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首页> 外文期刊>Geodiversitas >Middle Miocene Uruguaytheriinae (Mammalia, Astrapotheria) from Peruvian Amazonia and a review of the astrapotheriid fossil record in northern South America
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Middle Miocene Uruguaytheriinae (Mammalia, Astrapotheria) from Peruvian Amazonia and a review of the astrapotheriid fossil record in northern South America

机译:秘鲁亚马逊河中新世中新世Uruguaytheriinae(哺乳动物,Astrapotheria)和南美洲北部的Astraotheriid化石记录的回顾

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Five mandibular and dental specimens referred to the extinct South American ungulate clade Astrapotheria are described. They originate from late middle Miocene deposits of the Ipururo Formation in the Río Inuya-Río Mapuya area, Peruvian Amazonia. The first Peruvian astrapothere remains unearthed in a controlled stratigraphical context reveal the co-occurrence of the uruguaytheriine astrapotheriids Xenastrapotherium sp. and Granastrapotherium cf. snorki. Bispecific uruguaytheriine assemblages were so far restricted to the early Miocene of Venezuela and the late middle Miocene of Colombia. The Fitzcarrald local fauna, including the uruguay theriines described here, recalls unequivocally the Xenastrapotherium kraglievichi Cabrera, 1929-Granastrapotherium snorki assemblage, which characterizes the 13.6-12.76 Ma interval in the Honda Group of La Venta area, Colombia. The spatio-temporal distribution of low-latitude astrapotheriids (< 30°S) is then reviewed, illustrated, and further detailed in both stratigraphical and taxonomic points of view. The group appears in the fossil record during the Oligocene or the earliest Miocene (Uruguaytherium Kraglievich, 1928 and Xenastrapotherium Kraglievich, 1928 in Uruguay and Venezuela, respectively). Uruguaytheriinae are conspicuous elements of middle Miocene mammal assemblages of northern South America (Colombia, Brazil, Bolivia, and now Peru). Astrapotheria probably become extinct during the late Miocene (Huayquerian South American Land Mammal Age), but the youngest specimens are of uncertain taxonomic affinities and/or might be reworked (Astrapotheriidae indet. in Urumaco Formation of Venezuela; ?Astrapotheria in Rio Acre local fauna of Brazil).
机译:描述了五个被称为灭绝的南美有蹄类进化枝天花粉刺的下颌和牙齿标本。它们起源于秘鲁亚马孙地区里努·伊努亚—里约·马普亚地区伊普罗罗组的中新世中期晚期。在受控的地层环境中出土的第一个秘鲁蛇麻石遗骸揭示了乌拉圭酪氨酸蛇麻石Xenastrapotherium sp的同时存在。和Granastrapotherium cf. snorki。迄今为止,双特异性乌拉圭茶碱组合仅限于委内瑞拉的中新世早期和哥伦比亚的中中新世晚期。 Fitzcarrald当地的动物区系,包括这里描述的乌拉圭酪氨酸,清楚地回顾了1929年的Xenastrapotherium kraglievichi Cabrera-Granastrapotherium snorki组合,其特征是哥伦比亚La Venta地区本田群的13.6-12.76 Ma区间。然后对地纬度(<30°S)的低纬度类麻痹的时空分布进行了回顾,说明,并从地层学和分类学的角度进行了进一步的详细介绍。该组出现在渐新世或最早的中新世时期的化石记录中(分别在乌拉圭和委内瑞拉的乌拉瓜瑟尔·克拉格利维奇,1928年;克纳耶斯梯温姆·克拉格利耶维奇,1928年)。 Uruguaytheriinae是南美洲北部(哥伦比亚,巴西,玻利维亚和现在的秘鲁)中新世中期哺乳动物组合的显着元素。在中新世晚期(Huayquerian南美陆地哺乳动物时代),麻疯树可能已灭绝,但最年轻的标本具有不确定的分类学亲和力和/或可能被重新加工(委内瑞拉乌鲁马科组的麻疯树属;在里约阿克里当地动物区系中?巴西)。

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