Cretaceous-Paleocene transition along a rocky carbonate shore: Implications for the Cretaceous-Paleocene boundary event in shallow platform environments and correlation to the deep sea

D. Sanders, G. Keller, F. Schlagintweit, Martin Studený
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引用次数: 5

Abstract

The Cretaceous-Paleocene (K/P) boundary intervals are rarely preserved in successions of shallow-water limestones. Here, we describe a shallow rocky shore on the active orogenic wedge of the eastern Alps (Austria) fringed by a carbonate platform that was largely cannibalized by erosion. We compared this succession with similar nearshore environments globally, as well as the deep sea, to gain a better understanding of the environmental response to the K/P boundary transition. In the eastern Alps, Cretaceous and Paleocene lithofacies across the K/P boundary transition are separated by a hardground that formed during subaerial exposure and that terminates Upper Maastrichtian limestone with planktic foraminiferal assemblages deposited at neritic depth during zone CF3 (ca. 66.500 Ma). Above the hardground, there are beachrocks with early Danian zone P1a(1) assemblages, which indicate the hardground spans about ~600 k.y. of nondeposition and/or erosion. During the early Danian, the marine transgressive fringe fluctuated between “shoreface to emersion” environments, depositing limestones rich in bryozoans, rhynchonellids, coralline algae, and rare planktic foraminifera along with abraded, bored, and/or encrusted clasts eroded from older rocks. Repeated short subaerial exposure is marked by vadose diagenesis and hardgrounds, including an ~1.5 m.y. interval between magnetochrons C29n to C28n and planktic foraminiferal zones P1b to P1c(2). *Diethard.G.Sanders@uibk.ac.at Current address: Biologiezentrum-Oberösterreichisches Landesmuseum, Johann-Wilhelm-Klein-Strasse 73, A-4040 Linz, Austria. Sanders, D., Keller, G., Schlagintweit, F., and Studeny, M., 2019, Cretaceous-Paleocene transition along a rocky carbonate shore: Implications for the CretaceousPaleocene boundary event in shallow platform environments and correlation to the deep sea, in Adatte, T., Bond, D.P.G., and Keller, G., eds., Mass Extinctions, Volcanism, and Impacts: New Developments: Geological Society of America Special Paper 544, p. 1–XXX, https://doi.org/10.1130/2019.2544(06). © 2019 The Authors. Gold Open Access: This chapter is published under the terms of the CC-BY license and is available open access on www.gsapubs.org. OPEN ACCESS GO LD Downloaded from https://pubs.geoscienceworld.org/books/chapter-pdf/4929473/spe544-06.pdf by Princeton University user on 27 January 2020
沿岩质碳酸盐海岸的白垩纪-古新世过渡:浅层台地环境白垩纪-古新世边界事件的意义及其与深海的对比
白垩纪-古新世(K/P)边界层段在浅水灰岩层序中很少保存。在这里,我们描述了一个位于东阿尔卑斯山(奥地利)活跃造山楔上的浅岩岸,它的边缘是一个很大程度上被侵蚀蚕食的碳酸盐台地。我们将这种演替与全球类似的近岸环境以及深海环境进行了比较,以更好地了解环境对K/P边界转换的响应。在东阿尔卑斯,白垩纪和古新世的岩相跨越钾磷界线过渡,由地面暴露形成的硬地层分隔,并与上马斯特里希特石灰岩相终止,在CF3带沉积于浅海深度的浮游有孔虫组合(约66.500 Ma)。硬地之上为早大年P1a(1)带组合的滩岩,表明硬地的非沉积和/或侵蚀面积约为600 ky。在大年纪早期,海侵边缘在“滨面到外露”环境之间波动,沉积了富含苔藓虫、铃藻、珊瑚藻和稀有浮游有孔虫的石灰岩,以及从较古老的岩石中侵蚀而来的磨损、钻孔和/或包壳碎屑。重复的短时间陆上暴露以气包成岩作用和硬地层为标志,包括在磁时线C29n至C28n和浮游有孔虫带P1b至P1c之间约1.5 m.y.的间隔(2)。*Diethard.G.Sanders@uibk.ac.at目前地址:Biologiezentrum-Oberösterreichisches Landesmuseum, john - wilhelm - klein - strasse 73, A-4040, Linz, Austria。Sanders, D., Keller, G., Schlagintweit, F.和study, M., 2019,沿岩石碳酸盐岩海岸白垩纪-古新世过渡:浅层台地环境白垩纪-古新世边界事件的意义及其与深海的相关性,Adatte, T., Bond, d.p.g.和Keller, G.,编辑。,大灭绝,火山活动和影响:新发展:美国地质学会特别论文544,p. 1-XXX, https://doi.org/10.1130/2019.2544(06)。©2019作者。黄金开放获取:本章根据CC-BY许可条款发布,可在www.gsapubs.org上开放获取。OPEN ACCESS GO LD 2020年1月27日由普林斯顿大学用户从https://pubs.geoscienceworld.org/books/chapter-pdf/4929473/spe544-06.pdf下载
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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