Modelling the impact of large-scale hydroclimate change on prehistoric Polynesian island life

Charlotte V. Hipkiss , Justin Sheffield , Peter Langdon , David Sear
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Abstract

The South Pacific was one of the last regions on earth to be colonised by humans and offers a unique opportunity to study early climate-human interactions in environments previously untouched by people. Palaeoclimate evidence suggests the South Pacific has experienced shifts between dry and wet periods throughout the past three thousand years, the broad period of colonisation, with extremes in both modes being prevalent. Drought has significant repercussions for small Pacific islands, affecting water and food resources, with potential consequences on the viability of life on these islands leading to internal stress, conflict, collapse or migration. Previously, socio-ecological models have been developed to test mechanisms of change within prehistoric societies worldwide that can lead to migration or societal change, but thus far the connections between past climatic change and prehistoric island life within the tropical South Pacific have not been fully explored. This study utilises palaeoclimatic data alongside a new system dynamics socio-ecological model to explore the relationship between climate, agricultural carrying capacity and population dynamics on the Polynesian island of Mangaia (Cook Islands) in the tropical South Pacific. Model results suggest that as the population density of the island increases, the impact of drought events on population dynamics increases. We also show that the severity of the drought rather than the return frequency drove the largest changes in carrying capacity and population dynamics. Changes in long-term rainfall leading to persistent dry conditions impacted the timing and rate of population growth due to its role as a limiting factor for agricultural productivity. We compare our modelled results with the known history of population stress and societal change from Mangaia and found these corresponded with drought periods and low food availability. We demonstrate the potential for droughts to have impacted on the early colonisation and societal change on Eastern Polynesian islands.
模拟大规模水文气候变化对史前波利尼西亚岛屿生活的影响
南太平洋是地球上最后一个被人类殖民的地区之一,它提供了一个独特的机会来研究早期气候-人类在以前未被人类接触过的环境中的相互作用。古气候证据表明,在过去的三千年里,南太平洋经历了干湿交替的时期,这是一个广泛的殖民时期,两种模式的极端情况都很普遍。干旱对太平洋小岛屿产生重大影响,影响到水和粮食资源,对这些岛屿上生命的生存能力造成潜在后果,导致内部压力、冲突、崩溃或移徙。以前,社会生态模型已经被开发出来,以测试世界范围内史前社会的变化机制,这些变化可能导致移民或社会变化,但到目前为止,过去的气候变化与热带南太平洋史前岛屿生活之间的联系还没有得到充分的探索。本研究利用古气候数据和一个新的系统动力学社会生态模型来探索热带南太平洋曼加亚(库克群岛)的波利尼西亚岛的气候、农业承载能力和人口动态之间的关系。模型结果表明,随着岛上人口密度的增加,干旱事件对人口动态的影响增加。我们还表明,干旱的严重程度而不是回归频率驱动了承载能力和种群动态的最大变化。由于长期降雨是农业生产力的限制因素,因此导致持续干旱条件的变化影响了人口增长的时间和速度。我们将我们的模型结果与来自Mangaia的已知人口压力和社会变化的历史进行了比较,发现这些与干旱时期和低粮食供应相对应。我们展示了干旱对东波利尼西亚群岛早期殖民和社会变革的潜在影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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