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首页> 外文期刊>Journal of Paleontology >Torridorefugium eskridgensis (new ichnogenus and ichnospecies): Amphibian aestivation burrows from the lower Permian Speiser Shale of Kansas
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Torridorefugium eskridgensis (new ichnogenus and ichnospecies): Amphibian aestivation burrows from the lower Permian Speiser Shale of Kansas

机译:Torridorefugium eskridgensis(新ichnogenus和ichnospecies):来自堪萨斯州下二叠纪Speiser页岩的两栖动物洞穴

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Burrows of the lysorophid amphibian Brachydectes elongatus occur in deposits interpreted as ephemeral ponds within the Lower Permian Speiser Shale of eastern Kansas. The burrows of B. elongatus have been previously recorded in the Lower Permian strata of Texas, Oklahoma, and Kansas, but have not been described in detail and an ichnotaxonomic designation has not been provided. Torridorefugium eskridgensis new ichnogenus and ichnospecies show two types of burrow architecture distinguished by width-to-length ratios. Type I burrows are elongate, elliptical tubes 4-32 cm long and 2-7 cm wide. Type 11 burrows are short, elliptical tubes 1.5-3.5 cm long and 2.5-5 cm wide. Both Type I and 11 burrows may contain coiled skeletons of B. elongatus. Torridorefugium eskridgensis occur in clusters of up to 45 burrows with maximum concentrations of 20/m(2).The type specimens of Torridorefugium eskridgensis occur in a 40-cm-thick lens of calcareous mudstone that fills a 100-m-long paleodepression within a well-developed paleosol. The burrow clusters are capped by surfaces with evidence of subaerial exposure, and overlain by nonburrowed, massive mudstone containing the fossils of the charophyte Stomachara, the ostracodes Carbonita and Paraparchites, fish, amphibians, and reptiles. This succession suggests that lysorophids burrowed in response to episodic, perhaps seasonal, droughts on the Permian midcontinental coastal plain. Permian lysorophid burrowing behavior is analogous to that of the extant aestivating amphibians Amphiuma sp. and Siren intermedia that inhabit ephemeral rivers and ponds of the southeastern United States.
机译:堪萨斯州东部下二叠纪Speiser页岩中的溶蚀性两栖类Brachydectes elongatus洞穴出现在被解释为短暂池塘的沉积物中。先前已经在得克萨斯州,俄克拉荷马州和堪萨斯州的下二叠系地层中记录了伸长双歧杆菌的洞穴,但未进行详细描述,也未提供鱼类分类学名称。鱼类新栖鱼类和鱼类物种显示了两种类型的洞穴结构,以长宽比为特征。 I型洞穴是细长的椭圆形管,长4至32厘米,宽2至7厘米。 11型洞穴很短,椭圆管长1.5-3.5厘米,宽2.5-5厘米。 I型和11型洞穴都可能包含弯曲的B. elongatus骨架。臭rid铁皮发生在最多45个洞穴的簇中,最大浓度为20 / m(2)。臭rid铁皮的类型标本出现在40厘米厚的钙质泥岩中,充满了100米长的古白垩纪。发达的古土壤。洞穴群被有地下暴露迹象的表面所覆盖,并被未挖洞的块状泥岩覆盖,泥岩包含风化石气孔,化石,石炭纪和副轻石,鱼,两栖动物和爬行动物的化石。这种演替表明,溶石虫在二叠纪中陆沿岸平原上发生的偶发性季节性干旱(可能是季节性干旱)时会挖洞。二叠纪溶食卵的穴居行为类似于现存的两栖两栖动物Amphiuma sp。的穴居行为。和居住在美国东南部短暂河流和池塘中的警报器中间媒介。

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