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首页> 外文期刊>Cretaceous Research >Crescentiella morronensis (Crescenti) (incertae sedis) dominated microencruster association in Lower Cretaceous (lower Aptian) limestones from the Rar?u Massif (Eastern Carpathians, Romania)
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Crescentiella morronensis (Crescenti) (incertae sedis) dominated microencruster association in Lower Cretaceous (lower Aptian) limestones from the Rar?u Massif (Eastern Carpathians, Romania)

机译:颅骨莫隆(crescenci)( incertae sedis )在Rar的下白垩纪(下部Aptian)石灰岩中的微生物晶体结合在一起?U massif(东部 喀尔巴阡山脉,罗马尼亚)

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Abstract Analysis of eight outcrops from Rar?u Massif (Eastern Carpathians, Romania) revealed a rich assemblage of encrusting organisms mostly of problematic biological affiliation within platform-margin facies – Crescentiella morronensis, Radiomura cautica, Koskinobullina socialis, Pseudorothpletzella schmidi, Lithocodium aggregatum and bacinellid structures, encrusting calcified sponges (Calcistella jachenhausenensis, Neuropora lusitanica) and foraminifera (Coscinophragma cribrosa). Orbitolinids, calcareous green algae and rudists assign an early Aptian age (Bedoulian) for the studied limestones. In terms of species variety, abundance and structural microfabrics the studied microencruster association show similarity with the Upper Jurassic communities from reef and peri-reefal sedimentary settings. Comparisons with such assemblages are emphasized here. The presence of the sporolithacean and peyssonneliacean red algae (Sporolithon rude and Polystrata alba) contributes also to the construction of superimposed crusts. Even if the known stratigraphic range of the microencrusters is not strictly limited to the late Jurassic, reports of comparable associations in Urgonian-type facies is poorly documented. Therefore, it exemplifies the resistance and flourishing events of many encrusters throughout the Mesozoic. ]]>
机译:<![CDATA [ 抽象 从rar的八个露头的分析?U massif(东喀尔巴阡山脉,罗马尼亚)揭示了覆盖生物的丰富组合在平台边缘面内有问题的生物学轴承 - 颅骨莫罗森斯 radiomura cautica koskinobullina socialis 斜逸普雷扎拉施密集岩型骨髓增生和bacinellid结构,镶嵌钙化海绵( calcistella jachenhausenensis neuropora lusitanica )和foraminifera( coscinopharragma cribrosa )。胰蛋白酶,钙质绿藻和粗鲁斯主义者为学习的石灰岩分配了一个早期的安抚龄(卑河)。就物种品种,丰度和结构微制造而言,研究了微生物结合与珊瑚礁和Peri-Reefal沉积设置的上侏罗桑社区的相似性。这里强调了这种组合的比较。孢子素淤积和培森西生物红藻(孢子素粗鲁 polystrata alba )也有助于建设叠加的外壳。即使已知的微生物的地层范围没有严格限制在侏罗纪的晚期,腑脏型相片中的可比协会的报告尚未记录。因此,它举例说明了在整个中生代的许多核的抵抗和繁荣的事件。 ]]>

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