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First record of a conodont-bearing, hemipelagic Upper Carboniferous stratigraphic horizon in the MalaguideComplex (eastern Betic Cordillera)

机译：malaguide中具有牙形石，半海洋上石炭统地层视界的第一个记录复杂（东贝蒂科迪勒拉）

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Un horizonte carbonatado hemipelágico entre pizarras del ComplejoMaláguide del Corredor de Vélez Rubio-Lorca ha proporcionado conodontosdel Bashkiriense basal-Moscoviense medio. Esta edad es equivalente a (o ligeramentemás moderna que) la de los clastos de calizas con fósiles marinossomeros identificados en el Conglomerado de Marbella, que eran hastala fecha los elementos más modernos reconocidos en el Paleozoico maláguide.Este hallazgo revela una paleogeografía carbonífera en el DominioMaláguide algo más compleja de lo que hasta ahora se sospechaba, y ponede manifiesto la persistencia, en dicho dominio, de una zonación de ambientesde plataforma somera a cuenca hemipelágica hasta el Carboníferotardío

机译：VélezRubio-Lorca走廊的Maláguide综合体的板岩之间的半碳酸盐岩层位提供了基底-Moscoviense Bashkirian中部的牙形石。这个年龄相当于（或比现代年龄稍长一些）马贝拉集团（Marbella Conglomerate）中发现的带有海洋海洋化石的石灰岩碎屑，这是迄今为止古生代Maláguide中公认的最现代的元素。比以前怀疑的要复杂一些，并且显示了从浅台地到半海盆盆地直至石炭纪晚期的环境分区的持久性。

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Navas Parejo Pilar; Rodríguez Cañero Rosario; Martín Algarra Agustín;
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First record of a conodont-bearing, hemipelagic Upper Carboniferous stratigraphic horizon in the MalaguideComplex (eastern Betic Cordillera)

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