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Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife

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DOI

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Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife. / Batchelor, Richard A.

In: Scottish Journal of Geology, Vol. 52, No. 1, 08.2016, p. 65-67.

Research output: Contribution to journalArticlepeer-review

Harvard

Batchelor, RA 2016, 'Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife', Scottish Journal of Geology, vol. 52, no. 1, pp. 65-67. https://doi.org/10.1144/sjg2015-006

APA

Batchelor, R. A. (2016). Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife. Scottish Journal of Geology, 52(1), 65-67. https://doi.org/10.1144/sjg2015-006

Vancouver

Batchelor RA. Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife. Scottish Journal of Geology. 2016 Aug;52(1):65-67. https://doi.org/10.1144/sjg2015-006

Author

Batchelor, Richard A. / Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife. In: Scottish Journal of Geology. 2016 ; Vol. 52, No. 1. pp. 65-67.

Bibtex - Download

@article{383ebc4e8411498bba0020283fbd0bf6,
title = "Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife",
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.",
author = "Batchelor, {Richard A.}",
note = "A grant from The Carnegie Trust for the Universities of Scotland funded the fieldwork.",
year = "2016",
month = aug,
doi = "10.1144/sjg2015-006",
language = "English",
volume = "52",
pages = "65--67",
journal = "Scottish Journal of Geology",
issn = "0036-9276",
publisher = "GEOLOGICAL SOC PUBL HOUSE",
number = "1",

}

RIS (suitable for import to EndNote) - Download

TY - JOUR

T1 - Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife

AU - Batchelor, Richard A.

N1 - A grant from The Carnegie Trust for the Universities of Scotland funded the fieldwork.

PY - 2016/8

Y1 - 2016/8

N2 - 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.

AB - 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.

U2 - 10.1144/sjg2015-006

DO - 10.1144/sjg2015-006

M3 - Article

VL - 52

SP - 65

EP - 67

JO - Scottish Journal of Geology

JF - Scottish Journal of Geology

SN - 0036-9276

IS - 1

ER -

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    Batchelor, R. A. & Garton, R. E., 2013, In: Scottish Journal of Geology. 49, p. 149-152

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ID: 226432307

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