通往内陆的道路:巴布亚新几内亚马当省Simbai-Kaironk山谷的人类定居点

IF 1.1 3区 历史学 Q2 ANTHROPOLOGY Australian Archaeology Pub Date : 2021-12-09 DOI:10.1080/03122417.2021.2007600
Judith H. Field, Ben Shaw, G. Summerhayes
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引用次数: 2

摘要

新几内亚已经发现了人类在Sahul(更新世澳大利亚-新几内亚)存在的最早证据,北海岸是东南亚可能的殖民路线之一。在新几内亚已知的末次冰期(≥30kya)前考古遗址中,只有少数来自高地。连接北部海岸和中部科迪勒拉的通航通道,特别是“草原走廊”,可能促进了定居,但人们对这些走廊内边缘山区山谷的人类定居知之甚少。在北部山区边缘的Simbai-Kaironk山谷(海拔2000 - 1600米)进行的一项调查和挖掘计划确定了21公里走廊上的51个地点。放射性碳定年法表明,在31 ka时可能有人类存在,在17 - 15 ka期间有景观使用的明确证据,并且在中全新世时期遗址密度增加。大多数地点都是开放的,全新世的定居点位于海拔高度,可以优化山地森林、草原和低地资源。我们认为,自晚更新世以来,辛拜-凯隆克草原走廊为进入中部高原山谷提供了便利。更短和更直接的路径,通过突出的低洼地带横贯河谷,以及与之相关的虫媒疾病,很可能促进了整个全新世的海岸-高地运动。
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Pathways to the interior: Human settlement in the Simbai-Kaironk Valleys of the Madang Province, Papua New Guinea
Abstract New Guinea has yielded some of the earliest evidence for a human presence in Sahul (Pleistocene Australia-New Guinea), with the north coast being one of the likely colonisation routes from Southeast Asia. Of the known pre-Last Glacial Maximum (≥30kya) archaeological sites from New Guinea, only a handful come from the Highlands. Navigable pathways linking the north coast to the central cordillera, specifically ‘grassland corridors’, may have facilitated settlement, yet little is known about human settlement of fringe montane valleys within these corridors. A survey and excavation program within the Simbai-Kaironk Valleys (2,000–1,600 m asl) on the northern montane fringe identified 51 sites across a 21 km corridor. Radiocarbon dating suggests a possible human presence from 31 ka, clear evidence for landscape use from 17 to 15 ka, and an increase in site density from the Mid-Holocene. Most sites were from open settings, with Holocene settlements positioned at elevations optimising access to montane forests, grasslands and lowland resources. We argue that the Simbai-Kaironk grassland corridor has facilitated access to the central Highland valleys since the Late Pleistocene. Shorter and more direct pathways, transecting the river valleys via prominent spurs rising above the lowlands – and their associated insect-borne diseases – are likely to have facilitated coastal-Highland movement throughout the Holocene.
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9.10%
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