{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,28]],"date-time":"2025-10-28T18:40:44Z","timestamp":1761676844333,"version":"3.40.5"},"reference-count":51,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[2020,6,17]],"date-time":"2020-06-17T00:00:00Z","timestamp":1592352000000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"funder":[{"name":"Yorkshire Geological Society","award":["NA"],"award-info":[{"award-number":["NA"]}]}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["PYGS"],"published-print":{"date-parts":[[2020,11]]},"abstract":"<jats:p>\n            The foreshore at Redcar hosts the oldest Jurassic succession exposed on the Yorkshire-Cleveland Coast but has received little attention since the late nineteenth century. Temporary removal of beach sands by winter storms early in 2018 allowed for a sedimentological and palaeontological study of a nearly 60\u2005m-thick foreshore section. The rocks are latest Hettangian to Early Sinemurian in age (Early Jurassic) and comprise five coarsening-upward cycles (parasequences) that grade from mudstones through siltstones into\n            <jats:italic>Gryphaea<\/jats:italic>\n            -rich shell beds. Ammonites are reasonably common along with a diverse benthos that includes abundant bivalves (e.g.\n            <jats:italic>Gryphaea, Cardinia, Luciniola, Plagiostoma<\/jats:italic>\n            and\n            <jats:italic>Oxytoma<\/jats:italic>\n            ) and rarer serpulids, gastropods, foraminifera and solitary corals. In the upper part of the section thicker-shelled taxa are commonly bored by cirripedes and bryozoans. Despite relatively high benthic diversity and intense bioturbation, pyrite framboids are common with size distributions suggesting deposition under a moderately oxygen-restricted water column. The Redcar succession post-dates the end-Triassic mass extinction by as much as 4 Ma and the diverse marine assemblages indicate that recovery was substantially complete by this time.\n          <\/jats:p>","DOI":"10.1144\/pygs2019-011","type":"journal-article","created":{"date-parts":[[2020,5,6]],"date-time":"2020-05-06T12:56:21Z","timestamp":1588769781000},"page":"77-87","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":3,"title":["The Hettangian\u2013Sinemurian (Lower Jurassic) strata of Redcar, Cleveland Basin, NE England: facies and palaeoecology"],"prefix":"10.1144","volume":"63","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-4042-2489","authenticated-orcid":false,"given":"J. W.","family":"Atkinson","sequence":"first","affiliation":[{"name":"School of Earth and Environment, University of Leeds, Leeds. LS2 9JT, UK"}]},{"given":"P. B.","family":"Wignall","sequence":"additional","affiliation":[{"name":"School of Earth and Environment, University of Leeds, Leeds. LS2 9JT, UK"}]},{"given":"K. 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