首页> 外文期刊>Geologica Carpathica >The systematics and paleobiogeographic significance of Sub-Boreal and Boreal ammonites (Aulacostephanidae and Cardioceratidae) from the Upper Jurassic of the Bohemian Massif
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The systematics and paleobiogeographic significance of Sub-Boreal and Boreal ammonites (Aulacostephanidae and Cardioceratidae) from the Upper Jurassic of the Bohemian Massif

机译:波西米亚地块上侏罗世的亚北方和北方炸药(Aulacostephanidae和Cardioceratidae)的系统学和古生物学地理意义

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摘要

Upper Jurassic marine deposits are either rarely preserved due to erosion or buried under younger sediments in the Bohemian Massif. However, fossil assemblages from a few successions exposed in northern Bohemia and Saxony and preserved in museum collections document the regional composition of macro-invertebrate assemblages and thus provide unique insights into broad-scale distribution and migration pathways of ammonites during the Late Jurassic. In this paper, we focus on the systematic revision of ammonites from the Upper Oxfordian and Lower Kimmeridgian deposits of northern Bohemia and Saxony. The ammonites belong to two families (Aulacostephanidae and Cardioceratidae) of high paleobiogeographic and stratigraphic significance. Six genera belong to the family Aulacostephanidae (Prorasenia, Rasenia, Eurasenia, Rasenioides, Aulacostephanus, Aulacostephanoides) and one genus belongs to the family Cardioceratidae (Amoeboceras). They show that the Upper Jurassic deposits of the northern Bohemian Massif belong to the Upper Oxfordian and Lower Kimmeridgian and paleobiogeographically correspond to the German-Polish ammonite branch with the geographical extent from the Polish Jura Chain to the Swabian and Franconian Alb. Therefore, the occurrences of ammonites described here imply that migration pathway connecting the Polish Jura Chain with habitats in southern Germany was located during the Late Oxfordian and Early Kimmeridgian in the Bohemian Massif.
机译:上侏罗纪海相沉积物由于侵蚀而很少被保存,或者被埋藏在波希米亚地块的较年轻沉积物中。但是,波西米亚北部和萨克森州北部暴露出来并保存在博物馆藏品中的一些演替中的化石组合记录了大型无脊椎动物组合的区域组成,因此,对侏罗纪晚期的am石的大规模分布和迁移途径提供了独特的见解。在本文中,我们着重于对波希米亚北部和萨克森州的上牛津和下基米底吉安矿床的铵盐进行系统的修正。 mon虫属于古生物学和地层学意义重大的两个科((科和step科)。六个属属于Aulacostephanidae科(Prorasenia,Rasenia,Eurasenia,Rasenioides,Aulacostephanus,Aulacostephanoides),一个属属于Cardioceratidae(Amoeboceras)科。他们表明,北波希米亚地块的上侏罗统沉积物属于上牛津和下基米底吉安,古生物地理上对应于德国-波兰am铁矿分支,其地理范围从波兰侏罗链到斯瓦比亚和法兰克白垩纪。因此,这里描述的炸药的出现暗示了将波兰侏罗纪链与德国南部栖息地联系起来的迁移途径位于波希米亚地块的牛津晚期和基米底丁时期。

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