首页> 外文期刊>Annales Societatis Geologorum Poloniae >CRYPTIC ENCRUSTING FAUNA INSIDE INVERTEBRATE FOSSILS FROM THE ORDOVICIAN OF ESTONIA
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CRYPTIC ENCRUSTING FAUNA INSIDE INVERTEBRATE FOSSILS FROM THE ORDOVICIAN OF ESTONIA

机译:爱沙尼亚奥陶纪无脊椎动物化石内部的隐匿性动物

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This is the first report of encrusted cryptic surfaces in the Ordovician of Estonia. Only bryozoans and cornulitids occurred in nautiloids and trilobites. Bryozoans were the dominant encrusters, in terms of both the number of specimens and the encrustation area. Stalked echinoderms are common on the hardgrounds in the Middle and Upper Ordovician of Baltica, but the restricted space in nautiloid living chambers and trilobites probably prevented colonization by stalked echinoderms. Cryptic surfaces in nautiloids and trilobites usually are somewhat more encrusted than the open surfaces of hardgrounds in the Ordovician of Estonia. Encrusters presumably favoured cryptic surfaces, as these were less accessible for predators and grazers. Low encrustation densities, compared to North American hard substrates, seem to be characteristic for the Ordovician Baltic Basin.
机译:这是爱沙尼亚奥陶纪地壳隐伏表面的首次报道。鹦鹉螺和三叶虫中仅存在苔藓和角质。就标本数量和包壳面积而言,苔藓虫是主要的包壳动物。棘皮动物棘皮动物在波罗的海中上奥陶纪的硬地层中很常见,但是鹦鹉螺生活室和三叶虫的空间有限,可能阻止了棘皮动物棘皮动物的定居。鹦鹉螺和三叶虫的隐身表面通常比爱沙尼亚奥陶纪硬地的裸露表面硬得多。大概是青蟹喜欢隐秘的表面,因为掠食者和掠食者很难接触到这些表面。与北美硬质基质相比,低结壳密度似乎是奥陶纪波罗的海盆地的特征。

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