{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,11,20]],"date-time":"2024-11-20T05:33:50Z","timestamp":1732080830008,"version":"3.28.0"},"reference-count":64,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[2003,11,1]],"date-time":"2003-11-01T00:00:00Z","timestamp":1067644800000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["SJG"],"published-print":{"date-parts":[[2003,11]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>\n            This study concentrates on Vis\u00e9an Strathclyde Group microbial carbonates from the eastern Midland Valley of Scotland. In the largely non-marine Sandy Craig and West Lothian Oil-Shale formations persistent lithostratigraphical marker horizons, such as distinct microbial carbonates, are used to aid correlation of sequences where conventional biostratigraphy is limited to the identification of infrequent marine bands. In the newly described Rosyth core, microbial carbonates above the Burdiehouse Limestone are correlated with microbial horizons at Kingswood (Fife) and Inchkeith (Firth of Forth), a correlation supported by the presence of the bivalve\n            <jats:italic>Curvirimula scotica.<\/jats:italic>\n            The revised position of the Inchkeith microbial horizon to 20\u201330 m above the Burdiehouse Limestone contradicts earlier correlations of the Inchkeith sequences with the Burdiehouse Limestone. The microbial carbonates represent littoral and sublittoral zone stromatolites growing in &lt;20 m of water. The best modern analogues are stromatolites forming in East African Rift Valley lakes. These microbial carbonates formed in volcanically isolated shallow sub-basins or in association with delta progradation. Lavas and tuffs provided stable substrates free of clastic sediment for stromatolite nucleation, and their weathering may have enhanced Ca\n            <jats:sup>2+<\/jats:sup>\n            ion activity to promote carbonate precipitation. These lacustrine microbial carbonates cannot be implicitly linked with climatic events or basin-wide regression as has been proposed for a regionally persistent microbial carbonate below the Burdiehouse Limestone.\n          <\/jats:p>","DOI":"10.1144\/sjg39020151","type":"journal-article","created":{"date-parts":[[2010,1,15]],"date-time":"2010-01-15T00:30:59Z","timestamp":1263515459000},"page":"151-168","update-policy":"http:\/\/dx.doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":7,"title":["Stratigraphic and palaeoenvironmental significance of microbial carbonates in the Asbian Sandy Craig Formation of Fife"],"prefix":"10.1144","volume":"39","author":[{"given":"C.","family":"Guirdham","sequence":"first","affiliation":[{"name":"School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK (e-mail)"}]},{"given":"J. E.","family":"Andrews","sequence":"additional","affiliation":[{"name":"School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK (e-mail)"}]},{"given":"M. A. E.","family":"Browne","sequence":"additional","affiliation":[{"name":"British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK"}]},{"given":"M. T.","family":"Dean","sequence":"additional","affiliation":[{"name":"British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,7]]},"reference":[{"key":"e_1_3_2_2_1","doi-asserted-by":"publisher","DOI":"10.1144\/pygs.28.1.5"},{"key":"e_1_3_2_3_1","doi-asserted-by":"publisher","DOI":"10.1144\/sjg30020105"},{"key":"e_1_3_2_4_1","doi-asserted-by":"publisher","DOI":"10.1144\/sjg34020153"},{"key":"e_1_3_2_5_1","first-page":"427","volume-title":"Deltas: Models for Exploration","author":"BELT E. S.","year":"1975","unstructured":"BELT, E. S. 1975. Scottish carboniferous cyclothem patterns and their palaeoenvironmental significance. In Broussard, M. L. (ed.) Deltas: Models for Exploration, Houston Geological Society, Houston, TX, 427\u2013429."},{"key":"e_1_3_2_6_1","first-page":"203","volume":"158","author":"BRADLEY W. H.","year":"1929","unstructured":"BRADLEY, W. H. 1929. Algae Reef and Oolites of the Green River Formation. US Geological Survey Professional Papers, 158, 203\u2013223.","journal-title":"Algae Reef and Oolites of the Green River Formation"},{"key":"e_1_3_2_7_1","doi-asserted-by":"publisher","DOI":"10.1144\/pygs.47.3.215"},{"key":"e_1_3_2_8_1","unstructured":"BROWNE M. A. E. DEAN M. T. HALL I. H. S. McADAM A. D. MONRO S. K. & CHISHOLM J. I. 1999. A Lithostratigraphical Framework for the Carboniferous Rocks of the Midland Valley of Scotland. British Geological Survey Research Report RR\/99\/07."},{"key":"e_1_3_2_9_1","first-page":"1","volume-title":"The Oil Shales of the Lothians","author":"CARRUTHERS R. 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