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

被引:78
作者
Hower, James C. [1 ]
O'Keefe, Jennifer M. K. [2 ]
Watt, Michael A. [3 ]
Pratt, Timothy J. [4 ]
Eble, Cortland F. [5 ]
Stucker, J. D. [6 ]
Richardson, Allison R. [6 ]
Kostova, Irena J. [7 ]
机构
[1] Univ Kentucky, Ctr Appl Energy Res, Lexington, KY 40511 USA
[2] Morehead State Univ, Dept Phys Sci, Morehead, KY 40351 USA
[3] Weatherford Labs, Arvada, CO 80007 USA
[4] Ticora Geosci, Arvada, CO 80007 USA
[5] Kentucky Geol Survey, Lexington, KY 40506 USA
[6] Univ Kentucky, Dept Earth & Environm Sci, Lexington, KY 40506 USA
[7] Univ Sofia St Kliment Ohridski, Dept Geol & Paleontol, Sofia 1000, Bulgaria
关键词
Fungus; Funginite; Macrinite; Degradation; Rot; PLANT-MATERIAL; PEAT DEPOSITS; RAGGED EDGE; FIRE; REFLECTANCE; KALIMANTAN; PETROLOGY; HERRIN; PALEOECOLOGY; CHARCOALS;
D O I
10.1016/j.coal.2009.08.006
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
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. (C) 2009 Elsevier BY. All rights reserved.
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页码:135 / 143
页数:9
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