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A new biostratigraphically significant calcareous nannofossil species in the Early Pliocene of the Mediterranean
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2006
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BiologyEarly PlioceneMarine GeologyBiodiversityRounded SpeciesEngineeringPaleoenvironmental ReconstructionMediterranean Carlos LancisNatural SciencesMorphological EvidenceEvolutionary BiologyCretaceous PeriodMarine BiologyPlant TaxonomySubchron ThveraPaleobotany
Research Article| December 01, 2006 A new biostratigraphically significant calcareous nannofossil species in the Early Pliocene of the Mediterranean Carlos Lancis; Carlos Lancis 1Departamento de Ciencias de la Tierra, Facultad de Ciencias, Universidad de Alicante, Spain Search for other works by this author on: GSW Google Scholar José-Abel Flores José-Abel Flores 2Departamento de Geología, Facultad de Ciencias, Universidad de Salamanca, Spain email: flores@usal.es Search for other works by this author on: GSW Google Scholar Micropaleontology (2006) 52 (5): 477–481. https://doi.org/10.2113/gsmicropal.52.5.477 Article history received: 21 Aug 2006 accepted: 11 Sep 2006 first online: 06 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Carlos Lancis, José-Abel Flores; A new biostratigraphically significant calcareous nannofossil species in the Early Pliocene of the Mediterranean. Micropaleontology 2006;; 52 (5): 477–481. doi: https://doi.org/10.2113/gsmicropal.52.5.477 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyMicropaleontology Search Advanced Search Abstract Here we describe Reticulofenestra cisnerosii nov. sp. a rounded species of "Reticulofenestrid" with a well defined stratigraphic distribution in the Mediterranean Neogene. The first occurrence of this new taxa is placed in the middle part of subchron Thvera (C3n4n); in the subzone CN10b (Okada and Bukry 1980); and the last occurrence is observed into the subchron C3n1r, middle part of subzone CN 11a (Okada and Bukry 1980), just before the regular record of Discoaster asymmetricus. In the region studied, this species is linked with warm, moderately saline and relatively fertile waters. This species has also been observed in the equatorial Pacific. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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