首页> 外文期刊>Journal of Mammalian Evolution >Palaeothentid Marsupials of the Salla Beds of Bolivia (Late Oligocene): Two New Species and Insights into the Post-Eocene Radiation of Palaeothentoids
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Palaeothentid Marsupials of the Salla Beds of Bolivia (Late Oligocene): Two New Species and Insights into the Post-Eocene Radiation of Palaeothentoids

机译:玻利维亚(晚渐新世)Salla河床的古有袋有袋动物:两种新物种和对古新陈代谢的古类动物的辐射的认识

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We report the finding of new remains of palaeothentid marsupials (Paucituberculata: Marsupialia) from the late Oligocene of Salla, Bolivia (Deseadan South American Land Mammal Age). These fossils represent two new taxa, Antawallathentes illimani and Antawallathentes quimsacruza, increasing the known number of Deseadan palaeothentoid species to 11. Antawallathentes illimani is represented by two incomplete skulls and A. quimsacruza is known only from the holotype, a partial mandible with p3 - m4. Our phylogenetic analysis, based on a data matrix modified from that of Abello, suggests that the two new Salla species are members of the Palaeothentidae (sensu stricto) and are more closely related to each other than they are to other known palaeothentids. Although these new taxa inidicate a greater diversity of Deseadan palaeothentoids than previously appreciated, nowhere in the Deseadan are palaeothentoids abundant, as they are in later Colhuehuapian and Santacrucian faunas. Thus, Deseadan palaeothentoid species richness, coupled with the observation that these palaeothentoids are numerically few in Deseadan faunas, permits the development of a general outline of the post-Eocene palaeothentoid radiation. This may be summarized as follows: 1) EOB Pulse that began near the Eocene/Oligocene Boundary; 2) Deseadan Diversification, increased species richness without large population sizes; and 3) Early Miocene Diversification, increased species richness with local abundances. This Colhuehuapian to Santacrucian diversity with local abundences declined after the Santacrucian. Palaeothentoids are unknown after the Laventan SALMA.
机译:我们报告发现从玻利维亚的萨拉(Salla)渐新世晚期(Deseadan南美陆地哺乳动物时代)发现了古有袋有袋动物(Paucituberculata:Marsupialia)的新遗迹。这些化石代表了两个新的类群,即Antawallathentes illimani和Antawallathentes quimsacruza,使已知的Deseadan palaeothentoid物种数量增加到11个。Antawallathentesillimani由两个不完整的头骨代表,而A. quimsacruza仅从整型中获知,部分下颚为p3-m4 。基于从阿贝罗(Abello)修改的数据矩阵进行的系统发育分析表明,这两个新的Salla物种是Pala科的成员,彼此之间的亲缘关系比与其他已知的enti科更紧密。尽管这些新的分类群使Deseadan的古动物类群比以往更多地被发现,但是Deseadan中没有一个古类动物类群丰富,就像后来的Colhuehuapian和Santacrucian动物区系中那样。因此,Deseadan palentothentoid物种丰富,再加上在Deseadan动物群中这些palentententoids在数量上很少的观察,使得可以建立始新世后palaeothentoid辐射的总体轮廓。可以总结如下:1)在始新世/渐新世边界附近开始的EOB脉冲; 2)Deseadan多样化,物种丰富度增加,而种群数量不大; 3)中新世早期多样化,物种丰富度随着局部丰富而增加。在Santacrucian之后,这种Colhuehuapian到Santacrucian的多样性以及局部丰富性下降了。 Laventan SALMA之后不知道类古生物。

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