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三叠纪上部波兹伯格古生物群中一菊石动物群的埋藏学历史和营养相互关系。

Taphonomic history and trophic interactions of an ammonoid fauna from the Upper Triassic Polzberg palaeobiota.

机构信息

Department of Geology and Palaeontology, Natural History Museum Vienna, Burgring 7, 1010, Vienna, Austria.

Vienna Doctoral School of Ecology and Evolution, University of Vienna, Djerassiplatz 1, 1030, Vienna, Austria.

出版信息

Sci Rep. 2022 May 6;12(1):7455. doi: 10.1038/s41598-022-11496-y.

Abstract

The taphonomic mechanisms of a mono- to pauci-specific ammonoid fauna comprising 3565 specimens from the lower Carnian Polzberg Konservat-Lagerstätte near Lunz am See (Northern Calcareous Alps, Lower Austria) is described. The fossiliferous layers were deposited during the Julian 2 Ib (Austrotrachyceras austriacum Zone, Austrotrachyceras minor biohorizon). The deposits comprise abundant nektic ammonoids of the trachyceratid genus Austrotrachyceras. The bivalve Halobia, dominant among the invertebrates, is followed in abundance by the ammonoids Austrotrachyceras and Paratrachyceras, the coleoid Phragmoteuthis and frequent vertebrate actinopterygian fish. The monotonous ammonoid assemblage comprises abundant Austrotrachyceras, frequent Paratrachyceras, rare Carnites and Simonyceras. Recently collected ammonoids were sampled bed-by-bed and compared to extensive historical collections from the same localities. Bromalites (coprolites and regurgitalites) produced by large durophagous fish comprise ammonoid and fish masses and accompany the ammonoid-dominated Polzberg palaeobiota. The ammonoid fauna here presents a window into the nektic cephalopod world of the Upper Triassic assemblage and palaeoenvironment during the deposition of the fossiliferous layers. The frequent occurrence of the vertically oriented (external side horizontal to bedding plane) ammonoid shell fragments hint at a deposition after lethal fish or coleoid attacks. The Polzberg ammonoids were deposited under calm and dysoxic conditions in fine-laminated marlstones and shales of the lower Carnian Polzberg Sub-Basin within the Polzberg Konservat-Lagerstätte.

摘要

描述了一个由 3565 个标本组成的单到少数特化菊石动物群的埋藏机制,这些标本来自下卡尼安 Polzberg 保守地层(上奥地利北部白云石阿尔卑斯山,下奥地利州)。含化石层是在朱利安 2 Ib 期(Austrotrachyceras austriacum 带,Austrotrachyceras minor 生物层位)沉积的。沉积物中含有丰富的浮游菊石 Austrotrachyceras。双壳类 Halobia 是无脊椎动物中的优势种,其次是丰富的 Austrotrachyceras 和 Paratrachyceras 菊石、头足类 Phragmoteuthis 和常见的脊椎动物硬骨鱼。单调的菊石组合包括丰富的 Austrotrachyceras、常见的 Paratrachyceras、稀有 Carnites 和 Simonyceras。最近采集的菊石是按床分层采样的,并与同一地点的广泛历史收藏进行了比较。大型硬骨鱼类产生的 Bromalites(粪化石和回吐化石)包含菊石和鱼类的混合物,并伴随着以菊石为主的 Polzberg 古生物群。这里的菊石动物群提供了一个了解上三叠统组合中浮游头足类世界和化石层沉积期间古环境的窗口。频繁出现的垂直定向(外部侧面与层理面平行)菊石壳碎片暗示了在致命鱼类或头足类攻击之后的沉积。Polzberg 菊石是在上卡尼安 Polzberg 次盆地内的细层纹状泥灰岩和页岩中,在平静和缺氧的条件下沉积的,这些条件属于 Polzberg 保守地层。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2cb6/9076872/34264e969d09/41598_2022_11496_Fig1_HTML.jpg

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