Naturally occurring, microbially induced smectite-to-illite reaction
Document Type
Article
Date of Original Version
6-1-2019
Abstract
The occurrence of microbially induced smectite-to-illite (S-I) reaction has challenged both the notions of solely inorganic chemical control for this reaction and the conventional concept of a semiquantitative illite geothermometer for the reconstruction of the thermal and tectonic histories of sedimentary basins. Here, we present evidence for a naturally occurring microbially induced S-I transition, via biotic reduction of phyllosilicate structural Fe(III), in mudstones buried at the Nankai Trough, offshore Japan (International Ocean Discovery Program Site C0023). Biotic S-I reaction is a consequence of a bacterial survival and growth strategy at diagenetic temperatures up to 80 °C within the Nankai Trough mudstones. These results have considerable implications for petroleum exploration, modification of fault behavior, and the understanding of microbial communities in the deep biosphere.
Publication Title, e.g., Journal
Geology
Volume
47
Issue
6
Citation/Publisher Attribution
Kim, Jinwook, Hailiang Dong, Kiho Yang, Hanbeom Park, W. C. Elliott, Arthur Spivack, Tae hee Koo, Gilyoung Kim, Yuki Morono, Susann Henkel, Fumio Inagaki, Qiang Zeng, Tatsuhiko Hoshino, and Verena B. Heuer. "Naturally occurring, microbially induced smectite-to-illite reaction." Geology 47, 6 (2019). doi: 10.1130/G46122.1.