{"refrec":{"BRefID":220017,"RR":"<b>Casier, J.-G.; Préat, A.</b> (1990). Sédimentologie et Ostracodes de la Limite Eifelien-Givetien à Resteigne (Bord Sud Du Bassin de Dinant, Belgique). <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 60</i>: 75-105","BEntID":211750,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 60</i>: 75-105","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Casier, J.-G.; Préat, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Casier, J.-G.; Préat, A.","Englishabstract":"The global cyclic succession of the microfacies from the Upper Eifelian to Lower Givetian times shows evidence of shallowing from deeper settings, unaffected by storm-reworking, into «proximal» above storm wave base settings, near a shoreline coast. This overall regressive progradational megasequence indicates that deposition could have occurred on a ramp setting without any kind of continuous rims and-or typical lagoonal facies behind them. This general upward-coarsening progradational evolution corresponds probably to a phase of reduced sea-level rise or stillstand on the top of which the ramp setting has evolved into a carbonate progradational accretionnary platform. Forty-one ostracod species are reported and twenty-four described from the Hanonet Formation and from the base of the Trois-Fontaines Formation of the Resteigne quarry. Sixteen are known mainly from Germany and Poland and five of them are closely related to well established species. Sixteen species are placed in open nomenclature, three of which are new, and eight are comparable with previously described data. <i>Aparchites resteignensis</i> n.sp. is described in detail. The ostracod fauna indicates a shallow marine environment and an increase of water agitation near the Eifelian/Givetian boundary.","AbstractOtherLang":"L'analyse des couches de transition Eifelien-Givetien de Resteigne permet de définir trois zones de faciès peu profonds appartenant à une rampe mixte de faible pente, sans barrière récifale ou autre. La succession de ces trois zones met en évidence une mégaséquence d'accrétion littorale traduisant à la fois une diminution progressive de la bathymétrie et une augmentation importante de l'énergie. La distribution de cette dernière est entièrement déterminée par les positions respectives de zones d'action des vagues normales et des vagues de tempêtes. L'évolution de la dynamique sedimentaire au terme de l'accrétion littorale correspond au passage d'un système mixte de rampe terrigène carbonatée à une plate-forme carbonatée stable. Quarante et une espèces d'Ostracodes sont reconnues dans la Formation d'Hanonet et dans la base de la Formation de Trois-Fontaines. Vingt-cinq sont décrites. Seize espèces sont déjà connues principalement d'Allemagne et de Pologne et cinq sont rapprochées d'espèces déjà décrites. Huit autres espèces sont placées en nomenclature ouverte dont trois nouvelles et huit comparées à des espèces déjà décrites. Aparchites resteignensis n.sp. est fondée. Les associations d'Ostracodes indiquent également un milieu marin franc peu profond et un accroissement de l'agitation des eaux au niveau de la limite des étages Eifelien et Givetien.","BibLvlCode":"AS","StandardTitle":"Sédimentologie et Ostracodes de la Limite Eifelien-Givetien à Resteigne (Bord Sud Du Bassin de Dinant, Belgique)","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":"Microfacies, mixed ramp, Ostracods, Eifelian, Givetian, Paleoecology, Microfaciès, Rampe mixte, Ostracodes, Eifelien, Givetien, Paléoécologie. 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