Trilobites of the Cranbrook Lagerstätte (Eager Formation, Cambrian Stage 4), British Columbia

IF 1.3 4区 地球科学 Q3 PALEONTOLOGY Journal of Paleontology Pub Date : 2024-03-27 DOI:10.1017/jpa.2023.89
Mark Webster, Jean‐Bernard Caron
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Abstract

The Eager Formation (Cambrian Stage 4) of the Cranbrook area, British Columbia, contains abundant, sometimes beautifully preserved, trilobites and rare non-biomineralized taxa. Trilobites were first reported just over a century ago but have received little research attention, resulting in uncertainty in the number and identity of species within the assemblage and ambiguity in the age of the fauna. The trilobites of the Eager Formation in the Cranbrook area are described herein based largely upon material collected in 2015. A minimum of eight (and perhaps up to 11) trilobite species are recognized. The four species of olenelloids (Olenellus santuccii Webster n. sp., Olenellus? schofieldi, Mesonacis eagerensis, and Wanneria cranbrookense Webster n. sp.) are by far the most abundant elements of the fauna. At least two, and perhaps as many as five, species of dorypygid are present, as are two species of “ptychoparioids”. Paucity and poor preservational quality of specimens mean that the various dorypygid and “ptychoparioid” species are left in open nomenclature. Trilobite diversity in the Cranbrook Lagerstätte is comparable to that within other Lagerstätten from Cambrian Stage 4 (Series 2) of Laurentia. The diversity and abundance of trilobites, combined with biostratinomic and trace fossil data, suggest that the assemblage is autochthonous and/or parautochthonous, and that the local environment was at least periodically able to support a “typical” benthic trilobite community. The age of the Cranbrook Lagerstätte is constrained to lie within the middle Dyeran Stage of Laurentia, within what was a substantial stratigraphic gap in the distribution of Burgess Shale-type Lagerstätten. UUID: http://zoobank.org/5beab9df-6b6a-4d6d-95e8-57057cd47a66
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不列颠哥伦比亚省克兰布鲁克拉格斯塔特(埃格地层,寒武纪第 4 阶段)的三叶虫
不列颠哥伦比亚省克兰布鲁克地区的埃格地层(寒武纪第 4 阶段)包含大量有时保存完好的三叶虫和罕见的非生物矿化类群。三叶虫在一个多世纪前首次被报道,但很少受到研究人员的关注,导致该集合体中物种的数量和身份不确定,动物群的年龄也不明确。本文描述的克兰布鲁克地区埃格地层的三叶虫主要基于 2015 年采集的材料。至少确认了 8 个(可能多达 11 个)三叶虫物种。四种橄榄石(Olenellus santuccii Webster n. sp.、Olenellus? schofieldi、Mesonacis eagerensis 和 Wanneria cranbrookense Webster n. sp.)是迄今为止动物群中最丰富的成分。至少有两种(可能多达五种)多刺蝇,还有两种 "tychoparioids"。由于标本数量稀少且保存质量较差,因此各种dorypygid和 "tychoparioid "物种的命名都没有定论。克兰布鲁克采集站的三叶虫多样性与劳伦西亚寒武纪第 4 阶段(系列 2)其他采集站的三叶虫多样性相当。三叶虫的多样性和丰度,结合生物地层学和痕量化石数据,表明该集合体是自生和/或副自生的,当地环境至少能够定期支持一个 "典型的 "底栖三叶虫群落。克兰布鲁克拉格斯塔特的年代被推定为劳伦提亚的戴尔安中期,位于伯吉斯页岩型拉格斯塔特分布的一个巨大地层缺口内。UUID: http://zoobank.org/5beab9df-6b6a-4d6d-95e8-57057cd47a66
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来源期刊
Journal of Paleontology
Journal of Paleontology 地学-古生物学
CiteScore
2.80
自引率
7.10%
发文量
94
审稿时长
6-12 weeks
期刊介绍: The Journal of Paleontology publishes original articles and notes on the systematics, phylogeny, paleoecology, paleogeography, and evolution of fossil organisms. It emphasizes specimen-based research and features high quality illustrations. All taxonomic groups are treated, including invertebrates, microfossils, plants, vertebrates, and ichnofossils.
期刊最新文献
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