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Revisiting the role of high-energy Pacific events in the environmental and cultural history of Easter Island (Rapa Nui)

机译:重新审视高能量太平洋事件在复活节岛环境和文化史上的作用(Rapa Nui)

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摘要

Pacific islands are spread over thousands of kilometres of the Pacific Basin and are characterised by similar ecological features but very diverse geologic origins, from steep volcanoes to flat coral atolls. Several climatic phases have been shared across the region within the last 1,000years. Numerous and abrupt societal and cultural changes during the same period have been described for islands separated by thousands of kilometres. Conspicuous societal changes have been exclusively attributed to the main climatic patterns (changes in precipitation and temperature). The possible role of tsunamis and the occurrence of large volcanic eruptions as regional societal modulators, however, have traditionally received little attention from archaeologists, mainly due to the difficulty of recognising them in the sedimentary and geomorphological records. We explore the potential influence of the most important high-energy events in the Pacific on Polynesian societal changes, with a special focus on Easter Island. For example, the extreme Samalas eruption in AD 1257 may have been an indirect driver of the sudden population decline, land degradation and decreased food resources on many Pacific islands between AD 1250 and 1300, and the Kuwae eruption in AD 1450may have triggered the synchronous end of long voyaging expeditions across the Pacific. Important palaeo-tsunamis have had unquestionable impacts on coastal and seafaring societies. A direct effect of the main eruptions of the last millennia (AD 1257 and 1453) on Easter Island has not yet been identified by any record, but we have calculated the likelihood of destructive tsunamis with an estimated period of recurrence for large events of less than a century. This insight is new and needs to be taken into account to complement what we already know about Easter Island's cultural history and archaeological sites, especially those in vulnerable coastal locations.
机译:太平洋岛屿遍布成千上万公里的太平洋盆地,并以类似的生态特征为特征,而是从陡峭的火山到平珊瑚礁的地质起源。在过去的1,000年内,在整个地区共享了几个气候阶段。对于群岛分开数千公里的岛屿已经描述了同一时期的众多和突然的社会和文化变化。显着的社会变化仅归因于主要气候模式(降水和温度的变化)。然而,海啸的可能作用以及大火山爆发作为区域社会调制传统,传统上传统上从考古学家接受了很少的关注,主要是由于难以在沉积和地貌记录中认识到它们。我们探讨了太平洋最重要的高能量事件对波利尼西亚社会变化的潜在影响,特别关注复活节岛。例如,广告1257中的极端撒母马盐爆发可能是突然种群下降,土地退化和粮食资源在广告1250和1300之间的许多太平洋岛屿上的间接驾驶员,并且在AD 1450 May中的Kuwae爆发引发了同步端太平洋地区的长途旅行探险。重要的Palaeo-Tsunamis对沿海和海上社会产生了毫无疑问的影响。在复活节岛上的最后一千年(AD 1257和1453)的主要爆发的直接效应尚未通过任何记录来确定,但我们已经计算了破坏性海啸的可能性,估计的重复期限少于少于一个世纪。这种洞察力是新的,需要考虑到我们已经了解的复活节岛的文化历史和考古遗址,特别是那些在脆弱的沿海地区。

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