首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Middle Triassic (Ladinian) amphibian tracks from the Lower Keuper succession of southern Germany: Implications for temnospondyl locomotion and track preservation
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Middle Triassic (Ladinian) amphibian tracks from the Lower Keuper succession of southern Germany: Implications for temnospondyl locomotion and track preservation

机译:来自德国南部较低的Keuper连续的中间三叠纪(Ladinian)两栖动物:对Temnospontyl Locomotion和轨道保存的影响

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摘要

Triassic temnospondyl amphibian tracks are relatively rare, in contrast with the body fossil record. Herein we report temnospondyl tracks from the base of the Anthrakonitbank carbonate bed, within the upper Middle Triassic Lower Keuper succession (Erfurt Formation) in the Vellberg Fossil-Lagerstiitte of southern Germany. The sedimentary succession comprises restricted marine deposits, and the track-bearing layer includes microbial mats covering thin bone-beds. The ichnological material includes > 20 footprints, four of which are arranged in a trackway, and all footprints comprise manus impressions with no pes preserved. The combination of characters, such as tetradactyl clawless manus impressions, relative digit length and angulation, and trackway with low pace angulation, are different from any known tetrapod ichnotaxon. While the scarcity of material precludes a confident ichnotaxonomy, comparison with the autopodia in the body fossil record suggests capitosaur stereospondyls as the most probable trackmakers. Ichnological and sedimentological features indicate that the trackmakers displayed a walking-swimming locomotion, with a sprawling posture, only touching the substrate with the forelimbs, as seen in present-day swimming crocodiles. The Vellberg tetrapod tracks reported here contribute to our knowledge of the Triassic ichnological record, as well as the life style and habitats of temnospondyls.
机译:三叠纪的Temnosphondyl两栖动物曲目相对罕见,与身体化石记录相比。在这里,我们在德国南部Vellberg Fossil-Lagerstiitte的中间中间三叠纪较低的钥匙连续(Erfurt Formation)内,从蒽酮盐百合碳酸盐床的底部报告了Semnospontyl曲目。沉积连续包括限制的海洋沉积物,轨道承载层包括覆盖薄骨床的微生物垫。 IChnological材料包括> 20个占地面积,其中四个排列在轨道上,并且所有足迹包括没有保留PES的粉碎片印象。字符的组合,例如四酰胺克莱克拉夫勒芒实造影,相对数字长度和角度以及具有低速度角度的运动道,与任何已知的Tetrapod Ichnotaxon不同。虽然材料的稀缺性排除了一个自信的Ichnotaxonomy,但与身体化石记录的自动透视比较表明Capitosaur Sterepondyls作为最有可能的轨道制作人。 Ichnological和沉积物学特征表明,轨道制造商展示了一个步行游泳运动,庞大的姿势,只有在当今游泳鳄鱼中看到的前肢触摸基板。据报道,Vellberg Tetrapod轨道有助于我们对Triassic Ichnological记录的了解,以及Temnospondyl的生活方式和栖息地。

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