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Middle Pleistocene large-mammal faunas from North Iberia: palaeobiogeographical and palaeoecological implications

机译:来自北伊比利亚的中更新世大型哺乳动物动物群:古生物地理学和古生态学意义

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The rich Quaternary fossil record from the Cantabrian region (NW Iberia) is virtually restricted to the Late Pleistocene, with Middle Pleistocene findings very rare. This work presents the study of two Middle Pleistocene palaeontological sites in the Cantabrian region: Llantrales quarry and Mestas de Con mine, both discovered and first described in the 1950s but never studied in detail thereafter. The material was here re-analysed and re-evaluated. Taxonomic attributions have been changed in most cases and, consequently, chronological assignments of the fossils have also been changed. This first detailed study of the assemblage from Llantrales quarry revealed the occurrence of the large-sized deer Praemegaceros solilhacus, which has never been reported previously in North Iberia. Cervus cf.elaphus and Stephanorhinus cf.hundsheimensis were also identified. The age of these fossils was originally regarded as Pontian (late Miocene), but new palaeontological results indicate a much younger age, most likely from around 0.8 to 0.5Ma. A taxonomic re-evaluation of the fossils from Mestas de Con provided different results with respect to the 1950s works. The faunal association is composed of a large-sized deer (probably corresponding to Praemegaceros), Cervus elaphus, Capreolus cf.capreolus, Bison sp. (small sized), Equus sp. (large sized), Stephanorhinus hemitoechus, Ursus sp. and Homotherim latidens. This faunal association was evaluated within a western European context and proves to be highly analogous to other contemporary assemblages there. The chronology was initially regarded as late Villafranchian (in a broader sense). New results, documenting the co-occurrence of Stephanorhinus hemitoechus and Homotherium latidens, indicate a more precise and younger age, most likely between 0.6 and 0.4Ma. These two fossil assemblages provide new and relevant information on the Middle Pleistocene faunas from a geographical region where this information, compared with other western European areas, is rare and poorly known.
机译:来自坎塔布连地区(西北伊比利亚)的丰富的第四纪化石记录实际上仅限于晚更新世,而中更新世的发现非常罕见。这项工作介绍了坎塔布连地区的两个中更新世古生物学遗址:Llantrales采石场和Mestas de Conmine,它们都在1950年代被发现并首次被描述,但此后没有进行详细研究。这里对材料进行了重新分析和评估。在大多数情况下,生物分类的属性已改变,因此,化石的时间顺序也已改变。首次对Llantrales采石场的组合进行详细研究后,发现了大型鹿Praemegaceros solilhacus的发生,此前在北伊比利亚从未有过报道。还鉴定了宫颈cf.elaphus和Stephanorhinuscf.hundsheimensis。这些化石的年龄最初被认为是笨珍(中新世晚期),但是新的古生物学结果表明其年龄要年轻得多,最有可能在0.8Ma到0.5Ma之间。对Mestas de Con的化石进行的分类学重新评估与1950年代的作品提供了不同的结果。动物群协会由大型鹿(可能对应于Praemegaceros),长颈鹿,Capreolus cf.capreolus,Bison sp。组成。 (小型),马属sp。 (大型),Stephanorhinus hemitoechus,Ursus sp.。和Homotherim latidens。在西欧的背景下对该动物群进行了评估,并证明与该地区的其他当代组合高度相似。年表最初被认为是维拉弗兰奇时代晚期(广义上)。新的结果记录了半边无步伐木(Stephanorhinus hemitoechus)和白僵菌(Homootherium latidens)的同时出现,表明年龄更精确,更年轻,最有可能在0.6至0.4Ma之间。这两个化石组合为某个地理区域的中更新世动物群提供了新的相关信息,而与其他西欧地区相比,该信息是稀有且鲜为人知的。

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