{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,11,20]],"date-time":"2024-11-20T05:34:36Z","timestamp":1732080876712,"version":"3.28.0"},"reference-count":38,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[1987,5,1]],"date-time":"1987-05-01T00:00:00Z","timestamp":546825600000},"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":[[1987,5]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>\n            Two new records are described and one previous record reviewed of isolated coral colonies from Llandovery turbidites in the south-west Southern Uplands. Criteria allowing the distinction between modes of origin of such specimens by floatation, bedload transportation and\/or reworking are discussed. Two of the specimens, the tabulate corals\n            <jats:italic>Propora exigua<\/jats:italic>\n            and\n            <jats:italic>P. edwardsi,<\/jats:italic>\n            are interpreted as derived from contemporaneous shelf environments and transported by floatation and sinking to their points of interment. The third, a rugose coral\n            <jats:italic>Ceriaster<\/jats:italic>\n            sp., was probably transported in the same way initially, but may have reached its final locus of deposition as part of a turbidite bedload. All three corals are of biostratigraphic or palaeobiogeographic interest.\n            <jats:italic>Propora exigua<\/jats:italic>\n            is characteristic of the Telychian whilst\n            <jats:italic>P. edwardsi sensu stricto<\/jats:italic>\n            has only been recorded previously from earlier Llandovery rocks near Girvan. The geographical range of the genus\n            <jats:italic>Ceriaster<\/jats:italic>\n            was hitherto restricted to Asia.\n          <\/jats:p>","DOI":"10.1144\/sjg23010049","type":"journal-article","created":{"date-parts":[[2010,1,15]],"date-time":"2010-01-15T00:30:59Z","timestamp":1263515459000},"page":"49-64","update-policy":"http:\/\/dx.doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":4,"title":["The derivation, biostratigraphy and palaeobiogeographic significance of corals from Silurian deep-sea turbidite facies in the south-west Southern Uplands"],"prefix":"10.1144","volume":"23","author":[{"given":"Colin T.","family":"Scrutton","sequence":"first","affiliation":[{"name":"Department of Geology, The University, Newcastle upon Tyne, NE1 7RU"}]},{"given":"John A.","family":"McCurry","sequence":"additional","affiliation":[{"name":"Department of Geology, The University, St. Andrews, Fife, KY16 9ST"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,7]]},"reference":[{"key":"e_1_2_1_2_1","first-page":"209","article-title":"A method of predicting the density of fossil corals","volume":"4","author":"ABBOTT B. 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