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首页> 外文期刊>Neues Jahrbuch fur Geologie und Palaontologie. Abhandlungen >The distribution of benthic foraminifera in Cladocora caespitosa coral banks of the Veliko Jezero sediments (Mljet National Park, eastern Adriatic Sea)
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The distribution of benthic foraminifera in Cladocora caespitosa coral banks of the Veliko Jezero sediments (Mljet National Park, eastern Adriatic Sea)

机译:Veliko Jezero沉积物(Mljet国家公园,亚得里亚海东部)的Cladocora caespitosa珊瑚堤中底栖有孔虫的分布

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摘要

This paper compares distributional data of benthic foraminifera from surface sediments that were collected in 2003 and 2012 from Cladocora caespitosa coral banks in Veliko Jezero (Mljet National Park, eastern Adriatic Sea). Species composition and test preservation of benthic foraminifera provide information on the depositional history of shallow-water sediments, particularly on the source of the displaced foraminiferal tests. Two foraminiferal assemblages were identified. Peneroplids (Peneroplis pertusus and Penereplis planatus) and Elphidium crispum dominate in modern foraminiferal assemblages collected in 2012, whereas samples collected almost ten years earlier are characterized by frequent occurrences of Rosalina bradyi and Quinqueloculina sp. Our quantitative reconstruction revealed that symbiont-bearing peneroplids, foraminifera that are often associated with reef building corals, became dominant constituents over several years in this area. Taphonomic signatures of the assemblages are correlated to taxonomic units and granulometric properties of substrate sediments, indicating that taphonomic processes are crucial in defining the composition of assemblages.
机译:本文比较了2003年和2012年从Veliko Jezero(亚得里亚海东部Mljet国家公园)的Cladocora caespitosa珊瑚堤收集的地表沉积物中底栖有孔虫的分布数据。底栖有孔虫的种类组成和试验保存可提供有关浅水沉积物沉积历史的信息,尤其是有关有孔有孔虫试验来源的信息。确定了两个有孔虫的组合。在2012年收集的现代有孔虫组合中,Peneroplids(Peneroplis pertusus和Penereplisplanatus)和Elphidium crispum占主导地位,而将近十年前收集的样品的特征是频繁出现了Rosarosa bradyi和Quinqueloculina sp。我们的定量重建结果表明,在过去的几年中,通常与造礁珊瑚有关的带有共生生物的有节肢动物(有孔虫)已成为该地区的主要成分。组合的音标特征与底物沉积物的分类单位和粒度特性相关,这表明,拼音过程对于定义组合物的组成至关重要。

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