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首页> 外文期刊>Neues Jahrbuch fur Geologie und Palaontologie. Abhandlungen >An updated taxonomic view on the family Gomphotheriidae (Proboscidea) in the final Pleistocene of south-central Chile
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An updated taxonomic view on the family Gomphotheriidae (Proboscidea) in the final Pleistocene of south-central Chile

机译:有关智利中南部最后更新世的Gomphotheriidae(Proboscidea)科的最新分类学观点

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There is an abundant fossil record of the family Gomphotheriidae in Chile, which is en-tirely ascribed to the late Pleistocene. Despite this, the lack of taxonomically diagnostic material has lead to an extended discussion, which has not reached a consensus regarding the number of forms of gomphotheres effectively present. This paper discusses the taxonomy of Chilean gomphotheres, based on tooth morphology and biometry, paleoecological and biogeographical data. The morphol-ogy of the tusks indicates the presence of the Stegomastodon genus in Chile, while bivariate and multivariate analyses of the teeth show an important amount of variability within the studied sample, although with a tendency towards larger sizes for the genus Stegomastodon and the Chilean samples than for Cuvieronius, especially among the M3s and m3s. In spite of this, in this paper only the specimens from localities that yielded molars associated with tusks are assigned to the genus Stego-mastodon. Biogeographic information is consistent with the presence of a lowland-adapted taxon such as Stegomastodon, which could have reached the Chilean territory either through an Andean corridor from Argentina, or through a low-altitude route from Peru, then by the northern region of Chile. Bibliographic isotopic data also indicates an adaptative change to C3 feeding along a latitudinal gradient, around 35-41°S, which makes the Chilean and south Argentinean results quite similar at these latitudes. Due to the metric variability observed, the Chilean samples could not be assigned to individual species.
机译:智利的Gomphotheriidae科有大量化石记录,这完全归因于晚更新世。尽管如此,由于缺乏分类学诊断材料,导致了更广泛的讨论,关于有效存在的Gomphothers的数量尚​​未达成共识。本文根据牙齿的形态和生物特征,古生态和生物地理数据,讨论了智利公母的分类学。 Chile牙的形态学表明智利存在剑齿兽类,而对牙齿的双变量和多变量分析显示,在所研究的样本中,牙齿具有很大的变异性,尽管剑齿兽类和智利人倾向于变大。样本比Cuvieronius样本多,尤其是在M3和m3之间。尽管如此,在本文中,只有来自产生与牙相关的臼齿的地方的标本才被归为Stego-Mastodon属。生物地理信息与低地生物分类群(如剑齿象纲)的存在是一致的,它可以通过阿根廷的安第斯山脉走廊,或从秘鲁的低空路线到达智利的北部地区,然后到达智利的北部地区。书目同位素数据还表明,C3的进给量沿纬度梯度(约35-41°S)发生了适应性变化,这使得智利和阿根廷南部的结果在这些纬度上非常相似。由于观察到的度量变异性,无法将智利样品分配给单个物种。

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