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A POSSIBLE LATE CAMBRIAN VERTEBRATE FROM AUSTRALIA

机译:来自澳大利亚的可能的晚生寒武纪脊椎动物

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THE fossil record of early vertebrates starts with certainty with the dermal armour of agnathan fish from the Early-Middle Ordovician of Australia(1,2). Recent controversial acceptance that conodonts(3) and the fragments called Anatolepis(4,5) may be vertebrate remains(6), extends their fossil record back to the Late Cambrian. Now a new type of phosphatic skeleton from Australia shows a three-layered structure that indicates vertebrate affinity, but with several unique features not known in other vertebrates. The new evidence challenges the most widely accepted current theory for the development of the vertebrate skeleton(7-11), which assumes the odontode (skin denticle) to be the primitive patterning component. The Australian material provides an alternative model for early vertebrate dermal armour with which to assess the vertebrate-like hard tissues in conodonts(12,13) and the dermal armour of Anatolepis(4-6,14). [References: 29]
机译:早期脊椎动物的化石记录可以肯定地从澳大利亚中早奥陶纪的长鳍金枪鱼的皮甲开始(1,2)。最近有争议的证据表明牙形石(3)和称为Anatolepis(4,5)的碎片可能是脊椎动物的遗骸(6),将其化石记录扩展到了寒武纪晚期。现在,来自澳大利亚的一种新型磷骨架显示出三层结构,表明脊椎动物具有亲和力,但具有其他脊椎动物所不具备的几个独特特征。新的证据挑战了目前最广泛接受的有关脊椎动物骨骼发育的理论(7-11),该理论认为齿状突(皮肤牙质)是原始的构图成分。澳大利亚的材料为早期脊椎动物的皮肤铠装提供了另一种模型,利用该模型可以评估牙形刺中的脊椎动物样硬组织(12,13)和Anatolepis的皮肤铠装(4-6,14)。 [参考:29]

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