首页> 外文期刊>Journal of Systematic Palaeontology >Cephalopods from reef limestone of the Vasalemma Formation, northern Estonia (latest Sandbian, Upper Ordovician) and the establishment of a local warm-water fauna
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Cephalopods from reef limestone of the Vasalemma Formation, northern Estonia (latest Sandbian, Upper Ordovician) and the establishment of a local warm-water fauna

机译:爱沙尼亚北部Vasalemma组礁灰岩中的头足类动物(最新的上奥陶统桑迪比亚人)和当地温水动物群的建立

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摘要

The cephalopods of the reef limestones of the Vasalemma Formation, northern Estonia, are highly diverse and comprise 22 species belonging to 10 families and seven orders in a sample of >300 specimens. Most of the specimens were collected from shell concentrations in synsedimentary cavities and are interpreted as parautochthonous, washed in from nearby habitats. Nearly all of the shells are fragmented and nearly 15% are partially encrusted by epibionts. The assemblage is dominated by small (mostly less than 30 mm wide), straight-shelled actinocerids and orthocerids; in addition, coiled tarphycerids are common. The high-level taxonomic composition of the Vasalemma cephalopod assemblage, with a dominance of actinocerids and an absence of endocerids, is in agreement with deposition in a warm-water (tropical or subtropical), shallow, subtidal regime. At the species level the assemblage is highly endemic, but the generic composition allows for a statistical comparison with other faunas. A cluster analysis of contemporary assemblages reveals a high degree of similarity with late Sandbian cephalopod faunas of epicontinental Laurentia. The palaeogeographical distribution pattern is similar to that of brachiopods, which supports earlier interpretations of these clusters as mainly controlled by water temperature and depositional depth. Several of the Vasalemma genera became conspicuous elements of epicontinental Laurentia during the Katian, which emphasizes that immigration towards Laurentia was an important factor in Late Ordovician diversity dynamics. Of the described taxa, the following are new: Beloitoceras cautis sp. nov., Curtoceras abditus sp. nov., Hemibeloitoceras arduum sp. nov., H. molis sp. nov., Hoeloceras muroni sp. nov., Isorthoceras cavi sp. nov., I. maris sp. nov., I. padisense sp. nov., I. vexilli sp. nov., Ordogeisonoceras tartuensis sp. nov., Orthonybyoceras isakari sp. nov., O. moisense sp. nov., Pleurorthoceras organi sp. nov., Rummoceras rummuensis gen. et sp. nov. and Trocholites gennadii sp. nov.
机译:爱沙尼亚北部Vasalemma组的礁灰岩的头足类非常多样,在300多个标本的样本中包括22个属10个科的物种和7个阶。大部分标本是从副溶洞中的贝壳中收集的,被解释为是近原虫,从附近的栖息地冲刷而来。几乎所有的贝壳都破碎了,近15%的贝壳被部分表皮包裹着。该组合以小的(大多小于30毫米宽)的,直管的放线猕猴和直腮猴为主。此外,卷曲油菜籽很常见。 Vasalemma头足类组合的高级分类学组成,以放线act类为主,而没有内of类,与温水(热带或亚热带)浅层潮下带的沉积相一致。在物种层次上,这种组合是高度流行的,但是其通用组成允许与其他动物进行统计比较。对当代组合的聚类分析显示,与上陆劳伦西亚陆生晚期桑地亚头足类动物群具有高度相似性。古地理分布格局与腕足类相似,它支持这些团簇的早期解释,主要受水温和沉积深度控制。凯蒂安时期,瓦萨勒玛属的几个属成为陆生劳伦蒂亚的显着元素,这强调向劳伦蒂亚的移民是奥陶纪晚期多样性动态的重要因素。在所描述的分类中,以下是新的:分类信息。 11月,Curtoceras abditus sp.。十一月,Hemibeloitoceras arduum sp.。十一月,H. molis sp。十一月,Hoeloceras muroni sp.。十一月,Isorthoceras cavi sp。十一月,I。maris sp。十一月,I。padisense sp。十一月,I. vexilli sp。十一月,Ordogeisonoceras tartuensis sp。十一月,Orthonybyoceras isakari sp.。十一月,O. moisense sp。十一月,Pleurorthoceras Organi sp.。十一月,Rummoceras rummuensis gen。等。十一月和Trocholites gennadii sp。十一月

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