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Taxonomic revision of Late Triassic 'Lithocodium aggregatum Elliott' (Northern Calcareous Alps, Austria)

机译:分类改革后期三叠纪“Lithocodium Elliott”(北钙质阿尔卑斯山,奥地利)

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摘要

Late Triassic forms of Lithocodium aggregatum Elliott are revised taxonomically based on thin-section material from the Late Rhaetian of Mount Steinplatte, Tyrol, and Adnet, Salzburg. They are interpreted as the boring galleries (chambers and canals) of sponges (ichnogenus Entobia), excavating into microbial-oncoidal crusts and framebuilders. From the roof of these chambers, branching canals exhibiting successively decreasing diameters transect the crusts, while pioneering filaments bored downwards from the chamber bases into the bioclastic substrate. The traces of this activity are preserved as a micritic network. Irregular globular bodies displaying a thin microcrystalline wall occur inside the cement-filled chambers. These are interpreted as remnants of the former sponges (ectosome). The occurrence of abundant boring sponges in Late Triassic times could be linked to the biological crisis postulated around the Triassic-Jurassic boundary.
机译:基于Salzburg山泰特罗尔和Adnet的晚Rhaetian的薄剖面材料,基于薄剖面材料进行分类论期的薄晶二极管埃利特的晚期三叠系形式。 它们被解释为海绵(InChnognus enobia)的无聊画廊(腔室和运河),挖掘成微生物外壳和框架。 从这些腔室的屋顶,表现出连续减小的直径的分支分配器会横切地壳,同时从腔室碱向向下钻孔到生物旋气基材上的开创性长丝。 此活动的迹线保留为微距网络。 显示薄微晶壁的不规则球体发生在填充水泥的腔室内。 这些被解释为前海绵(Ectosome)的残余物。 晚期三叠纪时期丰富的镗孔海绵的发生可能与围绕三叠系侏罗纪边界的生物危机相关联。

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