{"refrec":{"BRefID":287807,"RR":"<b>Amorosi, A.; Antonioli, F.; Bertini, A.; Marabini, S.; Mastronuzzi, G.; Montagna, P.; Negri, A.; Rossi, V.; Scarponi, D.; Taviani, M.; Angeletti, L.; Piva, A.; Vai, G.B.</b> (2014). The Middle–Upper Pleistocene Fronte Section (Taranto, Italy): an exceptionally preserved marine record of the Last Interglacial. <i>Global Planet. Change 119</i>: 23-38. <a href=\"https://dx.doi.org/10.1016/j.gloplacha.2014.04.007\" target=\"_blank\">https://dx.doi.org/10.1016/j.gloplacha.2014.04.007</a>","BEntID":279832,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Global Planet. Change 119</i>: 23-38. <a href=\"https://dx.doi.org/10.1016/j.gloplacha.2014.04.007\" target=\"_blank\">https://dx.doi.org/10.1016/j.gloplacha.2014.04.007</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Amorosi, A.; Antonioli, F.; Bertini, A.; Marabini, S.; Mastronuzzi, G.; Montagna, P.; Negri, A.; Rossi, V.; Scarponi, D.; Taviani, M.; Angeletti, L.; Piva, A.; Vai, G.B.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Amorosi, A. <i>et al.</i>","Englishabstract":"The Fronte Section, a well-exposed stratigraphic succession from southern Italy (Taranto area), provides an uninterrupted marine sedimentary record of MIS 5e. At this location, a highly expanded (8.5 m thick) stratigraphic succession, unconformably overlying Middle Pleistocene marine clay deposits, provides evidence for sea-level fluctuations during the Last Interglacial. An integrated study of Fronte Section, including facies analysis, detailed macrofaunal and meiofaunal characterization, and sequence stratigraphy, is presented. The occurrence of <i>Persististrombus latus</i> (= <i>Strombus bubonius</i>) and other warm-water indicators (“<i>Senegalaise</i>” – “<i>Senegalian</i>” – guests of Gignoux, 1913), together with the presence of the dinocyst <i>Polysphaeridium zoharyi</i> and ten U-series dates on <i>Cladocora caespitosa</i> samples, permit an unequivocal MIS 5e age assignment to the upper part of the study succession. Above a stratigraphic unconformity marked by the boring coastal-lagoonal bivalve <i>Pholas dactylus</i>, the MIS 5e succession displays a first transgressive suite of brackish to shallow-marine deposits. These latter include highly fossiliferous muds rich in <i>C. caespitosa</i>, overlain by a fossil-rich calcarenite, 2 m-thick, yielding warm-water “Senegalian” mollusks. Above this prominent stratigraphic marker (regionally called <i>panchina</i>), which is interpreted to represent a short-lived phase of sea-level stillstand or gentle fall during MIS 5e, renewed transgression took place, leading to the accumulation of middle-outer shelf muds, about 5 m thick. The maximum flooding zone is clearly identified on the basis of the turnaround from a deepening-up to a shallowing-up trend. The upper part of Fronte Section records a second fossil-rich, sublittoral calcarenite containing warm-water mollusks, which is interpreted to reflect the subsequent phase of sea-level highstand, likely correlative with the MIS 5e plateau.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"The Middle–Upper Pleistocene Fronte Section (Taranto, Italy): an exceptionally preserved marine record of the Last Interglacial","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-07 01:31:30.180311","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Last Interglacial, MIS 5e, Quaternary, sequence stratigraphy, paleoecology, Taranto, Italy","OtherDescriptors":null,"Notes":null,"AnaPub":2014,"MonPub":null,"DateUpdate":"2018-02-13","DateCreate":"2017-08-09","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000338978900002","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.gloplacha.2014.04.007"},"refs":null,"anarec":{"AnaID":287807,"PubliDate":2014,"Pagination":"23-38","XtraPublOfAnaID":null,"ISBN":null,"Volume":"119","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42934,"SerRR":"Global and Planetary Change. 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