 140, 73 - 79, 01.09.2010

Abstract


References

  • Banks, D.A. 1986. Hydrothermal chimneys and fossil worms from the Tynagh Pb-Zn deposits, Ireland, Geology and genesis of mineral deposits in Ireland, 441-447.
  • Bitter, P.H., Scott, S.D. and Schenk, P.E. 1992. Chemosynthesis; an alternate hypothesis for carboniferous biotas in bryozoan/microbial mounds Newfoundland, Canada, Palaios, 7, 466-484.
  • Hannington, M.D., de Ronde, C.E.J. and Petersen, S. 2005. Seafloor tectonics and submarine hydro- thermal systems. Econ Geol 100thAnn vol: 111- 141
  • Haymon, R.M., Koski, R.A. and Sinclair, C. 1984. Fossils of hydrothermal vent forms discovered in Cretaceous sulfide ores of The Semail ophio- lite, Oman, Science, 223, 1407-1409.
  • Hebert, R. and Constantin, M. 1991. Petrology of hydrothermal metamorphism of oceanic Layer 3; implications for sulphide parageneses and redistribution, Economic Geology, 86, (3), 472- 485.
  • Ivanov, S. N. 1947. Study experience of geology and mineralogy of the Sibay massive sulphide deposit, Akademii Nauk SSSR, Uralskiy Filial, 2, 1-109 (in Russian).
  • Kuznetzov, A.P., and Sobetskii, V.A. 1988. Fosil fauna in the sulphide hydrothermal hills from the middle Devonian paleo-ocean of the Ural area. Doklady Akademii Nauk SSSR, 303, 1481 (in Russian). , Maslennikov, V. V. and Zaikov, V.V. 1993. The near hydrothermal fauna of the Silurian paleo- ocean in the South Ural. Izvestia Akademii Nauk SSSR. Seria Biologicheskaya, 4, 534- 535 (in Russian).
  • Little, C.T.S. 2002. The fossil record of hydrothermal vent communities. Cahiers Biol Marine 43: 313- 316.
  • Little, C. T. S., Maslennikov, V. V., Morris, N. J. and Zaykov, V.V. Silurian high temperature hydrothermal vent community from the Southern Urals, Russia, Nature, 1997. v. 385, no. 9, 3-6.
  • Lob'e, L. 1990. Oasises on the ocean floor. Moscow. Hydrometeoizdat (in Russian).
  • Malahova, N. P. 1969. Fauna and host sequence of massive sulphide deposits of the South Urals, Akademii Nauk SSSR, Uralskiy Filial, 81, 3-84 (in Russian).
  • Maslennikov, V. V. 2009. Oral communication; Institute of Mineralogy, Russia Academy of Science, Ural Division of RAS.
  • Monroe, J.S. and Wicander, R. 2005. Fiziksel jeoloji, yeryuvarý'nýn araþtýrýlmasý (türkçe baskýya hazýrlayanlar: Dirik, K. ve Þener, M.), TMMOB Jeoloji Mühendisleri Odasý Çeviri Serisi No 1, 642s., 2007, Ankara.
  • Prokin, V.A., Bogoyavlenskaya, O.V. and Maslennikov, V.V. 1985. Conditions of locations of fosil at massive copper sulphide deposits in the Urals. Geology of Ore Deposits, 1, 114-117 (in Russian).
  • Rona, P.A. 1984. Hydrothermal mineralization at seafloor spreading centers. Earth Sci Rev 20: 1-104. , Bostrom, K., Laubier, L., and Smith, K.L. (edt). 1983. Hydrothermal processes at seafloor spreading centers. Plenum, Newyork, 796 pp.
  • Qudin, E. and Constantinou, G. 1984. Black smoker chimney fragments in Cyprus sulphide deposits, Nature, 308, 349-353.
  • Spooner, E.T.C. and Fyfe, W.S. 1973. Sub-seafloor metamorphism, heat and mass transfer. Contribution Mineralogy and Petrology. 42, 287-304.
  • Zaykov, V.V., Shadlun, T.N., Maslennikov, V.V. and Bortnikov, N.S. 1995. Yaman-Kasy sulphide deposits - ancient "black smoker" of Urals paleoocean. Geology of ore deposits, 37, 511- 529.

Preliminary findings on the fossil traces in the massive sulphite deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli)

Year 2010, Volume: 140 Issue: 140, 73 - 79, 01.09.2010

Abstract

Tubeworm fossils have been found in the Upper Cretaceous aged massive sulphite deposits of the Eastern Black Sea Region. Similar ones of these tube worm fossils have been found in the massive sulfide deposits of Umman, Cyprus, Ireland and Urals. This fossil community defined in very few massive sulfide deposits in the world is the important evidence of the seafloor hydrothermal vents in Pontids. These worm-like forms can be considered as the ancestral forms of the unusual vent communities defined in places where modern hydrothermal vents are observed such as East Pacific Rise, Galapagos and Juan de Fuca Ridge.

References

  • Banks, D.A. 1986. Hydrothermal chimneys and fossil worms from the Tynagh Pb-Zn deposits, Ireland, Geology and genesis of mineral deposits in Ireland, 441-447.
  • Bitter, P.H., Scott, S.D. and Schenk, P.E. 1992. Chemosynthesis; an alternate hypothesis for carboniferous biotas in bryozoan/microbial mounds Newfoundland, Canada, Palaios, 7, 466-484.
  • Hannington, M.D., de Ronde, C.E.J. and Petersen, S. 2005. Seafloor tectonics and submarine hydro- thermal systems. Econ Geol 100thAnn vol: 111- 141
  • Haymon, R.M., Koski, R.A. and Sinclair, C. 1984. Fossils of hydrothermal vent forms discovered in Cretaceous sulfide ores of The Semail ophio- lite, Oman, Science, 223, 1407-1409.
  • Hebert, R. and Constantin, M. 1991. Petrology of hydrothermal metamorphism of oceanic Layer 3; implications for sulphide parageneses and redistribution, Economic Geology, 86, (3), 472- 485.
  • Ivanov, S. N. 1947. Study experience of geology and mineralogy of the Sibay massive sulphide deposit, Akademii Nauk SSSR, Uralskiy Filial, 2, 1-109 (in Russian).
  • Kuznetzov, A.P., and Sobetskii, V.A. 1988. Fosil fauna in the sulphide hydrothermal hills from the middle Devonian paleo-ocean of the Ural area. Doklady Akademii Nauk SSSR, 303, 1481 (in Russian). , Maslennikov, V. V. and Zaikov, V.V. 1993. The near hydrothermal fauna of the Silurian paleo- ocean in the South Ural. Izvestia Akademii Nauk SSSR. Seria Biologicheskaya, 4, 534- 535 (in Russian).
  • Little, C.T.S. 2002. The fossil record of hydrothermal vent communities. Cahiers Biol Marine 43: 313- 316.
  • Little, C. T. S., Maslennikov, V. V., Morris, N. J. and Zaykov, V.V. Silurian high temperature hydrothermal vent community from the Southern Urals, Russia, Nature, 1997. v. 385, no. 9, 3-6.
  • Lob'e, L. 1990. Oasises on the ocean floor. Moscow. Hydrometeoizdat (in Russian).
  • Malahova, N. P. 1969. Fauna and host sequence of massive sulphide deposits of the South Urals, Akademii Nauk SSSR, Uralskiy Filial, 81, 3-84 (in Russian).
  • Maslennikov, V. V. 2009. Oral communication; Institute of Mineralogy, Russia Academy of Science, Ural Division of RAS.
  • Monroe, J.S. and Wicander, R. 2005. Fiziksel jeoloji, yeryuvarý'nýn araþtýrýlmasý (türkçe baskýya hazýrlayanlar: Dirik, K. ve Þener, M.), TMMOB Jeoloji Mühendisleri Odasý Çeviri Serisi No 1, 642s., 2007, Ankara.
  • Prokin, V.A., Bogoyavlenskaya, O.V. and Maslennikov, V.V. 1985. Conditions of locations of fosil at massive copper sulphide deposits in the Urals. Geology of Ore Deposits, 1, 114-117 (in Russian).
  • Rona, P.A. 1984. Hydrothermal mineralization at seafloor spreading centers. Earth Sci Rev 20: 1-104. , Bostrom, K., Laubier, L., and Smith, K.L. (edt). 1983. Hydrothermal processes at seafloor spreading centers. Plenum, Newyork, 796 pp.
  • Qudin, E. and Constantinou, G. 1984. Black smoker chimney fragments in Cyprus sulphide deposits, Nature, 308, 349-353.
  • Spooner, E.T.C. and Fyfe, W.S. 1973. Sub-seafloor metamorphism, heat and mass transfer. Contribution Mineralogy and Petrology. 42, 287-304.
  • Zaykov, V.V., Shadlun, T.N., Maslennikov, V.V. and Bortnikov, N.S. 1995. Yaman-Kasy sulphide deposits - ancient "black smoker" of Urals paleoocean. Geology of ore deposits, 37, 511- 529.
There are 18 citations in total.

Details

Primary Language English
Subjects Engineering
Journal Section Articles
Authors

M. Kemal Revan

Taner Ünlü

Yurdal Genç

Publication Date September 1, 2010
Published in Issue Year 2010 Volume: 140 Issue: 140

Cite

APA Revan, M. K., Ünlü, T., & Genç, Y. (2010). Preliminary findings on the fossil traces in the massive sulphite deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli). Bulletin of the Mineral Research and Exploration, 140(140), 73-79.
AMA Revan MK, Ünlü T, Genç Y. Preliminary findings on the fossil traces in the massive sulphite deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli). Bull.Min.Res.Exp. September 2010;140(140):73-79.
Chicago Revan, M. Kemal, Taner Ünlü, and Yurdal Genç. “Preliminary Findings on the Fossil Traces in the Massive Sulphite Deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli)”. Bulletin of the Mineral Research and Exploration 140, no. 140 (September 2010): 73-79.
EndNote Revan MK, Ünlü T, Genç Y (September 1, 2010) Preliminary findings on the fossil traces in the massive sulphite deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli). Bulletin of the Mineral Research and Exploration 140 140 73–79.
IEEE M. K. Revan, T. Ünlü, and Y. Genç, “Preliminary findings on the fossil traces in the massive sulphite deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli)”, Bull.Min.Res.Exp., vol. 140, no. 140, pp. 73–79, 2010.
ISNAD Revan, M. Kemal et al. “Preliminary Findings on the Fossil Traces in the Massive Sulphite Deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli)”. Bulletin of the Mineral Research and Exploration 140/140 (September 2010), 73-79.
JAMA Revan MK, Ünlü T, Genç Y. Preliminary findings on the fossil traces in the massive sulphite deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli). Bull.Min.Res.Exp. 2010;140:73–79.
MLA Revan, M. Kemal et al. “Preliminary Findings on the Fossil Traces in the Massive Sulphite Deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli)”. Bulletin of the Mineral Research and Exploration, vol. 140, no. 140, 2010, pp. 73-79.
Vancouver Revan MK, Ünlü T, Genç Y. Preliminary findings on the fossil traces in the massive sulphite deposits of Eastern Black Sea Region (Lahanos, Killik and Çayeli). Bull.Min.Res.Exp. 2010;140(140):73-9.

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