Abstract The association of vertebrate remains and invertebrate traces, although less studied than other bioerosion traces, provides important paleoecological information. This report describes Cubiculum ornatum Roberts, Rogers, and Foreman 2007, Osteocallis Roberts, Rogers, and Foreman 2007 and other unidentified insect traces from the dermal skeletal remains of glyptodonts found in Uruguay. They come from the Fray Bentos Formation (Late Oligocene), the Camacho Formation (Late Miocene) and the Dolores Formation (Late Pleistocene-Early Holocene). The reported traces were likely made by sarcosaprophagous beetles, which indicate depositional conditions with dry episodes in a warm climate for the referred stratigraphical units.

中文翻译：

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来自乌拉圭的雕齿兽中的昆虫踪迹化石

摘要 脊椎动物遗骸和无脊椎动物痕迹的关联，虽然比其他生物侵蚀痕迹研究较少，但提供了重要的古生态信息。本报告描述了 Cubiculum ornatum Roberts、Rogers 和 Foreman 2007、Osteocallis Roberts、Rogers 和 Foreman 2007 以及来自在乌拉圭发现的雕齿兽皮肤骨骼遗骸的其他不明昆虫痕迹。它们来自 Fray Bentos 组（晚渐新世）、Camacho 组（晚中新世）和 Dolores 组（晚更新世-早全新世）。报告的痕迹很可能是由食肉甲虫产生的，这表明沉积条件在温暖气候下发生干燥事件，用于提及的地层单元。