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首页> 外文期刊>Palaeontology >LIFE IN PROTO-AMAZONIA: MIDDLE MIOCENE MAMMALS FROM THE FITZCARRALD ARCH (PERUVIAN AMAZONIA)
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LIFE IN PROTO-AMAZONIA: MIDDLE MIOCENE MAMMALS FROM THE FITZCARRALD ARCH (PERUVIAN AMAZONIA)

机译:原始AMAZONIA的生活:FITZCARRALD ARCH(秘鲁氨氮)中的中新世哺乳动物

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摘要

The Middle Miocene has been identified as a time of great diversification in modern lineages now distributed in tropical South America, and when basic archetypal traits defining Amazonia appear, including climatic humid conditions, basic floral physiognomy and phylogenetic composition of modern rainforests. Nonetheless, Middle Miocene localities in South America are poorly known, especially at low latitudes where only one species-rich locality, La Venta in Colombia, has been extensively studied. The present contribution describes the mammal fauna of Fitzcarrald, a new Middle Miocene local fauna from western Amazonia in Peru. Fitzcarrald is correlated with the Laventan South American Land Mammal Age based on the presence of taxa defining the Miocochilius assemblage zone' in La Venta. The mammalian fauna of Fitzcarrald comprises 24 taxa among cingulates, folivores, astrapotheres, notoungulates, litopterns, rodents, odontocetes and a possible marsupial. At this time, tropical South America was characterized by the presence of the Pebas megawetland, a huge lacustrine complex that provided unique ecological and environmental conditions most likely isolating northern South America from southern South America. These isolating conditions might have come to an end with its disappearance in the Late Miocene and the establishment of the subsequent Acre system, the predecessor fluvial system of modern Amazonia. Results of faunistic similarity between Fitzcarrald and other Miocene faunas throughout South America support these scenarios. The Fitzcarrald mammal fauna exhibits first appearance datums and last appearance datums of various taxa, showing that tropical South America has played a crucial role in the evolutionary history and biogeography of major clades, and revealing a more complex biological history than previously proposed, based on the record from the southern cone of the continent.
机译:中新世中期被确定为现在分布在南美热带地区的现代谱系的多元化时代,当定义亚马逊的基本原型特征出现时,包括气候湿润条件,基本的花理和现代雨林的系统发育组成。尽管如此,在南美中新世中部地区却鲜为人知,特别是在低纬度地区,那里仅对一种物种丰富的地区,即哥伦比亚的拉文塔进行了广泛研究。本文稿介绍了Fitzcarrald的哺乳动物区系,Fitzcarrald是来自秘鲁西部亚马逊地区的中新世中新地方性区系。 Fitzcarrald与Laventan南美土地哺乳动物时代有关,这归因于分类单元的存在,该分类单元定义了La Venta中的Miocochilius集合区。 Fitzcarrald的哺乳动物区系包括24种分类单元,包括扣齿状,叶状,斜方肌,三足类,立足类,啮齿类,齿形目和可能的有袋动物。这时,南美热带地区的特征是拥有巨大的湖水复合体Pebas megawetland,它提供了独特的生态和环境条件,极有可能将南美北部与南美南部隔离开来。这些孤立的条件可能随着中新世晚期的消失和随后的英亩系统(现代亚马逊河的前河流系统)的建立而结束。整个南美洲Fitzcarrald动物群与其他中新世动物群之间的相似性结果支持了这些情况。 Fitzcarrald哺乳动物动物区系显示出各种分类单元的最初出现基准和最后出现基准,表明热带南美在主要进化枝的进化历史和生物地理学中发挥了关键作用,并且揭示了比以前提出的更为复杂的生物学历史。记录来自该大陆的南部锥。

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