首页> 外文期刊>Geologie en Mijnbouw >Stratigraphy of the upper Vijlen Member (Gulpen Formation; Maastrichtian) in northeast Belgium, the southeast Netherlands and the Aachen area (Germany), with special reference to belemnitellid cephalopods
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Stratigraphy of the upper Vijlen Member (Gulpen Formation; Maastrichtian) in northeast Belgium, the southeast Netherlands and the Aachen area (Germany), with special reference to belemnitellid cephalopods

机译:比利时东北部,荷兰东南部和亚琛地区(德国)的上维赫伦成员(古尔彭组;马斯特里赫蒂安)地层,特别提到了贝氏类头足类动物

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Recent studies have demonstrated the complex depositional history of the Vijlen Member (Gulpen Formation) in the Maastricht-Aachen-Liege area, on which synsedimentary tectonics had a profound impact, in conjunction with regressive and transgressive episodes, the oldest portion of this member being preserved only locally, within channel-like structures. Our reinterpretation of the Vijlen Member, here presented, is at variance with current belemnite stratigraphy. To account for incongruities, reworking of belemnites is here proposed as a typical feature during Vijlen Member deposition. A renewed study of belemnites on the basis of these new data suggests that intervals 4-6 of the Vijlen Member are of late Maastrichtian age. With respect to the mean values of populations of Belemnitella junior Nowak and Belemnitella lwowensis Naidin, Vijlen Member intervals 4-5 are coeval with the Spyridoceramus tegulatus/Belemnitella junior Zone (sensu germanico), whereas at least the upper portion of interval 6 is correlatable with the basal Tenuipteria argentea/Belemnitella junior Zone (sensu germanico). Although reworking of belemnites appears to have been a common feature, this cannot be properly substantiated without additional geochemical analyses of individual guards. For this reason, we refrain from proposing a biostratigraphic zonation of the Vijlen Member based on belemnites. Alternatively, scaphitid ammonites might be used to subdivide this member, because species such as Acanthoscaphites (Acanthoscaphites) tridens (Kner), A. (Euroscaphites) varians blaszkiewiczi Jagt, Kennedy & Machalski, Hoploscaphites constrictus (J. Sowerby), H. tenuistriatus (Kner) and Hoploscaphites sp. have been recorded. The last-named taxon represents an interspecies hybrid between the North American Jeletzkytes dorfi Landman & Waage and an unidentified subspecies of the endemic European lineage of H. constrictus, allowing correlation of the lower portion of Vijlen Member interval 6 with the Hoploscaphites birkelundae Zone of the United States Western Interior
机译:最近的研究表明,马斯特里赫特-亚琛-列日地区的维伊伦成员(古尔彭组)的沉积历史很复杂,同沉积构造对它产生了深远的影响,同时还伴有渐进性和海侵性事件,该成员的最老部分得到了保存。仅局部存在于类似通道的结构中。我们对这里的维杰伦成员的重新解释与当前的贝莱芒特地层学有所不同。为了解决不一致问题,在此建议对贝伦尼特斯进行重新加工,作为维杰伦会员沉积期间的典型特征。根据这些新数据对贝伦尼特进行的新研究表明,维伊伦成员的4-6岁年龄段属于马斯特里赫特时代晚期。关于初生Belemnitella初生Nowak和lewowensis Naidin的种群平均值,Vijlen成员区间4-5与Spyridoceramus tegulatus / Belemnitella junior Zone(sensu germanico)相当,而至少区间6的上部与基底的Tenuipteria argentea / Belemnitella junior Zone(sensu germanico)。尽管贝伦尼特犬的返修似乎是一个共同的特征,但如果不对个别警卫人员进行额外的地球化学分析,就无法正确证实这一点。因此,我们不建议基于贝尼尼特对维伊伦成员进行生物地层划分。或者,可以使用鹰嘴豆科的am虫来细分该成员,因为物种有刺can(Acanthoscaphites)tridens(Kner),A。 Kner)和Hoploscaphites sp。已被记录。姓氏上的分类单元代表了北美Jeletzkytes dorfi Landman&Waage与欧洲地方性血统H. constrictus的一个不明亚种之间的种间杂种,使Vijlen成员区间6的下部与该种的Hoploscaphites birkelundae区相关联。美国西部内政

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