H. Astibia, J. C. Corral, Germán Álvarez-Pérez, Miguel Ángel López Horgue, Aitor Payros
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引用次数: 1
摘要
在始新世时期,比利牛斯地区可能作为连接西特提斯和北大西洋域的古生物地理纽带发挥了重要作用。然而,它的海洋动物仍然很少有记录。本文介绍了对纳瓦拉地区始新世中上(Lutetian至Priabonian)海洋宏观化石的首次研究结果,这些化石被纳入了Maximo Ruiz de Gaona的古生物收藏中,他对这一地区的地质和古生物学研究构成了强制性的历史参考。所描述的化石来自潘普洛纳盆地始新世灰岩地层和Urbasa-Andia灰岩地层及其上覆沉积物,位于潘普洛纳断层以西的Estella-Urbasa地区。一些被研究的标本来自于已不复存在的露头岩层。这一事实增加了保护和研究这些藏品的兴趣。来自埃斯特拉-乌尔巴萨地区的古生物学数据几乎是全新的。本研究对海洋大型动物24个分类群进行了描述。其中7种是纳瓦拉化石记录中的新发现物种,包括:patera Cyclolitopsis、barcelonensis Funginellastraea、Pycnodonte rarilamella、Metacrinus sp.、Triplacidia sp.,以及一种不确定的Cyclostomatida苔藓虫和一种不确定的Serpulidae annelid。在本研究和以前的研究中所描述的宏观古生物学关联并不像其他同时期欧洲地质区域那样多样化。除了可能的生态条件外,抽样偏差,尤其是地语学偏差,特别是文石骨架的无脊椎动物物种的消失,是主要的解释。
Nuevos datos sobre las faunas marinas del Eoceno medio-superior de Navarra (área surpirenaica occidental). Revisión de los fósiles de la colección Ruiz de Gaona
During Eocene times the Pyrenean area may have played an important role as a paleobiogeographic link between the Western Tethys and the North Atlantic domains. However, its marine faunas are still poorly documented. This paper presents the results of a first study on the mid–upper Eocene (Lutetian to Priabonian) marine macrofossils of Navarre included in the paleontological collection of Maximo Ruiz de Gaona, a researcher whose studies on the geology and paleontology of this territory constitute an obligatory historical reference. The described fossils come from the Eocene marly formations of the Pamplona basin and the Urbasa-Andia limestone Formation and overlying deposits, in the Estella-Urbasa area, west of the Pamplona fault. Some of the specimens studied come from outcrops that do not exist any longer. This fact increases the interest of conservation and the study of this collection. The paleontological data from the Estella-Urbasa area are almost entirely new. This study has allowed the description of 24 taxa of marine macrofauna. Seven of them ─Cyclolitopsis patera, Funginellastraea barcelonensis, Pycnodonte rarilamella, Metacrinus sp., Triplacidia sp., in addition to an indeterminate Cyclostomatida bryozoan and an indeterminate Serpulidae annelid─ are new to the fossil record of Navarre. The macropaleontological associations described in this and previous works are not as diverse as those from other coeval European geological regions. In addition to possible ecological conditions, sampling biases and, above all, taphonomic biases, specifically the loss of invertebrate species with aragonite skeletons, arise as the main explanation.
期刊介绍:
Since 1945 Estudios Geologicos publishes original research works, as well as reviews, about any topic on Earth Sciences.
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