...
首页> 外文期刊>Journal of Systematic Palaeontology >Boreal echinoids from the Tethys Realm: Infulaster and Hagenowia from the Upper Cretaceous of eastern Sardinia (Italy)
【24h】

Boreal echinoids from the Tethys Realm: Infulaster and Hagenowia from the Upper Cretaceous of eastern Sardinia (Italy)

机译:特提斯王国的北方类棘突类动物:撒丁岛东部(意大利)上白垩统的Infulaster和Hagenowia

获取原文
获取原文并翻译 | 示例
           

摘要

The occurrence of typical Boreal echinoid taxa in the Upper Cretaceous of Sardinia is reported and its implications discussed. These new records are unexpected, but not unprecedented, since previous studies have documented other benthic invertebrates with Boreal affinities from the Sardinian Cretaceous. Earlier papers have explained these occurrences by intermittent faunal exchange. This, however, fails to explain why they are absent from most Tethyan shelf deposits. Here we propose a new interpretation: these records could represent examples of a distribution mode widespread in present-day marine species, that of 'isothermal submergence'. This refers to distribution patterns where organisms occur at different depths at different latitudes. The palaeoenvironmental setting of Sardinia (pelagic limestones) and the Chalk Sea (epicratonic deposits) make such an interpretation plausible. A new species of cardiasterid heart urchin, Infulaster navicularis sp. nov., is described, as well as rostrum fragments of a Hagenowia species named in open nomenclature. The specimens were collected from the 'Lanaittu Marl' exposed in the Gorropu Canyon in eastern Sardinia, and are of Coniacian and Late Santonian age, respectively. The new Infulaster species is distinguished by a strongly elongated, non-cordiform outline, high, anteriorly projecting profile, narrow apical angle (c. 55°), and a plastron with two uniserially arranged sternal plates following the labrum. In form it is close to Hagenowia infulasteroides, but it differs from that taxon by its contiguous plastron and larger aboral ambulacral pores.
机译:报告了撒丁岛上白垩纪典型北方类棘突类动物的发生,并讨论了其含义。这些新记录是出乎意料的,但并不是前所未有的,因为以前的研究已经记录了撒丁岛白垩纪其他具有底栖生物的底栖无脊椎动物。较早的论文通过间歇性动物交换来解释这些现象。但是,这不能解释为什么大多数特提斯人的货架沉积物都没有它们。在这里,我们提出了一种新的解释:这些记录可能代表了当今海洋物种中广泛分布的一种分布模式,即“等温淹没”模式。这是指分布模式,其中生物发生在不同纬度的不同深度。撒丁岛(上层石灰岩)和白垩海(上克拉通沉积)的古环境使得这种解释是合理的。心形心顽童的新种,Infulaster navicularis sp。描述了nov。,以及以开放命名法命名的Hagenowia物种的讲台片段。这些标本是从撒丁岛东部戈罗普峡谷暴露的“ Lanaittu Marl”收集的,分别是科尼亚期和桑顿晚期。新的Infulaster种类的特点是:强烈拉长的,非伞形的轮廓,高的,向前突出的轮廓,窄的顶角(约55°)和a骨,其胸骨后跟着两个不规则排列的胸骨板。从形式上讲,它接近Hagenowia infulasteroides,但与它的分类单元不同之处在于其连续的腹甲和较大的胎盘眼孔。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号