Large diploporitan thecal attachment structures on diploporitan thecae: An uncommon encrustation relationship involving stalked echinoderms from the Silurian of the Cincinnati Arch region, eastern midcontinental USA

IF 1.7 3区 地球科学 Q2 PALEONTOLOGY
James R. Thomka, Thomas E. Bantel, Donald L. Bissett, Drew A. Billups
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Abstract

Holocystitid diploporitans (Echinodermata) are abundant within the middle Silurian (Wenlock: Sheinwoodian) Massie Formation of southeastern Indiana, USA. Diploporitan thecae are commonly encrusted by a variety of organisms, including the attachment structures of crinoids; however, no diploporitan aboral thecal attachments have previously been described in detail as encrusters on co-occurring diploporitan thecae. Herein, we describe thecae of that are encrusted by large discoidal attachment structures attributable to undetermined holocystitid diploporitans. The thecal attachment structures are discoidal, multi-plated, pore-bearing, and characterized by circular central depressions floored by flat platforms — a morphology that is identical to that of diploporitan attachments described from a laterally continuous hardground surface at the same locality. These encrusted specimens are significant because they demonstrate that (1) encrusting diploporitans were capable of developing identical aboral attachment morphologies when encountering both hardgrounds and sufficiently large bioclasts in softgrounds; and (2) encrusted diploporitan thecae were capable of remaining articulated long enough and in a sufficiently stable position to serve as substrata for large thecal attachments. Taken collectively, holocystitid diploporitans were characterized by greater aboral morphological plasticity and resistance to disarticulation than generally recognized.
双齿蜥趾甲上的大型双齿蜥趾甲附着结构:美国中洲东部辛辛那提拱地区志留纪棘皮动物的一种不常见的包壳关系
在美国印第安纳州东南部的志留纪中期(文洛克:Sheinwoodian)马西地层(Massie Formation)中,有大量棘皮动物(Holocystitid diploporitans)。Diploporitan 趾通常被多种生物所包壳,其中包括棘皮动物的附着结构;然而,以前没有详细描述过在共生的 diploporitan 趾上作为包壳的 diploporitan 口鳞附着物。在这里,我们描述了被巨大的盘状附着结构包壳的双壳类鳞甲,这些附着结构属于未确定的全口双壳类。螯状附着结构呈盘状,多层,有孔隙,其特征是中央有圆形凹陷,凹陷处有平整的平台--这种形态与同一地点横向连续硬地表面上的二栉水母附着物形态相同。这些包壳标本具有重要意义,因为它们证明了:(1)包壳双壳类在遇到硬地和软地中足够大的生物碎屑时,能够形成相同的口外附着形态;(2)包壳双壳类的趾骨能够保持足够长的铰接时间和足够稳定的位置,以作为大型趾骨附着的基底。综合来看,全口双壳类的口部形态可塑性和抗脱节能力比一般认为的要强。
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来源期刊
Palaeoworld
Palaeoworld PALEONTOLOGY-
CiteScore
4.00
自引率
5.90%
发文量
95
期刊介绍: Palaeoworld is a peer-reviewed quarterly journal dedicated to the study of past life and its environment. We encourage submission of original manuscripts on all aspects of palaeontology and stratigraphy, comparisons of regional and global data in time and space, and results generated by interdisciplinary investigations in related fields. Some issues will be devoted entirely to a special theme whereas others will be composed of contributed articles. Palaeoworld is dedicated to serving a broad spectrum of geoscientists and palaeobiologists as well as serving as a resource for students in fields as diverse as palaeobiology, evolutionary biology, taxonomy and phylogeny, geobiology, historical geology, and palaeoenvironment. Palaeoworld publishes original articles in the following areas: •Phylogeny and taxonomic studies of all fossil groups •Biostratigraphy, chemostratigraphy, chronostratigraphy •Palaeoecology, palaeoenvironment and global changes throughout Earth history •Tempo and mode of biological evolution •Biological events in Earth history (e.g., extinctions, radiations) •Ecosystem evolution •Geobiology and molecular palaeobiology •Palaeontological and stratigraphic methods •Interdisciplinary studies focusing on fossils and strata
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