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First description of subglacial megalineations from the late Paleozoic ice age in southern Africa

机译:南部非洲古生代晚期冰期的亚冰河巨界的首次描述

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摘要

We identify late Paleozoic ice age (LPIA) subglacial megalineations from field and geospatial imagery of the Twyfelfontein area of northern Namibia, and present the results of a geomorphometric analysis of those data. Asymmetric 0.1–1.5 km-long megawhalebacks indicate a paleo-ice flow to the northwest. We infer that an ice stream draining the LPIA Kaokoveld ice sheet existed within the proto-Huab River valley and that was comparable to ice streams in modern Antarctica. Recognition of a paleo-ice stream in northern Namibia supports interpretations of glaciogenic sedimentary successions (Itararé Group) in southern Brazil that suggest the presence of major, terrestrial glacial outlet systems in southern Africa during the LPIA.
机译:我们从纳米比亚北部Twyfelfontein地区的田野和地理空间图像中识别出晚古生代冰期(LPIA)冰川下巨线,并提出了这些数据的地貌分析结果。不对称的0.1–1.5公里长的巨鲸表明西北方向有古冰流。我们推断,原华布河谷内存在一条排放LPIA Kaokoveld冰原的冰流,与现代南极洲的冰流相当。对纳米比亚北部古冰流的认识支持了巴西南部对冰川成因的沉积演替(ItararéGroup)的解释,这表明在LPIA期间南部非洲存在着主要的陆地冰川出口系统。

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