{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,7,3]],"date-time":"2026-07-03T09:35:45Z","timestamp":1783071345678,"version":"3.54.6"},"reference-count":166,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[2021,1,15]],"date-time":"2021-01-15T00:00:00Z","timestamp":1610668800000},"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":["JGS"],"published-print":{"date-parts":[[2021,3]]},"abstract":"<jats:p>\n            The existing chronostratigraphic framework in NW Cyprus of two-phase, Early and Late Miocene reef and associated facies development is tested and improved using a combination of calcareous nannofossil, benthic and planktonic foraminiferal, and also Sr isotope dating. Following localized Late Oligocene neritic carbonate deposition (e.g. benthic foraminiferal shoals), reefs and related facies (Terra Member) began to develop\n            <jats:italic>c.<\/jats:italic>\n            24\u2005Ma (Aquitanian) and terminated\n            <jats:italic>c.<\/jats:italic>\n            16\u2005Ma (end-Burdigalian). Early Miocene reef and marginal facies were then extensively redeposited as multiple debris-flow deposits until\n            <jats:italic>c.<\/jats:italic>\n            13.7\u2005Ma, influenced by a combination of global sea-level fall (related to growth of the East Antarctic Ice Sheet) and local- to regional-scale tectonics. Reef growth and related deposition resumed (Koronia Member)\n            <jats:italic>c.<\/jats:italic>\n            9.1\u2005Ma (Tortonian), then terminated by\n            <jats:italic>c.<\/jats:italic>\n            6.1\u2005Ma (Middle Messinian), followed by the Messinian salinity crisis. Neritic accumulation in NW Cyprus began earlier (Late Oligocene), than in southern Cyprus (Early Miocene). The Early Miocene reefs developed on a roughly north\u2013south-trending structural high in the west (Akamas Peninsula area) whereas the Late Miocene reefs developed on both flanks of the neotectonic Polis graben. The two-phase reef development is mirrored in SE Cyprus and in some other Mediterranean areas (e.g. southern Turkey, Israel, Italy, southern Spain).\n          <\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary material:<\/jats:bold>\n            Global positioning system locations of dated samples, the Sr isotope method and the samples examined for planktonic foraminifera biostratigraphy are available at\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" specific-use=\"dataset is-supplemented-by\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.5205315\">https:\/\/doi.org\/10.6084\/m9.figshare.c.5205315<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2020-081","type":"journal-article","created":{"date-parts":[[2020,11,16]],"date-time":"2020-11-16T15:35:20Z","timestamp":1605540920000},"update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":6,"title":["Microfossil and strontium isotope chronology used to identify the controls of Miocene reefs and related facies in NW Cyprus"],"prefix":"10.1144","volume":"178","author":[{"ORCID":"https:\/\/orcid.org\/0000-0001-8416-0340","authenticated-orcid":false,"given":"Torin","family":"Cannings","sequence":"first","affiliation":[{"name":"School of GeoSciences, Grant Institute, University of Edinburgh, James Hutton Road, Edinburgh EH9 3FE, UK"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Elizabeth M.","family":"Balmer","sequence":"additional","affiliation":[{"name":"School of GeoSciences, Grant Institute, University of Edinburgh, James Hutton Road, Edinburgh EH9 3FE, UK"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-0454-0413","authenticated-orcid":false,"given":"Giovanni","family":"Coletti","sequence":"additional","affiliation":[{"name":"Dipartimento di Scienze dell'Ambiente e del Territorio e di Scienze della Terra, Universit\u00e0 di Milano\u2013Bicocca, 20126, Milano, Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-4171-7676","authenticated-orcid":false,"given":"Ryan B.","family":"Ickert","sequence":"additional","affiliation":[{"name":"Scottish Universities Environmental Research Centre, Scottish Enterprise Technology Park, Rankine Avenue, East Kilbride G75 0QF, UK"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Dick","family":"Kroon","sequence":"additional","affiliation":[{"name":"School of GeoSciences, Grant Institute, University of Edinburgh, James Hutton Road, Edinburgh EH9 3FE, UK"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Isabella","family":"Raffi","sequence":"additional","affiliation":[{"name":"Dipartimento di Ingegneria e Geotecnologie (InGeo), CeRSGeoUniversit\u00e0 degli Studi \u2018G. d'Annunzio\u2019 di Chieti\u2013Pescara Campus Universitario, via dei Vestini 31, 66013 Chieti Scalo, Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Alastair H. 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