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首页> 外文期刊>Journal of Iberian geology >A fern-bennettitalean floral assemblage in Tithonian- Berriasian travertine deposits (Aguilar Formation, Burgos- Palencia, N Spain) and its palaeoclimatic and vegetational implications
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A fern-bennettitalean floral assemblage in Tithonian- Berriasian travertine deposits (Aguilar Formation, Burgos- Palencia, N Spain) and its palaeoclimatic and vegetational implications

机译:Tithonian-Berriasian钙华沉积物(阿吉拉尔组,Burgos-Palencia,N西班牙)中的蕨类-贝尼替他林花艺组合及其古气候和植被意义

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This report describes a macrofloral fossil assemblage discovered in travertine deposits of the Tithonian-Berriasian Aguilar Formation (provinces of Palencia and Burgos, N Spain). The assemblage includes megaremains of a single species of Filicales (Cladophlebis denticulata) and of eleven taxa tentatively identified as Bennettitales (Otozamites mundae, Otozamites sp., Ptilophyllum pecten, Ptilophyllum pectiniformis, Ptilophyllum sp. cf. pectiniformis, Ptilophyllum acutifolium, Ptilophyllum sp., Pterophyllum cycadites, Pterophyllum sp. cf. thomasii, Zamites pumilio, and cf. Pseudocycas sp.). Specimens were preserved as impressions coated with a microbial film up to 5 mm thick made up of: bacteria and cyanobacteria. Based on the available sedimentological and palaeobotanical data, a dry-savannah vegetation and an arid climate were deduced. Late Jurassic macrofloras are globally scarce and have not previously been reported in Spain. Hence, the Aguilar Formation macroflora provides valuable information on the coeval phytogeography and palaeoclimate of southwestern Europe. Furthermore, the lack of floras observed so far in palaeotravertine deposits older than Pliocene in age makes this macroflora exceptional.
机译:这份报告描述了在Tithonian-Berriasian Aguilar组(西班牙帕伦西亚和布尔戈斯省)的钙华沉积物中发现的大型植物化石组合。该组合包括单一物种的Filicales(Cladophlebis denticulata)和11个分类群的巨型遗迹(暂定为Bennettitales(Otozamites mundae),Otozamites sp。,Ptilophyllum pecten,Ptilophyllum pectiniformis,Ptilophyllum sp.cf.苏铁蕨(Pterophyllum cycadites),凤尾蕨(Pterophyllum sp。),参见thomasii,萨米特斯(Zamites pumilio)和假拟苏铁(Pseudocycas sp。)。标本被保存为印模,印模上覆盖有厚达5毫米的微生物膜,该膜由细菌和蓝细菌组成。根据现有的沉积学和古植物学数据,推导出干旱大草原植被和干旱气候。侏罗纪晚期的大型植物在全球范围内都很稀少,以前在西班牙没有报道。因此,阿吉拉尔组大植物群提供了有关欧洲西南部的中世纪植物地理学和古气候的有价值的信息。此外,迄今为止,在年龄比上新世更老的古钙华沉积物中缺乏观察到的菌群,使这种大型菌群成为例外。

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