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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Pterosaur track assemblages from the Upper Jurassic (lower Kimmeridgian) intertidal deposits of Poland: Linking ichnites to potential trackmakers
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Pterosaur track assemblages from the Upper Jurassic (lower Kimmeridgian) intertidal deposits of Poland: Linking ichnites to potential trackmakers

机译:来自波兰的上侏罗纪(下kimmeridgian)intertidal沉积物的翼龙轨道组装:将ichnites连接到潜在的轨道制造商

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摘要

Two distinct tetrapod track assemblages, dominated by pterosaur traces, are reported from Upper Jurassic (lower Kimmeridgian, Hypselocyclum Zone) tidal flat carbonate deposits exposed in Wierzbica Quarry, 20 km south of Radom, Poland. The pterosaur tracks, tentatively assigned to Pteraichnus isp. are well preserved as a positive hyporelief in intertidal facies. Some are preserved with anatomical details (e.g., skin, claw or digital pad impressions) and quality sufficient to make preliminary ichnotaxonomic assignment. Nearly all collected specimens are larger than most other pterosaurian ichnites of the Late Jurassic age, thus adding to the growing diversity of pterosaur traces known from this time period. Morphometrical and anatomical analyses show that ctenochasmatoids or possibly non-pterydactyloid monofenestratans or rhamphorhynchids were most likely the trackmakers. Anatomical comparisons give new insights into the morphology of the pes of pterydactyloids and the most closely related non-pterodactyloids which may be correlated with a niche expansion into marginal marine and lacustrine environments by Middle and Late Jurassic pterosaurs. The palaeoenvironmental interpretation as tidal flat is confirmed by presence of vertically accreted tidal bundles, each representing deposition in one tidal cycle. Most likely then, this was one of the environments frequented by these pterosaurs and other small tetrapods. The wider palaeoecological significance of the tracks is evaluated in the context of other similar reports from the Late Jurassic of Europe, Africa and North America.
机译:由翼龙痕迹支配的两个不同的Tetrapod轨道组合,从上侏罗纪(下kimmeridgian,低矮的低粘性区域)潮汐扁平碳酸盐矿床,在威尔茨维察采石场以南以南南部20公里。翼龙轨道,暂定分配给Pteraichnus ISP。在潮间相比之下,保持良好的低调。有些是用解剖细节(例如,皮肤,爪子或数字垫印象)和质量足以进行初步IChnotaxoMic ronciC分配的质量。几乎所有收集的标本都比侏罗纪时代的大多数其他翼状胬肉核石大,因此增加了从这个时间段所知道的翼龙痕迹的越来越多的多样性。形态学和解剖学分析表明,Ctorochasmatoids或可能的非翼替丁基单食物或蝶窦最有可能是轨迹制造者。解剖学比较为翼状乳糖体的PE的形态和最密切相关的非翼绕组体的形态提供了新的见解,这些非翼绕组蛋白可以通过中间和晚期侏罗纪翼龙与利基膨胀到边缘海洋和湖泊环境相关。通过存在垂直增强的潮汐束确认,古环境解释是通过垂直增强的潮汐束来确认,每个潮汐束在一个潮汐循环中表示沉积。那么最有可能的是,这是这些翼龙和其他小型四面体经常光顾的环境之一。曲目的更广泛的古生学意义在欧洲,非洲和北美侏罗纪的其他类似报告的背景下评估。

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