LATE PLIOCENE (BLANCAN) VERTEBRATE FAUNAS FROM PEARSON MESA, HIDALGO COUNTY, NEW MEXICO AND GREENLEE COUNTY, ARIZONA

G. Morgan, P. Sealey, S. Lucas
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Abstract

Exposures at Pearson Mesa in the Duncan basin along the New Mexico-Arizona border have produced a diverse assemblage of late Pliocene (Blancan) vertebrates. The stratigraphic section at Pearson Mesa consists of more than 60 m of sandstones, mudstones, and sedimentary breccias of the Gila Group. Two distinct vertebrate faunas occur at Pearson Mesa: the early late Blancan Pearson Mesa Local Fauna (LF) is derived from the lower 15 m of the stratigraphic section and the latest Blancan Virden LF occurs in the upper 20 m of the section. The Pearson Mesa fauna consists of 25 species: 3 land tortoises ( Gopherus and two species of Hesperotestudo ); box turtle ( Terrapene ); colubrid snake; bird; and 19 mammals. Age-diagnostic mammals from the Pearson Mesa LF include: the ground sloth Paramylodon cf. P. garbanii ; the pocket gopher Geomys persimilis ; the cotton rat Sigmodon medius ; the three-toed horse Nannippus peninsulatus ; the one-toed horses Equus cf. E. cumminsii , and E. simplicidens ; and the peccary Platygonus bicalcaratus . The association of Paramylodon and Nannippus defines a restricted interval of time in the Blancan between the first appearance of South American immigrants (including Paramylodon ) in the southwestern US at ~3.0 Ma and the extinction of Nannippus at ~2.2 Ma. Magnetostratigraphy further constrains the age of the Pearson Mesa LF, with five normally-magnetized samples from the lower part of the section referred to the uppermost Gauss Chron (Chron 2An.1n; 2.58-3.04 Ma). Southwestern early late Blancan faunas (~2.6-3.0 Ma) correlative with Pearson Mesa include: Anapra, NM; Wolf Ranch and 111 Ranch, AZ; and Cita Canyon and Hudspeth, TX. A 10-m-thick sedimentary breccia overlying the Pearson Mesa LF lacks fossils and may represent a hiatus. The Virden LF consists of 22 species: toad; large Hesperotestudo ; Terrapene ; colubrid snake; lizard; two birds; and 15 mammals. A latest Blancan age (~1.8-2.2 Ma) for the Virden LF is indicated by the presence of the dwarf cotton rat Sigmodon minor and the small camelid Hemiauchenia gracilis , both restricted to latest Blancan faunas, and the association of the glyptodont Glyptotherium arizonae with the coyotelike canid Canis lepophagus . Southwestern latest Blancan faunas correlative with Virden include: La Union, NM and Curtis Ranch and San Simon, AZ.
新墨西哥州伊达尔戈县皮尔森台地和亚利桑那州格林利县晚上新世(白垩纪)脊椎动物区系
在新墨西哥州和亚利桑那州交界的邓肯盆地的皮尔森梅萨暴露,产生了上新世晚期(布兰坎)脊椎动物的多样化组合。Pearson Mesa的地层剖面包括60多米的Gila群的砂岩、泥岩和沉积角砾岩。皮尔逊台地有两种不同的脊椎动物区系:早、晚布兰卡地区皮尔逊台地本地动物群(LF)来自地层剖面的下15 m,而最新的布兰卡地区Virden动物群出现在地层剖面的上20 m。皮尔逊平原区动物群由25种组成:3种陆龟(Gopherus和2种Hesperotestudo);箱龟;无毒蛇的蛇;鸟;还有19种哺乳动物。Pearson Mesa LF的年龄诊断哺乳动物包括:地懒parylodon cf. P. garbanii;口袋地鼠(Geomys persimilis);棉鼠Sigmodon medium;三趾马南尼普斯半岛;单趾马(Equus cf. E. cumminsii)和单趾马(E. simplicidens);以及pecary platgonus bicalcaratus。副齿龙和南齿龙的结合定义了布兰坎地区南美移民(包括副齿龙)首次在美国西南部出现(约3.0 Ma)和南齿龙灭绝(约2.2 Ma)之间的一个有限时间间隔。磁地层进一步限制了Pearson Mesa LF的年龄,剖面下部的5个正常磁化样品指的是最上层的高斯时程(Chron 2An.1n;2.58 - -3.04 Ma)。与Pearson台地相关的西南早晚布兰坎动物群(~2.6 ~ 3.0 Ma)包括:Anapra, NM;狼牧场和111牧场,亚利桑那州;盖在皮尔逊台地LF上的一块10米厚的沉积角砾岩缺乏化石,可能代表了一个裂谷。Virden LF由22种组成:蟾蜍;大Hesperotestudo;Terrapene;无毒蛇的蛇;蜥蜴;两只鸟;还有15种哺乳动物。结果表明,在该地区发现的侏儒棉鼠Sigmodon minor和小骆驼科Hemiauchenia gracilis,以及glyptodon Glyptotherium arizonae与土狼类犬科Canis lepophagus存在关联,表明该地区的Blancan年龄较晚(~1.8 ~ 2.2 Ma)。与Virden相关的最新西南部布兰坎动物群包括:La Union, NM和Curtis Ranch以及San Simon, AZ。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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