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Fossil Cercopithecidae of the Afar depression, Ethiopia: Species systematics and comparison to the Turkana Basin.

机译:埃塞俄比亚阿法尔洼地的化石cercopithecidae:物种系统和与图尔卡纳盆地的比较。

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摘要

The fossil Cercopithecidae from the Afar Depression of Ethiopia add considerably to what is known of the family in the African Pliocene and Pleistocene. The sediments that have produced the fossil cercopithecids included in this thesis range in age from 4.4 to 0.25 million years ago (Ma). As most of this material has not been published, it is systematically described. Fossils in this sample represent a minimum of 13 species in 10 genera. At least three of the species and two of the genera are new. The Afar sample also adds to what is known of the other species, including the only relatively complete cranial material of middle Pleistocene Theropithecus. There is considerable turnover of species in the sample, with between 1 and 6 being present at any single time interval.; In order to put the Afar sample into a larger context it is compared with the fossil cercopithecid sample from the Turkana Basin, the only other region that spans a similar time interval, has a large cercopithecid sample, and is well controlled chronologically. Fourteen species (from nine genera) are present in the Turkana assemblage, of which probably only three species are shared between the two basins. At higher taxonomic levels the two regions are more similar.; When the timing of species turnover is compared between the two basins, both show a large number of species first and last appearances prior to 3.4 Ma. The Afar Depression has a second turnover event between 2.9 and 2.5 Ma, but in the Turkana Basin turnover occurs much later, after 2 Ma, with little change between 3.4 and 2.0 Ma. This lack of synchrony between the two basins suggests that Middle Pliocene turnover was not directly forced by a global climatic event.
机译:来自埃塞俄比亚阿法尔洼地的化石科蛇科化石大大增加了非洲上新世和更新世的家族化石。包含在本论文中的产生长尾鳄类化石的沉积物的年龄范围为4.4至25万年前(马)。由于大多数材料尚未发布,因此将对其进行系统地描述。该样品中的化石在10属中至少代表13种。至少有三个物种和两个属是新的。阿法尔(Afar)样本还增加了其他物种的知识,包括中更新世的唯一相对完整的颅骨材料(italic> Theropithecus )。样品中有相当数量的物种转换,在任何单个时间间隔内存在1-6种。为了将Afar样本放到更大的范围内,将其与来自Turkana盆地的cercopithecid化石样本进行了比较,Turkana盆地是唯一跨过相似时间间隔,拥有较大cercopithecid样本且在时间顺序上得到良好控制的其他区域。 Turkana组合中存在14种(来自9属),其中两个盆地之间可能只有3种。在较高的分类学水平上,这两个区域更为相似。比较两个流域的物种更新时间,都显示大量的物种在3.4 Ma之前先出现后出现。阿法尔洼地的第二次周转事件发生在2.9Ma和2.5Ma之间,但是在图尔卡纳盆地,发生周转的时间要晚得多,在2Ma之后,而在3.4Ma和2.0Ma之间变化很小。这两个盆地之间缺乏同步性,这表明中上新世的周转不是全球气候事件的直接推动。

著录项

  • 作者

    Frost, Stephen Robert.;

  • 作者单位

    City University of New York.;

  • 授予单位 City University of New York.;
  • 学科 Paleontology.; Anthropology Physical.
  • 学位 Ph.D.
  • 年度 2001
  • 页码 463 p.
  • 总页数 463
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 古生物学;人类学;
  • 关键词

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