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首页> 外文期刊>Lethaia: An International Journal of Palaeontology and Stratigraphy >Danian cold-water corals from the Baunekule facies, Faxe Formation, Denmark: a rare taphonomic window of a coral mound flank habitat
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Danian cold-water corals from the Baunekule facies, Faxe Formation, Denmark: a rare taphonomic window of a coral mound flank habitat

机译:丹麦法克斯组Baunekule相的丹尼亚冷水珊瑚:珊瑚丘侧面生境的罕见的透汗窗

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Well-preserved cold-water corals are comparatively rare in the fossil record. This is partly due to the very low fossilization potential of the predominantly aragonitic corals but also due to the fact that coral ecosystems of deep water are a geologically young development. A Middle Danian cold-water coral mound complex is well exposed in Faxe Quarry, Denmark. The coral mounds are intercalated with bryozoan mounds of various sizes and form the Faxe Formation. The coral limestone displays large variations in diagenesis, and this complicates the palaeoecological reconstructions. However, the Baunekule facies from the Faxe Formation contain a well-preserved originally aragonitic and calcitic fauna. The aragonitic skeletons have been recrystallized to calcite during early diagenesis and the excellent preservation makes taxonomic identifications straightforward. A diverse fauna of ten scleractinian coral species, nine stylasterine coral species and seven octocoral species has been described from the Baunekule facies. The fossil fauna represents an ecological niche between the dead coral framework and coral rubble on a flank of a growing Dendrophyllia coral mound with multiple colonization events. The diversity and relative abundance of the fossil scleractinian corals are comparable to the modern settings in the NE Atlantic and Mediterranean. The distribution and diversity of the octocorals and the stylasterine corals are suggested to represent coral gardens as described from modern setting in the NE Pacific. The presence of a diverse and abundant stylasterine fauna suggests a stable palaeoenvironment, probably in a bathymetric depth range of 200-400 metre.
机译:保存完好的冷水珊瑚在化石记录中相对较少。这部分是由于主要为阿拉贡语的珊瑚的化石潜力非常低,也归因于深水珊瑚生态系统在地质上是年轻的发展。丹麦的Faxe Quarry暴露了一个丹尼亚中部冷水珊瑚丘群。珊瑚丘与各种大小的苔藓虫丘嵌插在一起,形成了Faxe组。珊瑚石灰岩在成岩作用中表现出很大的差异,这使古生态重建变得复杂。但是,来自传真e组的Baunekule相包含了保存完好的原始文石和钙化动物群。早期成岩过程中,文石骨架已重结晶为方解石,出色的保存性能使分类学鉴定变得简单。从Baunekule相中描述了由10个Scleractinian珊瑚种类,9个Stasterasterine珊瑚种类和7个octocoral种类组成的不同动物区系。化石动物群代表了死去的珊瑚骨架和生长着的树突藻珊瑚丘侧面上的珊瑚瓦砾之间的生态位,该珊瑚丘具有多个定殖事件。巩膜化石珊瑚的多样性和相对丰度可与东北大西洋和地中海的现代环境相媲美。八角珊瑚和金针石珊瑚的分布和多样性被认为代表了东北太平洋现代环境中所描述的珊瑚花园。多样而丰富的金鸡汀动物区系的存在表明古环境稳定,大概在200-400米的测深范围内。

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