Department of Geology, University of Liège, Liège, Belgium ; Operational Directory 'Earth and History of Life', Royal Belgian Institute of Natural Sciences, Brussels, Belgium.
CNRS UMR 7207, Département Histoire de la Terre, Muséum National d'Histoire Naturelle, Paris, France.
PLoS One. 2014 Jan 21;9(1):e84709. doi: 10.1371/journal.pone.0084709. eCollection 2014.
Ichthyosaurs are reptiles that inhabited the marine realm during most of the Mesozoic. Their Cretaceous representatives have traditionally been considered as the last survivors of a group declining since the Jurassic. Recently, however, an unexpected diversity has been described in Upper Jurassic-Lower Cretaceous deposits, but is widely spread across time and space, giving small clues on the adaptive potential and ecosystem control of the last ichthyosaurs. The famous but little studied English Gault Formation and 'greensands' deposits (the Upper Greensand Formation and the Cambridge Greensand Member of the Lower Chalk Formation) offer an unprecedented opportunity to investigate this topic, containing thousands of ichthyosaur remains spanning the Early-Late Cretaceous boundary.
METHODOLOGY/PRINCIPAL FINDINGS: To assess the diversity of the ichthyosaur assemblage from these sedimentary bodies, we recognized morphotypes within each type of bones. We grouped these morphotypes together, when possible, by using articulated specimens from the same formations and from new localities in the Vocontian Basin (France); a revised taxonomic scheme is proposed. We recognize the following taxa in the 'greensands': the platypterygiines 'Platypterygius' sp. and Sisteronia seeleyi gen. et sp. nov., indeterminate ophthalmosaurines and the rare incertae sedis Cetarthrosaurus walkeri. The taxonomic diversity of late Albian ichthyosaurs now matches that of older, well-known intervals such as the Toarcian or the Tithonian. Contrasting tooth shapes and wear patterns suggest that these ichthyosaurs colonized three distinct feeding guilds, despite the presence of numerous plesiosaur taxa.
CONCLUSION/SIGNIFICANCE: Western Europe was a diversity hot-spot for ichthyosaurs a few million years prior to their final extinction. By contrast, the low diversity in Australia and U.S.A. suggests strong geographical disparities in the diversity pattern of Albian-early Cenomanian ichthyosaurs. This provides a whole new context to investigate the extinction of these successful marine reptiles, at the end of the Cenomanian.
鱼龙是一类生活在中生代海洋中的爬行动物。它们的白垩纪代表传统上被认为是自侏罗纪以来一直衰落的群体的最后幸存者。然而,最近在上侏罗统-下白垩统的沉积物中描述了出乎意料的多样性,但这种多样性在时间和空间上广泛分布,仅为最后鱼龙的适应潜力和生态系统控制提供了一些小线索。著名但研究甚少的英国高顿组和“绿砂”沉积层(上绿砂层和下白垩统的剑桥绿砂层成员)提供了一个前所未有的机会来研究这个课题,其中包含了跨越早白垩世-晚白垩世界线的数千条鱼龙遗骸。
方法/主要发现:为了评估这些沉积体中鱼龙组合的多样性,我们在每种骨骼类型中识别出形态型。当有可能时,我们将这些形态型组合在一起,使用来自同一地层和法国沃克顿盆地新地点的关节标本;提出了修订后的分类方案。我们在“绿砂”中识别出以下分类群:平鳍鱼龙类“Platypterygius” sp.和 Sisteronia seeleyi 属种新属种,不确定的大眼鱼龙类和罕见的归入未定属种的 Cetarthrosaurus walkeri。晚阿尔比阶鱼龙的分类多样性现在与较老的、著名的地层(如托尔阶或提通阶)相匹配。对比牙齿形状和磨损模式表明,尽管存在许多蛇颈龙类,这些鱼龙还是殖民了三个不同的摄食群体。
结论/意义:在它们最终灭绝前几百万年,西欧是鱼龙的多样性热点地区。相比之下,澳大利亚和美国的低多样性表明阿尔比阶-早塞诺曼阶鱼龙的多样性模式存在强烈的地理差异。这为研究这些成功的海洋爬行动物在塞诺曼阶末期灭绝提供了一个全新的背景。