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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >New insights on East Finnmark Platform palynostratigraphy and paleogeography - A study of three shallow cores from a Mississippian succession in the Barents Sea, Norway
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New insights on East Finnmark Platform palynostratigraphy and paleogeography - A study of three shallow cores from a Mississippian succession in the Barents Sea, Norway

机译:东芬马克平台地层古地理学的新见解-挪威巴伦支海密西西比演替过程中的三个浅层岩心研究

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Palynomorph assemblages from cores from three shallow stratigraphic boreholes (7029/3-U-1; 7127/10-U-2; 7127/10-U-3) drilled on the East Finnmark Platform have enabled the recognition of four miospore assemblages and two sub-assemblages from the Billefjorden Group in this area, rectifying earlier biozonations. The assemblages are correlated to the Western European biozonation and are based mainly on taxa abundance and the first and last appearances of selected species. All assemblages are Visean to possibly early Serpukhovian in age. Correlations with other biozonations from areas of similar paleolatitude are suggested. Our results suggest that strata assigned to the Billefjorden Group in the offshore may be slightly older than previously assumed. Even so, the Billefjorden Group succession in the offshore is younger than that recognized in the onshore. A mixed signature between the flora from the Arctic region and areas further south in the Euramerican Supercontinent has been observed which may be indicative that the Finnmark Platform was located in a microfloristic transitional region. Generically, the climate in this region was humid and warm during the Visean time which is reflected in the significant amount of neutral, humid and moderately humid floral elements represented by the miospore assemblages. (C) 2016 Elsevier B.V. All rights reserved.
机译:在East Finnmark平台上钻探的三个浅层地层岩心(7029 / 3-U-1; 7127 / 10-U-2; 7127 / 10-U-3)的岩心中的苔藓素组合已经能够识别出四个微孔组合和两个Billefjorden Group在该区域的子组件,纠正了早期的生物区带。这些组合与西欧的生物区划相关,并且主要基于分类单元的丰度以及所选物种的第一个和最后一个出现。所有的组合都是可见的,可能在年龄很早就出现在Serpukhovian中。建议与古纬度相似地区的其他生物区带相关。我们的结果表明,在海上分配给Billefjorden Group的地层可能比以前假定的要早。即便如此,离岸的Billefjorden Group的继任者比在岸的公证者年轻。观察到北极地区的植物群与欧美超大陆的更南区域之间的混合特征,这可能表明Finnmark平台位于微生物群落过渡区域。通常,在Visean时期,该地区的气候温暖而温暖,这反映在以小孢子组合为代表的大量中性,潮湿和中度潮湿的花卉元素上。 (C)2016 Elsevier B.V.保留所有权利。

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