早渐新世峡谷渡口水库沉积的蚁化石(膜翅目:蚁科)

IF 1.9 Q2 ENTOMOLOGY
J. LaPolla
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引用次数: 0

摘要

早渐新世(约32.0 Ma)峡谷渡口水库沉积物被认为含有大量保存完好的植物和动物化石。其中111个化石标本经鉴定,归属于5属:Dolichoderus、Liometopum、Camponotus、Lasius和Manica,隶属于Dolichoderinae、Formicinae和Myrmicinae 3个亚科。描述了两个新的化石种。绿walti Liometopum sp. 11 .是北美已知的第三个来自该属的化石物种,在形态上与弗洛里桑特沉积物中已知的另外两个化石物种不同。这三种化石的Liometopum物种与现存的三个北美物种进行了比较。Manica iviei sp. 11 .是该属在北美已知的第一个化石种,也是描述的第二个化石种。本种具有宽的腹侧端后突,在北美现存物种中只存在于Manica hunteri。峡谷渡口蚂蚁代表了北美唯一确定的渐新世时期包含蚂蚁的化石沉积物,因此提供了一个独特的视角来了解该大陆现代蚂蚁群落出现的时间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fossil ants (Hymenoptera: Formicidae) of the early Oligocene Canyon Ferry Reservoir deposit
The early Oligocene (ca. 32.0 Ma) Canyon Ferry Reservoir deposit is known to contain an extraordinary number of well-preserved plant and animal fossils. Among those are 111 fossil ant specimens that were examined and assigned to five genera: Dolichoderus, Liometopum, Camponotus, Lasius, and Manica from three subfamilies: Dolichoderinae, Formicinae, and Myrmicinae. Two new fossil species are described. Liometopum greenwalti sp. nov. is the third fossil species known from this genus in North America and is morphologically distinct from the other two fossil species that are known from the Florissant deposit. The three fossil Liometopum species are compared to the three extant North American species. Manica iviei sp. nov. is the first fossil species in this genus known from North America and only the second fossil species described. This species possesses a broad ventral postpetiolar process which among North American extant species is only present in Manica hunteri. The Canyon Ferry ants represent the only definitively Oligocene-aged fossil deposit that contains ants in North America and therefore offer a unique view into a time when the modern-day ant communities of the continent were emerging.
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