Notes on the origin of inertinite macerals in coals: Observations on the importance of fungi in the origin of macrinite

James C. Hower, Jennifer M.K. O'Keefe, Michael A. Watt, Timothy J. Pratt, Cortland F. Eble, J. D. Stucker, Allison R. Richardson, Irena J. Kostova

Research output: Contribution to journalArticlepeer-review

82 Scopus citations

Abstract

Macrinite is a, generally, rare inertinite maceral, often incorporating remnants and fragments of other macerals, including vitrinite, liptinite, and other inertinite. The associated inertinites include multiple forms of funginite. Funginite is also commonly found in association with vitrinite of slightly elevated reflectance and with degraded varieties of vitrinite. Together with the highly degraded macrinite, the latter two associations are here inferred to be part of a continuum of fungal and microbial degradation of peat. In any case, the origin of some macrinite is potentially distinct from that of inertinite generated by fire.

Original languageEnglish
Pages (from-to)135-143
Number of pages9
JournalInternational Journal of Coal Geology
Volume80
Issue number2
DOIs
StatePublished - Nov 1 2009

Keywords

  • Degradation
  • Funginite
  • Fungus
  • Macrinite
  • Rot

ASJC Scopus subject areas

  • Fuel Technology
  • Geology
  • Economic Geology
  • Stratigraphy

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