CALL FOR PROPOSALS:

ORGANIZERS

  • Harvey Thorleifson, Chair
    Minnesota Geological Survey
  • Carrie Jennings, Vice Chair
    Minnesota Geological Survey
  • David Bush, Technical Program Chair
    University of West Georgia
  • Jim Miller, Field Trip Chair
    University of Minnesota Duluth
  • Curtis M. Hudak, Sponsorship Chair
    Foth Infrastructure & Environment, LLC

 

Paper No. 11
Presentation Time: 9:00 AM-6:00 PM

FUNGAL REMNANTS AND FRAGMENTS OF LOW RANK COAL IN BIGA PENINSULA, NW TURKEY


MARAL, Mehmet, Geological Engineering, Istanbul Technical University, Istanbul Technical University Faculty of Mines, Maslak-Sariyer, Istanbul, 34469, Turkey, HOWER, James C., Center for Applied Energy Research, University of Kentucky, 2540 Research Park Drive, Lexington, KY 40511, O'KEEFE, Jen, Earth & Space Sciences, Morehead State University, 404-A Lappin Hall, Morehead, KY 40351, EBLE, Cortland F., Kentucky Geological Survey, University of Kentucky, 228 Mining and Mineral Resources Bldg, Lexington, KY 40506-0107 and TEMEL, Didem, Geological Engineering, Istanbul Technical University, Istanbul Technical University, Campus of Ayazaga, Faculty of Mines, Dept. of Geological Engineering, Maslak-Sarıyer, Istanbul, 34469, Turkey, maralm@itu.edu.tr

Fungi are associated with degradation and oxidation processes in coal-forming swamp and mire environments. In general, fungi, with symbiotic, parasitic, and saprophytic forms, are found with huminite/vitrinite the wood-derived maceral. This study focuses on identification and interpretation of the fungal fragments of low-rank coal in Biga Peninsula (Mancilik, Sebepli, Tutuncu), NW Turkey. For this aim, the coal occurrences were sampled and the fungal particles recovered from twelve coal samples at Kentucky Geological Survey. Microscopic investigations were performed on polished sections under reflected light and mounted sections with transmitted light at laboratories of University of Kentucky Center for Applied Energy Research, USA. Furthermore, fungal remains recovered through palynologic processing were compared with petrographic sections. Several fungal remnants, which found in transmitted light, could be identified on polished samples. Fungal examinations exhibited that saprophytic form accompanied with huminite/vitrinite, rather than symbiotic and parasitic types.
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