Glyptotherium cylindricum (Cingulata, Glyptodontidae) from the Late Pleistocene of Guatemala: the most complete record of Glyptodontinae from Central America

Francisco Cuadrelli, J. Escamilla, A. Zurita, D. Gillette, Lorena S. Dávila
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Abstract

Abstract Glyptodontinae stand out among the lineages of Glyptodontidae in having the greatest latitudinal distribution, including participation in the Great American Biotic Interchange, with significant speciation in new migration areas. The oldest records of Glyptodontinae occur in northern South America with Boreostemma from the middle Miocene–Pliocene. A later radiation incorporated the austral representatives ‘Glyptodontidium tuberifer’, ‘Paraglyptodon’ spp., Glyptodon munizi, Glyptodon reticulatus and Glyptodon jatunkhirkhi in the late Miocene–Late Pleistocene of southern South America, and the septentrional representatives Glyptotherium texanum and Glyptotherium cylindricum in the Pliocene–Late Pleistocene of North America, Central America and northeastern South America. Although knowledge of North and South American forms has increased in recent years, records from Central America are still scarce and fragmentary. Here we describe the most complete Central American glyptodontine fossils documented to date, which were recovered from the latest Pleistocene of Guatemala. The remains comprise: (1) an incomplete skull, the right and left hemimandibles, a fragmentary pelvis, cervical and caudal vertebrae, and articulated and isolated osteoderms; (2) a fragmentary pelvis, left hind limb (incomplete autopodium) and seven caudal vertebrae; (3) most of a dorsal carapace; (4) six incomplete caudal armature rings; and (5) a left hemimandible with complete dental series. Comparative assessment indicates that these remains are referrable to G. cylindricum. The presence of this species in northern Central America and northern South America during the latest Pleistocene spans more than 2200 km, suggesting a continuous distribution across this region, at least during the Last Glacial Maximum and the early Younger Dryas. Francisco Cuadrelli [ f.cuadrelli@gmail.com ]*, Juan Escamilla [ juanitoesca@gmail.com ] and Alfredo Zurita [ aezurita74@yahoo.com ], Laboratorio de Evolución de Vertebrados y Ambientes Cenozoicos–Centro de Ecología Aplicada del Litoral (CECOAL–CONICET) y Universidad Nacional del Nordeste, Corrientes, Argentina, 3400; David D. Gillette [daviddgillette@gmail.com ], 24 W. Travertine Trail, Flagstaff, AZ 86005, USA; Lorena S. Dávila [ sylodavila@gmail.com ], Colección de Fósiles, Museo Historia Natural, Universidad de San Carlos de Guatemala, Calle Mariscal Cruz 1–56, Zona 10, Ciudad de Guatemala, Guatemala, 01010.
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危地马拉晚更新世圆柱形齿齿兽(齿齿兽目,齿齿兽科):中美洲齿齿兽科最完整的记录
摘要glyptodontiae在Glyptodontidae谱系中具有最大的纬度分布,包括参与了大美洲生物交换,在新迁移地区有显著的物种形成。Glyptodontinae最古老的记录出现在南美洲北部,其中的Boreostemma来自中新世中期-上新世。较晚的一次进化包括南美洲南部中新世-晚更新世的南方代表Glyptodontidium tuberifer、paragyyptodon spp.、Glyptodon munizi、Glyptodon reticulatus和Glyptodon jatunkhirkhi,以及北美、中美洲和南美洲东北部的上新世-晚更新世的南方代表Glyptotherium texanum和圆柱形Glyptotherium。尽管近年来对北美和南美形式的了解有所增加,但来自中美洲的记录仍然稀少且零碎。在这里,我们描述了迄今为止记录的最完整的中美洲雕齿兽化石,这些化石是在危地马拉最新更新世发现的。这些遗骸包括:(1)一个不完整的头骨,左右下颌骨,破碎的骨盆,颈椎和尾椎,以及关节和孤立的骨皮;(2)骨盆碎片、左后肢(不完整的自椎体)和7根尾椎;(3)背甲壳的大部分;(4)六个不完整的尾枢环;(5)具有完整牙系的左半下颌骨。经比较鉴定,这些遗骨属于白茅属。该物种在最新更新世期间在中美洲北部和南美洲北部的存在范围超过2200公里,表明至少在末次盛冰期和新仙女木期早期在该地区连续分布。Francisco Cuadrelli [f.cuadrelli@gmail.com]*, Juan Escamilla [juanitoesca@gmail.com]和Alfredo Zurita [aezurita74@yahoo.com], Evolución生态环境与生态环境中心实验室Ecología沿海应用(CECOAL-CONICET),阿根廷,科伦特斯,3400;大卫D.吉列[daviddgillette@gmail.com], 24 W。Travertine Trail, Flagstaff, AZ 86005, USA;Lorena S. Dávila [sylodavila@gmail.com], Colección de Fósiles,危地马拉圣卡洛斯大学自然历史博物馆,危地马拉市10区Mariscal Cruz 1-56街,危地马拉,01010。
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