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Taphonomy of exceptionally preserved crustaceans from the Upper Carboniferous of southeastern Ireland

机译:来自爱尔兰东南部上石炭统的特殊保存的甲壳类动物的音系

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摘要

The Castlecomer Fauna, a Konservat-Lagerstatte from the Upper Carboniferous of Ireland, is dominated by two species or exceptionally preserved spinicaudatan conchostracan branchiopod crustaceans; over 300 articulated specimens are known from short lengths of core from two boreholes. The spinicaudatans were entombed at various angles to bedding in thin event beds deposited in a paralic environment. Cuticle is the only tissue represented. The fossils are essentially two-dimensional as specimens collapsed following decay-induced loss of the structural strength of the cuticle. Some three-dimensionality was retained, however, as clay-grade material, probably sediment, infiltrated the carapace during or after burial, preventing the valves from being compacted to the same plane as the body of the specimen. Cuticle-lined voids created by decay of the labile tissues (notably within the tubelike antennal rami) were lined or infilled by authigenic clay minerals that were subsequently metamorphosed. The antennae, mandibles, distal parts of the claspers, and the telson are preserved in excellent detail, often retaining all or most of their original relief. Other anatomical features (antennal protopods, head, proximal part of claspers, trunk appendages) are usually preserved in two dimensions, either as a film of carbon. or a dark-colored stain. The antennules, maxillules, and maxillae are rarely preserved. Decay experiments confirm that this variation reflects differences in the recalcitrance (thickness and degree of sclerotization) of the cuticle that covered different parts of the body. Complete decay of certain appendages precedes appreciable deterioration in the morphology of others. Some of the disparity exhibited by exceptionally preserved fossil arthropods is likely to be taphonomic rather than biological in origin.
机译:来自爱尔兰上石炭纪的Konservat-Lagerstatte的Castlecomer动物区系,主要由两个物种或保存得非常好的棘金龟属conchostracan branchiopod甲壳类动物组成。从两个钻孔的短岩心中,已知有300多个关节标本。 Spinicaudatans以各种角度被包埋在paralic环境中沉积的薄事件床中。表皮是唯一代表的组织。化石本质上是二维的,因为标本在腐烂诱导的表皮结构强度损失之后坍塌。但是保留了某些三维尺寸,因为在埋葬期间或之后,粘土级材料(可能是沉积物)渗入了甲壳,从而阻止了瓣膜被压紧到与标本主体相同的平面上。由不稳定组织的腐烂产生的表皮衬里的空隙(特别是在管状触角罗姆内)被自成因的粘土矿物衬里或填充,这些粘土矿物随后被变质了。触角,下颌骨,锁骨的远端和电话被精心保存,经常保留其全部或大部分原始浮雕。其他解剖特征(前足突足,头部,锁骨近端,躯干附属物)通常以二维形式保存,或者以碳膜的形式保存。或深色污渍。腱,上颌和上颌很少被保存。衰变实验证实,这种变化反映了覆盖身体不同部位的角质层的顽固性(厚度和硬化程度)的差异。某些附件的完全腐烂先于其他附件的形态显着恶化。保存异常的化石节肢动物所表现出的某些差异可能是同源的,而不是生物学的。

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