下泥盆统页岩微生物褶皱结构

IF 0.5 4区地球科学 Q4 GEOLOGY Scottish Journal of Geology Pub Date : 2016-02-16 DOI:10.1144/sjg2015-006

R. Batchelor

{"title":"下泥盆统页岩微生物褶皱结构","authors":"R. Batchelor","doi":"10.1144/sjg2015-006","DOIUrl":null,"url":null,"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.","PeriodicalId":49556,"journal":{"name":"Scottish Journal of Geology","volume":null,"pages":null},"PeriodicalIF":0.5000,"publicationDate":"2016-02-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1144/sjg2015-006","citationCount":"2","resultStr":"{\"title\":\"Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife\",\"authors\":\"R. Batchelor\",\"doi\":\"10.1144/sjg2015-006\",\"DOIUrl\":null,\"url\":null,\"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.\",\"PeriodicalId\":49556,\"journal\":{\"name\":\"Scottish Journal of Geology\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.5000,\"publicationDate\":\"2016-02-16\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1144/sjg2015-006\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Scottish Journal of Geology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1144/sjg2015-006\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Scottish Journal of Geology","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1144/sjg2015-006","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOLOGY","Score":null,"Total":0}

引用次数: 2

摘要

本报告描述了苏格兰下泥盆世沉积物中首次记录的微生物褶皱结构。在新英格兰法夫州Wormit的页岩地层中，发现了一个独特的褶皱表面，这被解释为软沉积物基质上微生物垫的产物。该组合反映了浅水湖泊或潮下环境。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

查看原文

微信好友朋友圈 QQ好友复制链接

本刊更多论文

Microbial wrinkle structures in Lower Devonian shales, Wormit, Fife

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.

求助全文

通过发布文献求助，成功后即可免费获取论文全文。去求助

来源期刊

Scottish Journal of Geology 地学-地质学

CiteScore

1.70

自引率

0.00%

发文量

审稿时长

>12 weeks

期刊介绍： Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh. Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology. The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors. The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.