西西里新生代晚期埃托比亚的自然铸型

IF 1.6 3区 地球科学 Q2 GEOLOGY
V. Garilli, Á. Dávid, S. Dominici
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引用次数: 1

摘要

与其他遗迹化石一样,1837年对Entobia Bronn遗迹化石的研究,归因于钻孔海绵的活动,有助于了解埋藏过程和重建古环境。在这里,我们描绘了西西里岛的一个多样化的Entobia群落,这是第一个在这个地中海岛屿上描述的群落,基于对保存完好的自然铸件的发现。所研究的关联由七个ichnotaxa、Entobia cateniformis、E.cateniforms form A、E.geometrica、E.laquea、E?巨口E.ovula E?来自西西里岛西北部的Altavilla Milicia和Sferracavallo晚新生代遗址的悖论。Aragoniotic双壳类,主要是类性病,是负责产生这些ichnotaxa的无聊生物的基质。Entobia也被发现与由多毛类产生的无聊的Caulostrepsis taeniola的自然模型有关。湖相学和壳床埋藏学表明,所调查的矿床是在低沉积速率的条件下形成的;沉积后过程涉及有利于保存方解石壳的化学条件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
NATURAL CASTS OF ENTOBIA FROM THE LATE CAENOZOIC OF SICILY
As with other ichnofossils, the study of the ichogenus Entobia Bronn, 1837, attributed to the activity of boring sponges, is useful to understand taphonomic processes and reconstruct paleoenvironments. Here we delineate a diverse Entobia assemblage from Sicily, the first described from this Mediterranean island, based on the discovery of well-preserved natural casts. The studied association is represented by seven ichnotaxa, Entobia cateniformis, E. cateniformis form A, E. geometrica, E. laquea, E. ?megastoma, E. ovula, E. ?paradoxa, which come from the late Caenozoic sites of Altavilla Milicia and Sferracavallo, in north-western Sicily. Aragonitic bivalves, mostly veneroids, served as substrate for the boring organisms responsible of producing these ichnotaxa. Entobia was also found associated with natural casts of the boring Caulostrepsis taeniola, produced by polychaetes. Ichnology and shell-bed taphonomy indicates that investigated deposits formed in conditions of low rate of sedimentation; post depositional processes involved chemical conditions favorable to the preservation of calcite shells.
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来源期刊
CiteScore
3.60
自引率
4.30%
发文量
28
审稿时长
>12 weeks
期刊介绍: The Rivista Italiana di Paleontologia e Stratigrafia was founded in 1895. It publishes original papers dealing with all fields of paleontology and of stratigraphy, from Italy and the Mediterranean to the Tethys, as well across the globe from China to North America.
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