{"refrec":{"BRefID":233867,"RR":"<b>Donovan, S.; Jagt, J.W.M.</b> (2005). <i>Flosculichnus tectus</i>, an etched attachment scar from the Upper Cretaceous (Maastrichtian) of The Netherlands. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 75</i>: 207-210","BEntID":225552,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 75</i>: 207-210","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Donovan, S.; Jagt, J.W.M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Donovan, S.; Jagt, J.W.M.","Englishabstract":"A single example of a rosette-shaped embedment structure on the carina of a scalpellid cirripede (Bosquet Collection) from the basal portion of the Valkenburg Member (Maastricht Formation) at St Pietersberg (Maastricht, southern Limburg, The Netherlands) is described as a new ichnogenus and species, <i>Flosculichnus tectus</i>. It differs from other resetted traces in calcareous hard substrates, which consist of slender, radiating borings, in having a scalloped, cyclic structure surrounding a central depression. The most probable producing organisms are either an unidentified, sessile, unmineralised invertebrate or, perhaps more likely, a scalpellid cirripede.","AbstractOtherLang":"Dans la collection Bosquet, sur la carène d'un cirripède scalpellidé se trouve une structure d'enfouissement, en forme de rosette. Ce cirripède provient de la partie basale du Valkenburg Member (Formation de Maastricht) de la Montagne Saint-Pierre (Maastricht, Zuid-Limburg, Pays-Bas). Cette structure est décrite comme <i>Flosculichnus tectus</i>, représentant un nouvel ichnogenre et une nouvelle espèce. D'autres traces connues en formes de rosettes dans des substrats calcaires dures forment de fines perforations radiaires. <i>F. tectus</i> consiste en une structure écaillée, cyclique, entourant une dépression centrale. L'origine de cette structure est ou bien un invertébré marin non-identifié, sessile, non minéralisé, ou bien - et ceci est plus probable - un cirripède scalpellidé.","BibLvlCode":"AS","StandardTitle":"<i>Flosculichnus tectus</i>, an etched attachment scar from the Upper Cretaceous (Maastrichtian) of The Netherlands","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2025-07-02 08:58:19.190595","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Trace fossils, embedments, new taxa, Cretaceous, Maastrichtian, The Netherlands","OtherDescriptors":null,"Notes":null,"AnaPub":2005,"MonPub":null,"DateUpdate":"2014-02-26","DateCreate":"2014-02-26","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":233867,"PubliDate":2005,"Pagination":"207-210","XtraPublOfAnaID":null,"ISBN":null,"Volume":"75","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":64308,"SerRR":"Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. 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