首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Late Paleozoic microfaunas in the pebbles of the Podlipoglav conglomerate, Central Slovenia
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Late Paleozoic microfaunas in the pebbles of the Podlipoglav conglomerate, Central Slovenia

机译:斯洛文尼亚中部Podlipoglav Conglomerate的鹅卵石晚期古生代微荷

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摘要

The Paleozoic conglomerate at Podlipoglav in the transitional area between the External and Internal Dinarides of Slovenia contains limestone pebbles that have been examined micropaleontologically. The recovered conodont faunas are marked by the obvious absence of shallow-water taxa. The Lower to Middle Devonian faunas are characterized by relatively abundant polygnathids that are assigned to the Emsian and early Eifelian excavatus-nothoperbonus, laticostatus and costatus Zones. The Pennsylvanian conodont faunas contain relatively deep-water Neolochriea or gondolellids indicating an early Bashkirian and Moscovian age. A presence of the radiolarian species Pseudoalbaillella nodosa suggests a deep-water setting during the early Moscovian and it is the oldest yet-reported albaillellid finding in Central Europe.
机译:在斯洛文尼亚的外部和内部二导物之间的过渡区域的Podlipoglav的古生代群含有石灰石鹅卵石在微创上被检查。 回收的康诺顿动物群是明显的浅水分类群。 较低的中域德文尼亚·群族的特征是相对丰富的多功能体,分配给Emsian和早期的Ecavatubatus-nothoperbonus,Laticostatus和Costatus区。 宾夕法尼亚州康诺特动物群含有相对深水的NeoLochriea或宫殿,表明Bashkirian及莫斯科夫时代早期。 在莫斯科夫早期的莫斯科夫期间存在深水环境,玉米氏菌,尤其是欧洲中部最古老但阿巴布拉的发现,这是一个深水环境。

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