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Abstract
This report describes the first recorded occurrence of microbial wrinkle structures in Lower Devonian sediments in Scotland. A shale horizon at Wormit, NE Fife, has yielded a distinctive puckered surface that is interpreted as the product of microbial mats on a soft sediment substrate. This assemblage reflects a shallow-water lacustrine or sub-tidal environment.
Original language | English |
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Pages (from-to) | 65-67 |
Number of pages | 3 |
Journal | Scottish Journal of Geology |
Volume | 52 |
Issue number | 1 |
Early online date | 16 Feb 2016 |
DOIs | |
Publication status | Published - Aug 2016 |
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Dive into the research topics of 'Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife'. Together they form a unique fingerprint.Projects
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Regional distribution of the Lower Devon: Regional distribution of Lower Devonian Palaeohelcura tridactyla trace fossil in Scotland
Finch, A. A. (PI) & Batchelor, R. A. (CoI)
15/07/14 → 14/10/14
Project: Standard