<rdf:RDF xmlns:dwc="http://rs.tdwg.org/dwc/terms/" xmlns:cnt="http://www.w3.org/2011/content#" xmlns:spm="http://rs.tdwg.org/ontology/voc/SpeciesProfileModel" xmlns:bibo="http://purl.org/ontology/bibo/" xmlns:sdo="http://schema.org/" xmlns:trt="http://plazi.org/vocab/treatment#" xmlns:rdfs="http://www.w3.org/2000/01/rdf-schema#" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:xsd="http://www.w3.org/2001/XMLSchema#" xmlns:fabio="http://purl.org/spar/fabio/" xmlns:cito="http://purl.org/spar/cito/" xmlns:sdd="http://tdwg.org/sdd#" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dwcFP="http://filteredpush.org/ontologies/oa/dwcFP#">
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        <dc:title>The Lower Pliocene marine gastropods of Santa Maria Island, Azores: Taxonomy and palaeobiogeographic implications</dc:title>
        <dc:creator>Sacchetti, Claudia</dc:creator>
        <dc:creator>Landau, Bernard</dc:creator>
        <dc:creator>Ávila, Sérgio P.</dc:creator>
        <rdf:type rdf:resource="fabio:JournalArticle"/>
        <bibo:journal>Zootaxa</bibo:journal>
        <dc:date>2023</dc:date>
        <bibo:pubDate>2023-05-24</bibo:pubDate>
        <bibo:volume>5295</bibo:volume>
        <bibo:issue>1</bibo:issue>
        <bibo:pageStart>1</bibo:pageStart>
        <bibo:pageEnd>150</bibo:pageEnd>
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        <dwc:box>[151,288,798,825]</dwc:box>
        <dwc:class>Gastropoda</dwc:class>
        <dwc:family>Fasciolariidae</dwc:family>
        <dwc:genus>Fusinus</dwc:genus>
        <dwc:kingdom>Animalia</dwc:kingdom>
        <dwc:order>Neogastropoda</dwc:order>
        <dwc:pageId>69</dwc:pageId>
        <dwc:pageNumber>70</dwc:pageNumber>
        <dwc:phylum>Mollusca</dwc:phylum>
        <dwc:rank>species</dwc:rank>
        <dwc:species>undetermined</dwc:species>
    </rdf:Description>
    <rdf:Description rdf:about="http://treatment.plazi.org/id/03CF879C2C570900FF1DFCFEFBF6722F#section_1">
        <rdf:type rdf:resource="spm:InfoItem"/>
        <spm:hasContent>  Plate 4 L</spm:hasContent>
    </rdf:Description>
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        <spm:hasContent>  Santa Maria material examined.Maximum height 51.0 mm, width 2.4 mm. One specimen from LNEGcollection (unnumbered), Ponta do Norte lighthouse, Santa Maria Island, Azores, Touril Complex, Lower Pliocene.</spm:hasContent>
    </rdf:Description>
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        <rdf:type rdf:resource="spm:InfoItem"/>
        <spm:hasContent>  Description.Shell large, solid, fusiform, with moderate height conical spire. Protoconch missing. Six convex teleoconch whorls preserved. Surface on first four whorls eroded. Penultimate whorl convex, with periphery mid-whorl and suggestion of weak spiral sculpture. Last whorl broadly convex moderately constricted at base, with broad long siphonal fasciole; fine spiral sculpture above base, strong spiral cord on fasciole. Aperture ovate, outer lip incomplete, but without sign of labial varix.</spm:hasContent>
    </rdf:Description>
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        <spm:hasContent>  Discussion.A single large specimen in the LNEG collection with dorsum embedded in matrix, labelled  Euthriaaf.  magnaBellardifrom Ponta do Norte lighthouse, is, in our opinion, not a  Euthria Gray, 1850(Superfamily Buccinoidea) based on its very broad siphonal fasciole that is not recurved, as it is in the genus  Euthria.The siphonal canal and tip of the fasciole are covered in matrix so we cannot confirm if the fasciole curves around a pseudoumbilicus as it does in many  Fusinusspecies.Moreover, the outer lip is not thickened as it is in the genus  Euthria. We have assigned it the subfamily Fusininae Wrigley, 1927, genus  Fusinus Rafinesque, 1815tentatively, as we cannot match it to any European or West African fossil or extant species. However, it is somewhat reminiscent of another odd species,  Fusinus clavilithoidesLandau, Harzhauser, B̧y̧kmeriç &amp; Breitenberger, 2016 from the middle Miocene eastern Mediterranean KaramanBasin of Turkeybut differs in having strong cords on the siphonal fasciole, lacking in the Turkish species. In their discussion, Landau et al. (2016: 223)considered the subfamily Peristerniinae Tryon, 1880for their Turkish specimen, but members of that subfamily have columellar folds. The columellar edge is only partially exposed in the Santa Maria specimen but no signs of folds are seen.</spm:hasContent>
    </rdf:Description>
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        <spm:hasContent>  Distribution.Lower Pliocene: Atlantic: Santa Maria Island, Azores(this paper).</spm:hasContent>
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