博若莱下托瓦西亚的窄鳍鱼类和托瓦西亚海洋缺氧事件期间鱼龙保存的化学地层背景

J. Martin, G. Suan, B. Suchéras-Marx, Louis Rulleau, J. Schlögl, Kévin Janneau, Matt Williams, A. Léna, Anne-Sabine Grosjean, E. Sarroca, V. Perrier, V. Fernandez, Anne‐Lise Charruault, E. Maxwell, P. Vincent
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引用次数: 5

摘要

摘要:我们报道了在法国东南部博若莱的LafargeHolcim Val d'Azergues采石场的下托瓦里亚层发现的新的鱼龙材料。一个部分关节的头骨和一个保存在碳酸盐固结物中的较小的、未准备但可能不完整的骨架被确定为窄翼龙,这是早侏罗世在欧洲广泛分布的一个科。这些标本是欧洲已知的保存最完好的托瓦西亚标本之一,其中一个标本疑似保存了软组织。它们的保存状态归因于水-沉积物界面附近长时间的缺氧条件和硫酸盐还原菌活性导致的早期碳酸盐胶结作用的结合。我们还提供了从研究地点获得的碳和锶同位素值,可以与其他Toarcian脊椎动物产生地点和与Toarcian海洋缺氧事件(T-OAE)相关的环境扰动进行详细的时间比较。这些比较表明,长时间的低底水氧合和低积累速率有利于鲸尾纲脊椎动物相对较高的丰度和良好的保存状态。在T-OAE期间普遍存在的环境条件可能是Lagerstätte-type沉积物的广泛性质以及海洋生物的特殊保存的原因。测试T-OAE是否对海洋脊椎动物有生物影响,需要一个精确的化学地层学背景,跨越Pliensbachian-Toarcian间隔的化石记录。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Stenopterygiids from the lower Toarcian of Beaujolais and a chemostratigraphic context for ichthyosaur preservation during the Toarcian Oceanic Anoxic Event
Abstract We report new ichthyosaur material excavated in lower Toarcian levels of the LafargeHolcim Val d'Azergues quarry in Beaujolais, SE France. A partially articulated skull and a smaller, unprepared but likely subcomplete skeleton preserved in a carbonate concretion are identified as stenopterygiids, a family of wide European distribution during the Early Jurassic. These specimens are among the finest preserved Toarcian exemplars known from Europe and, in one of them, soft tissue preservation is suspected. Their state of preservation is attributed to the combination of prolonged anoxic conditions near the water–sediment interface and early carbonate cementation resulting from the activity of sulfate-reducing bacteria. We also present carbon and strontium isotope values obtained from the study site that allow detailed temporal comparisons with other Toarcian vertebrate-yielding sites and environmental perturbations associated with the Toarcian Oceanic Anoxic Event (T-OAE). These comparisons suggest that the relatively high abundance and good preservation state of Toarcian vertebrates was favoured by a prolonged period of low bottom water oxygenation and accumulation rates. The environmental conditions that prevailed during the T-OAE were probably responsible for the extensive nature of Lagerstätte-type deposits with exceptional preservation of marine organisms. Testing whether the T-OAE had a biological impact on marine vertebrates requires a precise chemostratigraphic context of the fossil record spanning the Pliensbachian–Toarcian interval.
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