Paleoclimatic Reconstruction and Archaeological Investigation at Xcoch, Puuc Region of Yucatan, Mexico: Exploratory Research into Arctic Climate Change and Maya Culture Process

墨西哥尤卡坦半岛普克地区Xcoch古气候重建与考古调查：北极气候变化与玛雅文化进程的探索性研究

• 批准号: 0940183
• 负责人: Ezra B. Zubrow
• 金额: $ 30万
• 依托单位: SUNY at Buffalo
• 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: 2009-10-01 至 2013-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0940183&HistoricalAwards=false
• 关键词: Paleoclimatic; Reconstruction; Archaeological; Investigation; Xcoch

This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5).This research project investigates climatic change from a global perspective through archaeological excavation and survey in the Puuc region of Yucatan, Mexico and at the Maya center of Xcoch. Climate change in the Arctic is not just a contemporary phenomenon, such change had social and cultural consequences for many past human societies far from northern Polar Regions, including the Maya lowlands. Changing climate facilitated Norse colonization of the North Atlantic Islands during the Medieval Warm Period (AD 800-1300). At about the same time, the Maya of Yucatan, Mexico, were experiencing disruptions to rainfall patterns leading to sustained periods of drought. How Arctic climate change affected processes of cultural development and decline in the North Atlantic and Maya Lowlands has the potential to inform us today regarding the far reaching and serious cultural-environmental impact of global climate change. Climate data from places like the Puuc region, characterized as a semi-arid tropical climate and dry forest vegetation that suffers from a long precarious dry season, has the potential to inform us about the complex effects that Arctic climate change had and has on the global climate system. Climate change has long been seen as a major factor in the decline of ancient Maya civilization. Cycles of drought affecting agriculture and available drinking water in particular are believed to have being critical in the phenomenon known as the Classic Maya collapse beginning around the 9th century AD. The site of Xcoch is uniquely suited for climatic change research because it had a long occupation but experienced significant depopulations by the 9th century, contains a deep cave to a permanent water source, and there are many ponding features (aguadas); all these factors give Xcoch the potential to provide long-term paleoclimatic information. The nearby centers of Uxmal, Muluch Tzekel, and Xuch also contain aguadas and there are several other deep caves in the region that will be tested. This work is largely based upon new, untested ideas and has never been tried in the Yucatan but involves new approaches, requires diverse expertise, and engages interdisciplinary perspectives. Survey and excavation at Xcoch will resume in 2009 when multidisciplinary climate change data will be collected, analyzed, and compared with northern data. This research engages the Arctic community because it is becoming increasingly apparent that Arctic climate changes have global culture-environmental impacts. In order to fully understand what those impacts are, interdisciplinary and cross regional investigations, such as the proposed project, need to take place both in the north and in the south engaging the scientific community in a global discussion. The data that the PI expects to uncover at Xcoch will be added to this ongoing discussion with northern scientists. This research is viewed as potentially transformational, connecting what up to this point have been primarily regionalized archaeological research on the affects of climate change on local social and cultural systems, the Xcoch project will attempt globalize this research by connecting the north with the south.

该奖项是根据2009年美国复苏和再投资法案（公法111-5）资助的。该研究项目通过在墨西哥尤卡坦州Puuc地区和Xcoch玛雅中心的考古发掘和调查，从全球角度研究气候变化。北极的气候变化不仅仅是一个当代现象，这种变化对远离北方极地地区的许多过去的人类社会，包括玛雅低地，都产生了社会和文化后果。中世纪温暖时期（公元800-1300年），气候变化促进了挪威人对北大西洋岛屿的殖民化。大约在同一时间，墨西哥尤卡坦半岛的玛雅人正经历着降雨模式的中断，导致持续的干旱。北极气候变化如何影响北大西洋和玛雅低地的文化发展和衰落进程，有可能告诉我们今天关于全球气候变化的深远和严重的文化环境影响。来自Puuc地区等地的气候数据具有半干旱热带气候和干燥森林植被的特点，遭受长期不稳定的旱季，有可能告诉我们北极气候变化对全球气候系统的复杂影响。长期以来，气候变化一直被视为古玛雅文明衰落的主要因素。干旱周期影响农业，特别是可获得的饮用水，被认为是公元世纪左右开始的古典玛雅崩溃现象的关键。Xcoch的网站是唯一适合气候变化研究，因为它有一个长期的占领，但经历了显着的人口减少到第9世纪，包含一个深洞的永久水源，并有许多积水功能（aguadas）;所有这些因素给Xcoch提供长期的古气候信息的潜力。附近的Uxmal，Muluch Tzekel和Xuch中心也包含aguadas，该地区还有其他几个深洞将被测试。这项工作主要是基于新的，未经测试的想法，从来没有在尤卡坦半岛尝试过，但涉及新的方法，需要不同的专业知识，并从事跨学科的观点。2009年将恢复Xcoch的调查和挖掘工作，届时将收集、分析多学科气候变化数据，并与北方数据进行比较。这项研究吸引了北极社区，因为北极气候变化对全球文化环境的影响越来越明显。 为了充分了解这些影响是什么，需要在北方和南方进行跨学科和跨区域的调查，如拟议的项目，使科学界参与全球讨论。PI希望在Xcoch发现的数据将被添加到与北方科学家正在进行的讨论中。 这项研究被认为是潜在的变革，连接到这一点上已经主要是区域化的考古研究气候变化对当地社会和文化系统的影响，Xcoch项目将试图通过连接北方与南方全球化的研究。