Evaluating SW Ethiopia as a Late Quaternary Refugium: Archaeology and Paleoenvironment

将埃塞俄比亚西南部评估为晚第四纪避难所：考古学和古环境

• 批准号: 0553371
• 负责人: Steven Brandt
• 金额: --
• 依托单位: University of Florida
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2006
• 资助国家: 美国
• 起止时间: 2006-05-01 至 2009-04-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0553371&HistoricalAwards=false
• 关键词: Evaluating; SW; Ethiopia; Late; Quaternary

During the late Pleistocene (~125-10,000 years ago), the African continent experienced major fluctuations in climate, from warm and humid to very dry and cold conditions. How anatomically modern humans adapted biologically and culturally to these changes has been a subject of considerable interest and significance. For example, some scholars argue that the cold, dry conditions of 70-60 ka may have been the context of early Later Stone Age/Upper Paleolithic technological and social innovations that allowed Homo sapiens to leave Africa during subsequent warm periods to populate Eurasia and eventually the Americas. Others suggest similar cold and arid conditions during the last glacial maximum ~ 20-11,000 years ago depopulated much of Northern and Eastern Africa until warmer and wetter conditions of the early Holocene allowed for the rapid migration of hunter-gatherers into former deserts and other diverse environments..During cold, dry periods, where did people live? How did their behavior change? In comparison to research on major population dispersals during warm and humid periods, little attention has been directed at identifying potential refugia, reconstructing their prehistoric environments, checking whether people lived there during prehistoric arid periods, and examining how they used local resources. Modern and ancient climate and circulation data suggest that Southwestern Ethiopia captured significant rainfall during arid periods when much of Northern and Eastern Africa had desert conditions. SW Ethiopia, with forest patches and resources absent elsewhere in the Horn, may have constituted a refugium for Northern and Eastern African human populations 70-60 ka and 20-11 ka. To evaluate this hypothesis, the researchers propose to gather archaeological and paleoclimatic data for the period bracketing the Last Glacial Maximum (30-5 ka), to test whether Southwestern Ethiopia was a refugium during this hyperarid period, and provide analogical information to guide future research on earlier arid periods.The group will use multiple, independent lines of evidence to create chronologically secure sequences of environmental change and human behavior for a little-studied region of potentially major significance to the survival of African human populations of the late Quaternary. The research will also be relevant to other archaeological/anthropological issues: such as: 1) environments and human behaviors in previous and subsequent arid periods in Africa, 2) global comparisons of Pleistocene refugia, 3) environmental and social contexts of subsistence change prior to plant domestication, and 4) the origins of the enormous genetic, linguistic, and cultural diversity of today's peoples of the Horn of Africa.This project will also promote international collaboration between American, European, and Ethiopian scholars, and will stimulate the development of Ethiopian research and education by involving senior Ethiopian scholars and graduate students. The research group will work with local people to create archaeology exhibits and enhance other displays in 3 rural museums, improving local Ethiopians' ability to contribute to and access information about prehistory and cultural heritage. Proposed ecological studies of threatened natural areas may also contribute to their conservation. Finally, this project will raise the profile of the cultures, history, and prehistory of southern Ethiopia, a region long marginalized in Ethiopian history. Finally, this research will contribute to global discussions of sudden climatic change and human responses past and present, a topic vital to food security and political stability around the world.

在更新世晚期（约125- 10，000年前），非洲大陆经历了气候的重大波动，从温暖潮湿到非常干燥和寒冷的条件。现代人类在解剖学上如何在生物学和文化上适应这些变化，一直是一个相当有趣和重要的课题。例如，一些学者认为，70-60 ka的寒冷，干燥的条件可能是早期晚石器时代/旧石器时代晚期技术和社会创新的背景，使智人在随后的温暖时期离开非洲，居住在欧亚大陆，最终到达美洲。另一些人认为，大约20- 11，000年前末次盛冰期期间类似的寒冷和干旱条件使北方和东非大部分地区人口减少，直到全新世早期温暖和潮湿的条件允许狩猎采集者迅速迁移到以前的沙漠和其他不同的环境。在寒冷干燥的时期，人们住在哪里？他们的行为如何改变？与研究温暖和潮湿时期的主要人口扩散相比，很少有人关注确定潜在的避难所，重建史前环境，检查史前干旱时期是否有人居住在那里，以及研究他们如何使用当地资源。现代和古代的气候和环流数据表明，埃塞俄比亚西南部在干旱时期获得了大量的降雨，而北方和东部非洲的大部分地区都是沙漠。埃塞俄比亚西南部的森林斑块和资源在非洲之角的其他地方都没有，可能是北方和东非人口70-60 ka和20-11 ka的避难所。为了评估这一假设，研究人员建议收集末次冰期最大期（30-5 ka）的考古和古气候数据，以测试埃塞俄比亚西南部在这个极端干旱时期是否是一个避难所，并提供类比信息以指导未来对早期干旱时期的研究。独立的证据线，以创建环境变化和人类行为的时间顺序安全序列的一个很少研究的地区的潜在重大意义的生存非洲人类人口的第四纪晚期。 该研究还将与其他考古学/人类学问题相关：例如：1）非洲先前和随后干旱时期的环境和人类行为，2）更新世避难所的全球比较，3）植物驯化之前生存变化的环境和社会背景，以及4）巨大的遗传，语言，该项目还将促进美国、欧洲和埃塞俄比亚学者之间的国际合作，并将通过吸收埃塞俄比亚高级学者和研究生参与，促进埃塞俄比亚研究和教育的发展。该研究小组将与当地人民合作，在3个农村博物馆创建考古展品，并加强其他展览，提高当地居民对史前史和文化遗产的贡献和获取信息的能力。拟议对受威胁的自然地区进行的生态研究也可能有助于保护这些地区。最后，该项目将提高埃塞俄比亚南部的文化，历史和史前史的形象，这是一个长期被埃塞俄比亚历史边缘化的地区。最后，这项研究将有助于全球讨论气候突然变化和人类过去和现在的反应，这是一个对世界粮食安全和政治稳定至关重要的话题。