Journals / Turkish Journal of Fisheries and Aquatic Sciences / 2014 / Cilt: 14 - Sayı: 2

The First marine filamentous fungi discovered in the bottom sediments of the oxic/anoxic interface and in the bathyal zone of the black sea

Pages
497–505
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 results indicate to the presence of so far unknown species of mycobiota in the bottom sediments of the oxic/anoxic interface and maximal depths of the Black Sea.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:This is the first information about the filamentous fungi of the deep soft sediments at the transition zone from oxic to anoxic conditions in the Bosporus outlet area of the Black Sea (117.4, 149.9, 252.4, 262.7 and 295.7m) and maximal depth (2250m) of the Black Sea.
📊
Key Findings & Data:At direct microscopy of the deep -water bottom sediments the filamentous mycobiota, belonging to Division.
💡
Conclusion & Impact:The results indicate to the presence of so far unknown species of mycobiota in the bottom sediments of the oxic/anoxic interface and maximal depths of the Black Sea.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Özet

This is the first information about the filamentous fungi of the deep soft sediments at the transition zone from oxic to anoxic conditions in the Bosporus outlet area of the Black Sea (117.4, 149.9, 252.4, 262.7 and 295.7m) and maximal depth (2250m) of the Black Sea. At direct microscopy of the deep -water bottom sediments the filamentous mycobiota, belonging to Division. Ascomycota were found. The results indicate to the presence of so far unknown species of mycobiota in the bottom sediments of the oxic/anoxic interface and maximal depths of the Black Sea. The morphologic difference of mycelium indicates to species diversity of fungi in the extreme benthic conditions. Large accumulations of mycelium in the bottom sediments in Black sea deep -water zone is the evidence o f fungi habitation in the hydrogen sulfide zone. By the present time this information is based on the individual studies and brings more questions than answers. However, the mycelium was found at several stations near Bosporus region of the Black Sea, whic h proves the regularities of the phenomenon. Further studies of this region s bottom sediments are needed to yield more information about the fungi of the soft sediments in the transitional oxic/anoxic water masses and deep water of the Black Sea.

🔖

Cite This Article

SERGEEVA, N. G., KOPYTİNA, N. I. (2014). The First marine filamentous fungi discovered in the bottom sediments of the oxic/anoxic interface and in the bathyal zone of the black sea. Turkish Journal of Fisheries and Aquatic Sciences, Cilt: 14 - Sayı: 2, 497–505. https://ajindex.com/articles/407823

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (1)

  1. Artemchuk, N. Ya. 1981. Mikoflora of the seas of the U.S.S.R., Мoscow, Science, 190 pp. Buchalo, A.S. 2003. Fungi in saline water bodies. In: E. Nevo, A. Oren, S.P. Wasser (Eds.), Fungal life in the Dead Sea. A.R.G. Gantner Verlag, Ruggell Buchalo AS, 361 pp. Cathrine, S.J. and Raghukumar, C. 2009. Anaerobic denitrification in fungi from the coastal marine sediments off Goa, India Mycological Research, 113 (1): 100 -109 Damare, S., Raghukumar, C. and Raghukumar, S. 2006. Fungi in deep -sea sediments of the Central Indian Basin. Deep -Sea, Research I, 53(1): 14 –27. Dudka, I.A. and Kopytina, N.I. 2011. Species Diversity of the Black Sea Fungal.Abstract 3 rd Bi-annual BS Scientific Conference and UP-GRADE BS -SCENE Project Joint Conference. 1 –4 November 2011, Odessa. Ukraine: 203 -204. Kohlmeyer, J. and Kohlmeyer, E. 1979. Marine Mycology. The Higher Fungi. Academic Press, New York, 690 pp. Kopytina, N.I. and Zaytsev, Yu.P. 2011. Mycological researches in the hydrogen -sulfide zone of the Black Sea (review). Ecological Safety of the Coastal and Shelf Zone and Integrated use of the Shelf’s Resources, 25: 286 – 298. (in Russian). Korovchinsky, N.M.and Sergeeva, N.G. 2008. A new family of the order Ctenopoda (Crustacea: Cladocera) from the depths of the Black Sea. Zootaxa, 1795: 57 – 66. Kriss, A.E. 1959. Marine microbiology (deepwater).- M. Publ. house, USSR Aca. Sci., 455 pp. (in Russian). Kriss, A.E. and Novozhilova, M.I 1954. Presence of yeasts in seas and oceans. Mikrobiologiya, 23(6): 669 -8 3 (in Russian). Kriss, A.E., Rukina, E.A. and Biryuzova, V.I. 1951. Microzoning in the heterotrophy microorganizms’ distribution in the Black Sea. Mikrobiologiya, 20(3): 256 -260. (in Russian). Kriss, A.E., Rukina, E.A. and Tichonenko, A.S. 1952 Distribu tion of the yeast organisms in the sea. Journal of General Biology, 8(3): 232 -242 (in Russian). Kurakov, A.V., Lavrentiev, R.B., Nechitaylo, T.Yu., Golyshin, P.N. and Zvyagintsev, D.G. 2008. Diversity of facultatively anaerobic filamentous fungi in soils. Mikrobiologiya, 77(1): 103 -112 (in Russian). Meyers, S.P., Ahearn, D.G. and Roth, F.J. 1967. Mycological investigations of the Black Sea Bull. Mar. Sci. Gulf. Caribbean, 17 (3): 576 -596. Pivkin, M.V., Kuznetsova, T.A. and Sova, V.V. 2006. Marine fungi and their metabolites Vladivostok, Dalnauka Publ., 247 pp. (in Russian). Polikarpov, G.G. 2012. Extreme life and created by it the life’s sphere for itself in the Black sea bathyal). Marine Ecological Journ