拉普兰瑞典喀里多尼亚山脉寒武纪早期(第4阶段)首次发现小型贝壳化石和腕足类和三叶虫的新发现

IF 1.2 4区 地球科学 Q2 GEOLOGY Gff Pub Date : 2021-07-03 DOI:10.1080/11035897.2021.1895303
C. Skovsted, T. Topper, S. McLoughlin, Ove Johansson, Fan Liu, V. Vajda
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引用次数: 5

摘要

在瑞典北部拉普兰Torneträsk湖Luobákte以南的Grammajukku组中发现了新的化石,包括在该组上部的石灰岩床层中发现了一组小Shelly化石(SSF),在该组下部的粉砂岩中发现了腕足类和三叶虫。这种中等多样性的SSF动物群是瑞典Caledonides中首次报道的此类动物群,包括来自波罗的海的tommotiid Lapworthella schodackensis和bradoriia spine Mongolitubulus spinosus的首次记录,以及Bradoria sp.的碎片标本和另外一种bradoriid节肢动物、原牙形虫和helcionelloid软体动物的遗骸。此外,石灰岩床上还发现了大量的腕足动物Botsfordia cf. caelata和Eoobolus cf. priscus的标本,以及一种未识别的椭球头三叶虫。在Grammajukku组更低的地方,在粉砂岩的几个层次上发现了两种腕足动物的标本,正脊类水蛭,三叶虫Ellipsocephalus cf. gripi和一种身份不明的holmiid三叶虫,以前被认为是非化石的。这些发现显著增加了拉普兰北部Grammajukku组古生物群的已知多样性,为斯堪的纳维亚地区下寒武统的生物地层学和古环境以及寒武统动物的古生物地理学提供了新的认识。
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First discovery of Small Shelly Fossils and new occurrences of brachiopods and trilobites from the early Cambrian (Stage 4) of the Swedish Caledonides, Lapland
ABSTRACT New fossil discoveries are reported from the Grammajukku Formation at Luobákte south of Lake Torneträsk in northern Swedish Lapland, including a fauna of Small Shelly Fossils (SSF) from a limestone bed in the uppermost part of the formation and new occurrences of brachiopods and trilobites in siltstones of the lower part of the formation. The moderately diverse SSF fauna is the first of its kind reported from the Swedish Caledonides and includes the first record of the tommotiid Lapworthella schodackensis and the bradoriid spine Mongolitubulus spinosus from Baltica, together with fragmentary specimens of Bradoria sp. and remains of one additional bradoriid arthropod, a protoconodont and a helcionelloid mollusc. In addition, the limestone bed yields abundant specimens of the brachiopods Botsfordia cf. caelata and Eoobolus cf. priscus and an unidentified ellipsocephalid trilobite. Lower down in the Grammajukku Formation, specimens of both brachiopod taxa, orthothecid hyoliths, the trilobite Ellipsocephalus cf. gripi and an unidentified holmiid trilobite were found at several levels in a siltstone, previously regarded as unfossiliferous. These discoveries markedly increase the known diversity of the palaeobiota from the Grammajukku Formation in northern Lapland and provide new insights into the biostratigraphy and palaeoenvironment of the lower Cambrian in Scandinavia and the palaeobiogeography of Cambrian faunas in general.
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来源期刊
Gff
Gff 地学-地质学
CiteScore
2.80
自引率
10.00%
发文量
11
审稿时长
>12 weeks
期刊介绍: GFF is the journal of the Geological Society of Sweden. It is an international scientific journal that publishes papers in English covering the whole field of geology and palaeontology, i.e. petrology, mineralogy, stratigraphy, systematic palaeontology, palaeogeography, historical geology and Quaternary geology. Systematic descriptions of fossils, minerals and rocks are an important part of GFF''s publishing record. Papers on regional or local geology should deal with Balto-Scandian or Northern European geology, or with geologically related areas. Papers on geophysics, geochemistry, biogeochemistry, climatology and hydrology should have a geological context. Descriptions of new methods (analytical, instrumental or numerical), should be relevant to the broad scope of the journal. Review articles are welcome, and may be solicited occasionally. Thematic issues are also possible.
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