Enigmatic organisms preserved in early Ordovician macroborings, western Utah, USA

被引:2
作者
Benner, Jacob S. [1 ]
Ekdale, Allan A. [2 ]
de Gibert, Jord M. [3 ]
机构
[1] Tufts Univ, Dept Geol, Medford, MA 02155 USA
[2] Univ Utah, Dept Geol & Geophys, Salt Lake City, UT 84112 USA
[3] Univ Barcelona, Dept Estratigrafia Paleontol Geociencies Marines, Barcelona 08028, Spain
来源
CURRENT DEVELOPMENTS IN BIOEROSION | 2008年
关键词
Bioerosion; macroboring; hardground; Ordovician Bioerosion Revolution; Fillmore Formation;
D O I
10.1007/978-3-540-77598-0_3
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Macroborings in the Lower Ordovician Fillmore Formation, western Utah, USA, occasionally contain fossil remains of enigmatic organisms. In the most complete specimens a common morphology can be observed. The calcified body wall of the animal is vase-shaped, mimicking the shape of the boring itself. An ovoid body leads Lip to a neck that contains either a single or double cylinder near the aperture of the boring. The incomplete preservation of the specimens is not sufficient to identify the biological affinity of the organism at this time, but a review of potential groups is warranted. While Such groups as barnacles, bivalves, mitrates, and a host of worm-like forms are potential boring inhabitants, none fit what is known of the morphology of the specimens from Utah. Regardless, recognition and future identification of these animals will lead to a greater understanding of complex hardground trophic system,; during the Ordovician Bioerosion Revolution.
引用
收藏
页码:55 / +
页数:3
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