{"refrec":{"BRefID":234231,"RR":"<b>Brzobohaty, R.; Nolf, D.</b> (1996). Otolithes de myctophidés (poissons téléostéens) des terrains tertiaires d'Europe: révision des genres <i>Benthosema, Hygophum, Lampadena, Notoscopelus</i> et <i>Symbolophorus</i>. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 66</i>: 151-176","BEntID":225915,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 66</i>: 151-176","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Brzobohaty, R.; Nolf, D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Brzobohaty, R.; Nolf, D.","Englishabstract":"Twenty-nine species of \"non-<i>Diaphus</i>\" myctophids are recorded from the Tertiary (mainly Neogene) strata of Europe. One among them, <i>Lampadena speculigeroides</i> is new, and two species previously considered as doubtful, are revalidated: <i>Lampadena gracile</i> (SCHUBERT, 1912) and <i>Notoscopelus mediterraneus</i> (KOKEN, 1891). The bulk of our data concerns the Mediterranean realm (including the Paratethys). The history of myctophid populations in that basin can be summarised as follows. From Priabonian till Burdigalian, rich myctophid associations, dominated by the genus <i>Diaphus</i> were already represented. This genus continues to dominate the associations up to the Piacenzian. In the Burdigalian. nine \"non-<i>Diaphus</i>\" species appear, and two of them persist in the present day Mediterranean fauna. Nine species are recorded from the Langhian and four of those appeared after the Burdigalian. There are no data for the Serravallian. In the Tortonian, 11 species are known. Five among them already existed in the Langian, one does not exceed the upper boundary of the Tortonian, two persist till the Pliocene, and three persist till present. For the Messinian, otoliths are known only from skeletons with otoliths in situ (six genera, including <i>Diaphus</i>), and preservation quality of these otoliths is poor. Although, precise relationships between otolith-based and skeleton-based species are difficult to evaluate, the Messinian skeletons do not include any myctophic genus that is not known by otoliths from the Tortonian or the Pliocene. The Zanclian association counts 12 species of which six already existed in the Tortonian. Among the six new ones, five are Recent, but only two of them live in the present day Mediterranean. All taxa who in the present day fauna are known only from outside the Mediterranean, disappeared from that basin since the end of the Zanclian. It seems that till that time, more oceanic conditions that the present-day ones prevailed in the Mediterranean. Notwithstanding the appearence of some new species at the end of the Piacenzian, it seems almost certain that the climatic deterioration and the isolation of the Mediterranean have been much more destructive for the Palaeomediterranean fauna than the Messinian salinity crisis.","AbstractOtherLang":"Vingt-neuf espèces de myctophidés \"non-<i>Diaphus</i>\" sont recensées dans les terrains tertiaires (essentiellement néogènes) d'Europe. Une d'entre elles, <i>Lampadena speculigeroides</i> est nouvelle et deux autres, considérées comme douteuses, sont revalidées: <i>Lampadena gracile</i> (SCHUBERT, 1912) et <i>Notoscopelus mediterraneus</i> (KOKEN, 1891). C'est surtout dans le Bassin méditerranéen (incluant la Paratéthys) que la plupart des données ont été obtenues. Le peuplement en myctophidés peut y être résumé comme suit. Du Priabonien au Burdigalien, de riches associations de myctophidés, dominées par le genre <i>Diaphus</i>, étaient déjà en place; ce genre dominera d'ailleurs jusqu'au Plaisancien, mais plus dans la Méditerranée actuelle (trois espèces seulement). Au Burdigalien, sept espèces \"non-<i>Diaphus</i>\" apparaissent, dont deux actuelles. La faune langhienne compte neuf espèces, dont quatre sont apparues après le Burdigalien. Le Serravalien correspond à une lacune complète de données. Au Tortonien, on connaît une association riche de onze espèces dont cinq existaient déjà au Langhien; une ne dépasse pas la limite supérieure du Tortonien, deux persistent jusqu'au Pliocène et trois espèces actuelles apparaissent, dont deux méditerranéennes ci une extra-méditerranéenne. Au Messinien, on ne connaît que des otolithes mal conservées, associées à des squelettes (six genres, incluant <i>Diaphus</i>). Quoique l'établissement de relations précises entre les espèces établies sur des squelettes et des otolithes reste problématique, la faune messinienne ne comporte aucun genre de mycotphidé qui ne soit représenté par des otolithes tortoniennes ou pliocènes. L'association zanclienne compte douze espèces dont six existaient déjà au Tortonien. Parmi les six nouvellement apparues, cinq sont actuelles, mais deux seulement persistent dans la faune récente de la Méditerranée. A la fin du Zanclien, tous les taxa qui, dans la nature actuelle, vivent uniquement hors de la Méditerranée sont disparus. Il semble donc que jusqu'alors, des conditions plus franchement océaniques que maintenant régnaient en Méditerranée. Malgré l'apparition de quelques espèces nouvelles à la fin du Plaisancien, il parait certain que la détérioration climatique et l'isolement de la Méditerranée a, dès le Pliocène terminal, été davantage destructif pour la faune océanique paléoméditerranéenne que la crise de salinité du Messinien.","BibLvlCode":"AS","StandardTitle":"Otolithes de myctophidés (poissons téléostéens) des terrains tertiaires d'Europe: révision des genres <i>Benthosema, Hygophum, Lampadena, Notoscopelus</i> et <i>Symbolophorus</i>","OrigTitleLangCode":"fr","OrigTitleLangCodeExtended":"fre","OrigTitleLangID":22,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Myctophids, \"non-Diaphus\", Neogene, Mediterranean, Europe","OtherDescriptors":null,"Notes":null,"AnaPub":1996,"MonPub":null,"DateUpdate":"2014-08-20","DateCreate":"2014-03-14","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":234231,"PubliDate":1996,"Pagination":"151-176","XtraPublOfAnaID":null,"ISBN":null,"Volume":"66","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":64308,"SerRR":"Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. Aardwetenschappen = Bulletin de l'Institut Royal des Sciences Naturelles de Belgique. Sciences de la Terre. KBIN: Brussel.  ISSN 0374-6291","StandardTitleSer":"Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. Aardwetenschappen = Bulletin de l'Institut Royal des Sciences Naturelles de Belgique. Sciences de la Terre","ISSN":"0374-6291","AbbrevSer":"Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. 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