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来自加拿大西部的保存异常完好的甲壳类动物揭示了隐生代寒武纪的辐射。

Exceptionally preserved crustaceans from western Canada reveal a cryptic Cambrian radiation.

机构信息

Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom.

出版信息

Proc Natl Acad Sci U S A. 2012 Jan 31;109(5):1589-94. doi: 10.1073/pnas.1115244109. Epub 2012 Jan 17.

Abstract

The early history of crustaceans is obscured by strong biases in fossil preservation, but a previously overlooked taphonomic mode yields important complementary insights. Here we describe diverse crustacean appendages of Middle and Late Cambrian age from shallow-marine mudstones of the Deadwood Formation in western Canada. The fossils occur as flattened and fragmentary carbonaceous cuticles but provide a suite of phylogenetic and ecological data by virtue of their detailed preservation. In addition to an unprecedented range of complex, largely articulated filtering limbs, we identify at least four distinct types of mandible. Together, these fossils provide the earliest evidence for crown-group branchiopods and total-group copepods and ostracods, extending the respective ranges of these clades back from the Devonian, Pennsylvanian, and Ordovician. Detailed similarities with living forms demonstrate the early origins and subsequent conservation of various complex food-handling adaptations, including a directional mandibular asymmetry that has persisted through half a billion years of evolution. At the same time, the Deadwood fossils indicate profound secular changes in crustacean ecology in terms of body size and environmental distribution. The earliest radiation of crustaceans is largely cryptic in the fossil record, but "small carbonaceous fossils" reveal organisms of surprisingly modern aspect operating in an unfamiliar biosphere.

摘要

甲壳动物的早期历史被化石保存的强烈偏见所掩盖,但以前被忽视的埋藏学模式提供了重要的补充见解。在这里,我们描述了来自加拿大西部死亡之谷组的浅海泥岩中具有中晚寒武纪年龄的多样化甲壳动物附肢。这些化石呈扁平状和碎片状的碳化外皮,但由于其详细的保存,提供了一系列系统发育和生态数据。除了前所未有的复杂、主要关节的过滤附肢外,我们还确定了至少四种不同类型的颚。这些化石共同提供了冠群鳃足类和总群桡足类和介形类的最早证据,将这些类群的范围从泥盆纪、宾夕法尼亚纪和奥陶纪追溯回来。与现存形式的详细相似性表明,各种复杂的食物处理适应的早期起源和随后的保存,包括持续了 5 亿年进化的定向下颌不对称性。与此同时,死亡之谷化石表明甲壳动物的生态学在体型和环境分布方面发生了深刻的长期变化。甲壳动物的最早辐射在化石记录中很大程度上是隐蔽的,但“小的碳化化石”揭示了具有惊人现代特征的生物体在一个陌生的生物圈中运作。

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