Doctoral Dissertation Improvement Grant: The Archaeology of Local Human Response to a Global Environmental Transformation

博士论文改进补助金：当地人类对全球环境转变反应的考古学

• 批准号: 0941208
• 负责人: C Michael Barton
• 金额: $ 1.46万
• 依托单位: Arizona State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2009
• 资助国家: 美国
• 起止时间: 2009-09-01 至 2011-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0941208&HistoricalAwards=false
• 关键词: Doctoral; Dissertation; Improvement; Grant; Archaeology

This project is a case study designed to identify the dynamics of local subsistence adaptations to the climate-induced environmental transformation of the Pleistocene-Holocene transition. Set in the Mediterranean region of southeast Spain, it includes two systematic archaeological surveys and the geochemical analysis of stone tools collected during the past decade of archaeological research in the study area. The surveys sample the sources of raw material, from which stone tools were made, along three natural corridors connecting major ecological zones from the Mediterranean coast through the mountains to Spain's interior plain and establish the archaeological presence or absence of late Pleistocene human groups where the natural corridors intersect the interior plain. Each survey is the first of its kind in the region. Two previous pilot projects leading to the current dissertation project have helped pioneer the use of Proton Induced X-ray Emission (PIXE) analysis to produce quantifiable geochemical signatures from stone tools and the raw material used to make them. Geochemical signatures are used here to link archaeological sites on a chronological scale, to track the movement and land-use patterns of human groups, and to establish the economic territories of groups with access to specific raw material sources.The Pleistocene-Holocene transition is the only previous global environmental transformation confronted by modern humans - making it the best available analog for understanding potential human reactions to future climate change. However, late Pleistocene archaeological records in most of Europe are dominated by the Last Glacial Maximum (LGM), which forced major shifts in demography. Human populations abandoned continental Europe west of the Ural Mountains at the LGM and packed into defined refugium areas. As the ice receded, and the Pleistocene began its transition to the Holocene climate regimes in which we now live, refugia populations dispersed outward and recolonized Europe. Mediterranean Spain was an exception, where the interval between late Pleistocene and early Holocene remained a relative continuum. For example, no territory in the study area was excluded from the subsistence base by glaciation. Changes in land-use can be considered responses to the ecological aspects of climate transformation and not simply a response to newly available land. As a result, Mediterranean Spain is a natural venue for studying the ecodynamics of human adaptation to the Pleistocene-Holocene transition.Resilience in subsistence adaptations is a function of access to sufficient resources. Viewed from this perspective, late Pleistocene and early Holocene hunter-gatherer subsistence economies balanced a set of variables roughly analogous to those of local subsistence economies in climate-sensitive developing nations today. Exponential changes in population density between the Holocene and now redefine what is sufficient, as differences in technology modify the degree and pathways of access, but neither alters the fundamental relationships. An archaeological perspective allows a better understanding of ultimate, rather than proximate, causes of social and ecological system resilience - and that is the broader impact of this research. It recognizes global climate transformation as a challenge that local human groups have previously confronted, and it creates a conceptual framework within which to examine the decision-making processes and that allowed them to adapt in a world of unprecedented change.

该项目是一项个案研究，旨在确定当地生存适应更新世-全新世气候引起的环境转变的动态。它位于西班牙东南部的地中海地区，包括两次系统的考古调查，以及对过去十年研究地区考古研究期间收集的石器进行的地球化学分析。这些调查沿着从地中海海岸通过山脉连接主要生态区到西班牙内陆平原的三条自然走廊采样原材料的来源，并确定在自然走廊与内陆平原相交的地方是否存在晚更新世人类群体。每一次调查都是该地区此类调查的第一次。导致本次论文项目的前两个试点项目帮助开创了使用质子诱导X射线发射(PIXE)分析的先河，以从石器和制造石器的原材料中产生可量化的地球化学特征。在这里，地球化学特征被用来在时间尺度上连接考古遗址，跟踪人类群体的迁徙和土地利用模式，并建立能够获得特定原材料来源的群体的经济领土。更新世-全新世的转变是现代人面临的唯一以前的全球环境变化-使其成为了解人类对未来气候变化的潜在反应的最佳可用模拟。然而，欧洲大部分地区的晚更新世考古记录都是由末次冰盛期(LGM)主导的，这迫使人口结构发生了重大变化。人们在LGM上抛弃了乌拉尔山脉以西的欧洲大陆，涌入了划定的避难区。随着冰川消退，更新世开始向我们现在所处的全新世气候制度过渡，避难者人口向外分散，重新殖民欧洲。地中海西班牙是一个例外，在那里，晚更新世和早全新世之间的时间间隔仍然是一个相对连续的时期。例如，研究区域内没有任何领土因冰川作用而被排除在生存基地之外。土地利用的变化可以被认为是对气候变化的生态方面的反应，而不仅仅是对新获得的土地的反应。因此，地中海西班牙是研究人类适应更新世-全新世过渡的生态动力学的天然场所。生存适应的适应性是获得足够资源的函数。从这个角度来看，晚更新世和早全新世狩猎采集自给自足经济平衡了一系列变量，大致类似于今天对气候敏感的发展中国家的当地自给自足经济。从全新世到现在，人口密度的指数变化重新定义了什么是足够的，因为技术差异改变了获取的程度和途径，但都没有改变基本关系。从考古学的角度可以更好地理解社会和生态系统复原力的根本原因，而不是近因--这就是这项研究的更广泛影响。它认识到全球气候变化是当地人类群体以前面临的挑战，并创建了一个概念框架，在这个框架内审查决策过程，使他们能够适应一个前所未有的变化的世界。