A model of dinoflagellate cyst distribution around the K/Pg boundary and its paleoenvironmental implications (Eastern Alps)

IF 1.7 4区 地球科学 Q2 Earth and Planetary Sciences
O. Mohamed, W. Piller
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引用次数: 1

Abstract

A new model was developed for the paleogeographic distribution of dinoflagellate cysts across the Cretaceous/Paleogene (K/Pg) boundary. Four sections in the Eastern Alps were studied. The Knappengraben and Gamsbach sections are located in the Gosau Basin of Gams, Austria. They are continuous across the boundary and represent a bathyal environment. The Waidach section north of Salzburg (Austria) contains neritic deposits of the Helvetic unit but shows a hiatus at the boundary. The Goppling section between Teisendorf and Oberteisendorf (Bavaria, Germany) belongs to a turbidite-rich, deep-water system (Ultrahelvetic unit), and is considered to be continuous across the boundary. The occurrence and distribution of dinoflagellate cysts in these sections suggests that Trabeculidinium, Adnatosphaeridium, Spiniferites, Pterodinium, Impagidinium, Achomosphaera and Codoniella are restricted to bathyal environments, whereas Areoligera, Manumiella and Trithyrodinium are restricted to the neritic environment. The abundance of Manumiella and Trithyrodinium indicate a high nutrient supply. Hystrichosphaeridium -dominated assemblages have been recorded in both neritic and bathyal environments. Two Manumiella spikes were recorded only at Waidach and interpreted to reflect slight coolings of oceanic surface waters. In the Danian, acme of Spongodinium delitiense are recorded ~1 m above the K/Pg boundary in the neritic and bathyal environments. These acmes could reflect a slight cooling of surface waters in the earliest Danian. The palynofacies analysis in the Gams Basin reveals a high abundance of amorphous organic matter in the Maastrichtian, and black phytoclasts in the Danian, which indicates intensified terrigenous run-off in the Danian with higher sea-floor oxygenation. In the Waidach section, palynomorphs are much more abundant, indicating a shelf to basin transitional area with dysoxic-anoxic conditions at the sea-floor. Austrian Journal of Earth Sciences Vienna DOI: 10.17738/ajes.2017.0003 A model of dinoflagellate cyst distribution around the K/Pg boundary and its paleoenvironmental implications (Eastern Alps) 1)*) 2) Omar MOHAMED & Werner E. PILLER 1) Faculty of Science, Geology Department, Minia University, El-Minia, Egypt; 2) Institute of Earth Sciences (Geology and Palaeontology), University of Graz, Heinrichstrasse 26, 8010 Graz, Austria; *) Corresponding author, omar.mohamed@mu.edu.eg Dinoflagellate cysts; palynofacies; Cretaceous/Paleogene; Eastern Alps
东阿尔卑斯地区K/Pg边界鞭毛藻包囊分布模式及其古环境意义
建立了白垩纪/古近纪(K/Pg)界线上鞭毛藻包囊古地理分布的新模型。研究了东阿尔卑斯山的四个剖面。Knappengraben和Gamsbach部分位于奥地利Gams的Gosau盆地。它们连续跨越边界,代表着深海环境。萨尔茨堡(奥地利)北部的怀达奇剖面包含Helvetic单元的浅海沉积,但在边界处显示出间断。Teisendorf和Oberteisendorf(德国巴伐利亚州)之间的Goppling剖面属于一个富含浊积岩的深水体系(Ultrahelvetic单元),被认为是连续跨越边界的。甲藻囊的出现和分布表明,小叶藻、Adnatosphaeridium、Spiniferites、Pterodinium、Impagidinium、Achomosphaera和Codoniella局限于深海环境,Areoligera、Manumiella和Trithyrodinium局限于浅海环境。沙门氏菌和甲状三甲菌的丰度表明营养供应充足。在浅海和深海环境中均记录了以Hystrichosphaeridium为主的组合。仅在怀达奇记录到两个Manumiella尖峰,并解释为海洋表层水的轻微冷却。在大年纪,在海浅海和深海环境中,在K/Pg边界以上约1 m处记录了delitiense海绵藻的顶点。这些顶点可能反映了大年早期地表水的轻微冷却。Gams盆地孢粉相分析显示,Maastrichtian期无定形有机质丰度高,Danian期黑色植物碎屑丰度高,表明Danian期陆源径流加剧,海底氧合程度较高。在怀达奇剖面,地貌更为丰富,表明海底为陆架-盆地过渡区,存在缺氧-缺氧条件。东阿尔卑斯地区K/Pg边界附近鞭毛藻包囊分布模型及其古环境意义1)*)2)Omar MOHAMED & Werner E. PILLER 1)埃及Minia大学地质学系,El-Minia;2)奥地利格拉茨大学地球科学(地质与古生物学)研究所,奥地利格拉茨海因里希大街26,8010;*)通讯作者,omar.mohamed@mu.edu.eg鞭毛藻囊肿;palynofacies;白垩纪/下第三系;东部的阿尔卑斯山脉
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来源期刊
Austrian Journal of Earth Sciences
Austrian Journal of Earth Sciences Earth and Planetary Sciences-Paleontology
CiteScore
3.10
自引率
0.00%
发文量
0
审稿时长
>12 weeks
期刊介绍: AUSTRIAN JOURNAL OF EARTH SCIENCES is the official journal of the Austrian Geological, Mineralogical and Palaeontological Societies, hosted by a country that is famous for its spectacular mountains that are the birthplace for many geological and mineralogical concepts in modern Earth science. AUSTRIAN JOURNAL OF EARTH SCIENCE focuses on all aspects relevant to the geosciences of the Alps, Bohemian Massif and surrounding areas. Contributions on other regions are welcome if they embed their findings into a conceptual framework that relates the contribution to Alpine-type orogens and Alpine regions in general, and are thus relevant to an international audience. Contributions are subject to peer review and editorial control according to SCI guidelines to ensure that the required standard of scientific excellence is maintained.
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