{"data":{"id":"10.6084/m9.figshare.1623175","type":"dois","attributes":{"doi":"10.6084/m9.figshare.1623175","prefix":"10.6084","suffix":"m9.figshare.1623175","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Korn, Dieter","nameType":"Personal","givenName":"Dieter","familyName":"Korn","affiliation":[],"nameIdentifiers":[]},{"name":"Ghaderi, Abbas","nameType":"Personal","givenName":"Abbas","familyName":"Ghaderi","affiliation":[],"nameIdentifiers":[]},{"name":"Leda, Lucyna","nameType":"Personal","givenName":"Lucyna","familyName":"Leda","affiliation":[],"nameIdentifiers":[]},{"name":"Schobben, Martin","nameType":"Personal","givenName":"Martin","familyName":"Schobben","affiliation":[],"nameIdentifiers":[]},{"name":"Ashouri, Ali Reza","nameType":"Personal","givenName":"Ali Reza","familyName":"Ashouri","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"The ammonoids from the Late Permian \u003ci\u003eParatirolites\u003c/i\u003e Limestone of Julfa (East Azerbaijan, Iran)"}],"publisher":"Taylor \u0026 Francis","container":{},"publicationYear":2015,"subjects":[{"subject":"Biochemistry"},{"subject":"Medicine"},{"subject":"Microbiology"},{"subject":"FOS: Biological sciences","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"FOS: Biological sciences","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"Molecular Biology"},{"subject":"59999 Environmental Sciences not elsewhere classified","subjectScheme":"FOR"},{"subject":"FOS: Earth and related environmental sciences","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"FOS: Earth and related environmental sciences","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"39999 Chemical Sciences not elsewhere classified","subjectScheme":"FOR"},{"subject":"FOS: Chemical sciences","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"FOS: Chemical sciences","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"Ecology"},{"subject":"Sociology"},{"subject":"FOS: Sociology","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"FOS: Sociology","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"Immunology"},{"subject":"FOS: Clinical medicine","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"FOS: Clinical medicine","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"69999 Biological Sciences not elsewhere classified","subjectScheme":"FOR"},{"subject":"Plant Biology"},{"subject":"Computational Biology"}],"contributors":[],"dates":[{"date":"2015-12-14","dateType":"Created"},{"date":"2016-10-25","dateType":"Updated"},{"date":"2015","dateType":"Issued"}],"language":null,"types":{"ris":"DATA","bibtex":"misc","citeproc":"dataset","schemaOrg":"Dataset","resourceType":"Dataset","resourceTypeGeneral":"Dataset"},"relatedIdentifiers":[{"relationType":"IsSupplementTo","relatedIdentifier":"10.1080/14772019.2015.1119211","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["95821746 Bytes"],"formats":[],"version":null,"rightsList":[{"rights":"Creative Commons Attribution 4.0 International","rightsUri":"https://creativecommons.org/licenses/by/4.0/legalcode","schemeUri":"https://spdx.org/licenses/","rightsIdentifier":"cc-by-4.0","rightsIdentifierScheme":"SPDX"}],"descriptions":[{"description":"The Changhsingian (Late Permian), 4 to 5 m thick \u003ci\u003eParatirolites\u003c/i\u003e Limestone has yielded diverse ammonoid assemblages composed of the genera \u003ci\u003eNeoaganides\u003c/i\u003e, \u003ci\u003ePseudogastrioceras\u003c/i\u003e, \u003ci\u003eDzhulfites\u003c/i\u003e, \u003ci\u003eParatirolites\u003c/i\u003e, \u003ci\u003eJulfotirolites\u003c/i\u003e, \u003ci\u003eAlibashites\u003c/i\u003e, \u003ci\u003eAbichites\u003c/i\u003e, \u003ci\u003eStoyanowites\u003c/i\u003e and \u003ci\u003eArasella\u003c/i\u003e. The succession of ammonoid species allows for a subdivision of the rock unit into eight biozones, in ascending order: \u003ci\u003eDzhulfites zalensis\u003c/i\u003e Zone, \u003ci\u003eParatirolites trapezoidalis\u003c/i\u003e Zone, \u003ci\u003eParatirolites kittli\u003c/i\u003e Zone, \u003ci\u003eStoyanowites dieneri\u003c/i\u003e Zone, \u003ci\u003eAlibashites mojsisovicsi\u003c/i\u003e Zone, \u003ci\u003eAbichites abichi\u003c/i\u003e Zone, \u003ci\u003eAbichites stoyanowi\u003c/i\u003e Zone and \u003ci\u003eArasella minuta\u003c/i\u003e Zone. The following 20 new species are described by two of us (DK and AG): \u003ci\u003eNeoaganides ultimus\u003c/i\u003e sp. nov., \u003ci\u003ePseudogastrioceras relicuum\u003c/i\u003e sp. nov., \u003ci\u003eDzhulfites zalensis\u003c/i\u003e sp. nov., \u003ci\u003eDzhulfites hebes\u003c/i\u003e sp. nov., \u003ci\u003eParatirolites coronatus\u003c/i\u003e sp. nov., \u003ci\u003eParatirolites birunii\u003c/i\u003e sp. nov., \u003ci\u003eParatirolites quadratus\u003c/i\u003e sp. nov., \u003ci\u003eParatirolites multiconus\u003c/i\u003e sp. nov., \u003ci\u003eParatirolites serus\u003c/i\u003e sp. nov., \u003ci\u003eJulfotirolites kozuri\u003c/i\u003e sp. nov., \u003ci\u003eAlibashites ferdowsii\u003c/i\u003e sp. nov., \u003ci\u003eAlibashites uncinatus\u003c/i\u003e sp. nov., \u003ci\u003eAlibashites stepanovi\u003c/i\u003e sp. nov., \u003ci\u003eAbichites subtrapezoidalis\u003c/i\u003e sp. nov., \u003ci\u003eAbichites alibashiensis\u003c/i\u003e sp. nov., \u003ci\u003eAbichites ariaeii\u003c/i\u003e sp. nov., \u003ci\u003eAbichites paucinodus\u003c/i\u003e sp. nov., \u003ci\u003eAbichites shahriari\u003c/i\u003e sp. nov., \u003ci\u003eAbichites terminalis\u003c/i\u003e sp. nov. and \u003ci\u003eStoyanowites aspinosus\u003c/i\u003e sp. nov. After the time-equivalent Chinese occurrences, the material described here is the most diverse assemblage known from the critical interval before the end-Permian mass extinction. 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