西澳大利亚坎宁盆地南部Barnicarndy 1地层井早奥陶世三叶虫

Patrick M. Smith, Heidi J. Allen
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摘要

摘要 本文描述了从西澳大利亚坎宁盆地巴尼卡迪 1 号钻孔岩芯中提取的早奥陶世(特雷马多克世至弗洛亚世)南比特地层中的 23 个三叶虫类群。其中包括一个新属(Veeversaspis gen:Asaphellus zheni sp. nov.、Madiganaspis lauriei sp. nov.、Norasaphus (Norasaphus) jagoi sp. nov.、Rodingaia leggi sp. nov.、Sanbernardaspis excalibur sp. nov.和 Veeversaspis jelli gen. et sp. nov.该动物群可分为三个不同地层的组合,即 Apatokephalus sp.-Veeversaspis jelli gen.组合(深度 2177.50-2382.94 米)、Asaphellus trinodosus 组合(深度 2030.07-2177.52 米)和 Asaphellus zheni sp.组合(水深 1595.83-2001.88 米)。这两个地层最低的集合体与晚至最新的震旦纪年龄一致(均位于 Paroistodus proteus 区)。第三个,也是最高的一个组合与中弗洛亚时代一致(在 Oepikodus communis 区内)。这一系统性的贡献完善了以往基于年龄诊断的球齿动物群的生物地层学工作,并证明了利用多个分类群进行更可靠的生物地层年龄估算在地层学上的实用性。P.M. Smith [ Patrick.Smith@austmus.gov.au ],澳大利亚新南威尔士州悉尼市澳大利亚博物馆研究所古生物学部;澳大利亚新南威尔士州悉尼市麦考瑞大学生物科学系。H.J. Allen [ heidi.allen@dmirs.wa.gov.au ], Geological Survey of Western Australia, Department of Mines, Industry Regulation and Safety, Mineral House, 100 Plain Street, East Perth, Western Australia, 6004, Australia.
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Early Ordovician trilobites from Barnicarndy 1 stratigraphic well of the southern Canning Basin, Western Australia
Abstract Twenty-three trilobite taxa are described here from the Early Ordovician (Tremadocian to Floian) Nambeet Formation retrieved from the Barnicarndy 1 drillcore, Canning Basin, Western Australia. This includes one new genus, Veeversaspis gen. nov., and six new species: Asaphellus zheni sp. nov., Madiganaspis lauriei sp. nov., Norasaphus (Norasaphus) jagoi sp. nov., Rodingaia leggi sp. nov., Sanbernardaspis excalibur sp. nov., and Veeversaspis jelli gen. et sp. nov. This fauna can be divided into three stratigraphically distinct assemblages, the Apatokephalus sp.–Veeversaspis jelli gen. et sp. nov. Assemblage (2177.50–2382.94 m depth), Asaphellus trinodosus Assemblage (2030.07–2177.52 m depth), and Asaphellus zheni sp. nov. Assemblage (1595.83–2001.88 m depth). The two stratigraphically lowest assemblages are consistent with a late to latest Tremadocian age (both within the Paroistodus proteus Zone). The third, and highest, assemblage is consistent with a mid-Floian age (within the Oepikodus communis Zone). This systematic contribution refines previous biostratigraphic work based on an age-diagnostic conodont fauna and demonstrates the stratigraphic utility of using multiple taxonomic groups for more robust biostratigraphic age estimates. P.M. Smith [ Patrick.Smith@austmus.gov.au ], Palaeontology Department, Australian Museum Research Institute, Sydney, New South Wales, 2010, Australia, and Department of Biological Sciences, Macquarie University, Sydney, New South Wales, 2109, Australia. H.J. Allen [ heidi.allen@dmirs.wa.gov.au ], Geological Survey of Western Australia, Department of Mines, Industry Regulation and Safety, Mineral House, 100 Plain Street, East Perth, Western Australia, 6004, Australia.
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