首页> 外文期刊>Acta palaeobotanica >A revised stratigraphy for the Palaeocene Agatdalen flora (Nuussuaq Peninsula, western Greenland): correlating fossiliferous outcrops, macrofossils, and palynological samples from phosphoritic nodules
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A revised stratigraphy for the Palaeocene Agatdalen flora (Nuussuaq Peninsula, western Greenland): correlating fossiliferous outcrops, macrofossils, and palynological samples from phosphoritic nodules

机译:古新世Agatdalen植物区系(格陵兰西部Nuussuaq半岛)的修订地层学:关联化石露头,大型化石和来自磷结核的孢粉样本

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The Cretaceous and Palaeogene floras of western Greenland that were initially described as part of the classical work “Flora fossilis arctica” by Oswald Heer in the 19th century are currently under revision. The Nuussuaq Basin has repeatedly been investigated by geologists and marine invertebrate palaeontologists. These studies provide a modern stratigraphic framework and a basis for revisions of various Cretaceous to Eocene floras from this region, and the correlation of fossil material to stratigraphic units and formal formations. This paper is the first in a series of papers that (i) correlate macrofossil (museum) material and fossil-rich localities with the modern lithostratigraphic framework, (ii) describe new pollen, spores, and other marine/freshwater palynomorphs, and (iii) revise the macrofossil remains from the Agatdalen area (particularly the Danian Agatdal Formation). Since the work of B. Eske Koch in the 1960s and 70s, questions emerged about the correlation of plant fossiliferous outcrops and whether the so-called Agatdalen flora, referred to the Agatdal Formation, originates from a single sedimentary unit or not. In this paper, we summarise the stratigraphy of the Agatdalen area and correlate the fossil plant-bearing outcrops described by Koch to the current lithostratigraphy. We establish which plant fossils belong to the Agatdal Formation and re-assign a great number of other plant fossils to their correct formations. New palynological material is briefly described and correlated to the macrofossil localities and the Agatdal Formation. Previous accounts on the macrofossils (leaves, fruits, seeds) are briefly discussed and directions for future revisions are outlined.
机译:格陵兰岛西部的白垩纪和古近纪植物群最初被描述为19世纪奥斯瓦尔德·赫尔(Oswald Heer)的经典著作“弗洛拉化石”的一部分。 Nuussuaq盆地已被地质学家和海洋无脊椎动物古生物学家反复调查。这些研究为该地区各种白垩纪至始新世植物群的修订以及化石物质与地层单元和形式构造的相关性提供了现代的地层学框架和基础。本文是(i)将大型化石(博物馆)材料和富含化石的地方与现代岩相地层学框架相关联的论文系列中的第一篇,(ii)描述了新的花粉,孢子和其他海洋/淡水古植物形态,以及(iii )修改Agatdalen地区(尤其是Danian Agatdal组)的大型化石残骸。自从B. Eske Koch在1960年代和70年代开展工作以来,人们开始质疑植物化石露头的相关性,以及所谓的Agatdalen植物群(称为Agatdal地层)是否起源于单个沉积单元。在本文中,我们总结了Agatdalen地区的地层,并将Koch描述的含化石植物的露头与当前的岩相地层联系起来。我们确定哪些植物化石属于Agatdal地层,然后将大量其他植物化石重新分配给它们的正确地层。简要介绍了新的孢粉学材料,并将其与大型化石的位置和阿格达特形成相关。简要讨论了大型化石(叶子,果实,种子)的先前记录,并概述了未来修订的方向。

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