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Spiraloconulus suprajurassicus n. sp. - a New Benthic Foraminifer from the Late Jurassic of the Northern Calcareous Alps of Austria

机译:Spiraloconulus suprajurassicus n。 SP。 - 来自奥地利北部钙质阿尔卑斯山的侏罗纪的新的底栖传染媒线

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摘要

A new large-sized foraminifer is described as Spiraloconulus suprajurassicus n. sp. from the Kimmeridgian-Tithonian of the Northern Calcareous Alps of Austria. A further occurrence is from the Late Tithonian-Early Berriasian of Romania. It represents the third species of the genus Spiraloconulus Allemann & Schroeder, 1980 known so far from the interval Late Aalenian-Bathonian (Early Callovian?). Given its ammobaculitoid morphology, its coarsely agglutinated habitus and the preference for well-agitated external platform settings, S. suprajurassicus can be compared with S. giganteus Cherchi & Schroeder. A Middle-Late Jurassic phylogenetic lineage from S. perconigi to S. giganteus and finally S. suprajurassicus is postulated attended by an increase of complexity of the marginal zone. Spiraloconulus suprajurassicus represents a rare foraminifer in the Late Jurassic of the Northern Calcareous Alps, mostly occurring in resediments, e.g., the Barmstein Limestone.
机译:一种新的大型传染料被描述为Spiraloconulus suprajurassicus n。 SP。 来自奥地利北钙质阿尔卑斯山的Kimmeridgian-Tithonian。 进一步的发生是来自罗马尼亚的晚期的泰特尼亚早期的白蚁。 它代表了螺旋聚体的第三种种类的螺旋体和施罗德,1980年,到目前为止已达到了半夜糖 - 浴室(早期Callovian?)。 鉴于其氨基杀虫素形态,其粗凝集的栖息地和对令人兴奋的外部平台设置的偏好,Suprajurassicus可以与S.Giganteus Chrochi&Schroeder进行比较。 从S.Perconigi到S. Giganteus的中期侏罗纪系统发育谱系,最后S. suprajurassicus通过增加边际区域的复杂性的增加。 Spiraloconulus Suprajurassicus代表北方钙质阿尔卑斯山的晚期侏罗纪的罕见的传染料,大部分发生在植入中,例如,巴里斯坦石灰石。

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