SGER: Scientific Drilling for Human Origins: Exploring the Application of Drill Core Records to Understanding Hominin Evolution

SGER：人类起源的科学钻探：探索钻芯记录在了解古人类进化中的应用

• 批准号: 0725553
• 负责人: Andrew Cohen
• 金额: --
• 依托单位: University of Arizona
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2007
• 资助国家: 美国
• 起止时间: 2007-08-01 至 2010-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0725553&HistoricalAwards=false
• 关键词: SGER; Scientific; Drilling; Human; Origins

PIs propose to investigate how continental scientific drilling can be used as a tool in understanding the environmental background of human origins. This new research direction in merging earth science and paleoanthropology will involve obtaining sediment drill core samples from lake beds located on-land, close to areas of critical importance for understanding human evolution. Their efforts will be focused around critical time intervals for human origins during the last 3.5 million years. In this first phase of research, they will obtain critical site-survey and subsurface data for four key localities in Kenya and Ethiopia, essential to the success of a future drilling program, to be funded by a later proposal. They also request partial funding for a drilling workshop, to consider the technical and scientific opportunities and challenges posed by each of the sites under consideration.Prior researchers have asked the key question of why evolution of humans and their close relatives displays a pulsed pattern, with well-defined periods of extensive speciation or extinction, cultural change and geographic expansion, interspersed with long periods when relatively little change seems to occur. Is this the result of broad forcing effects of either directional environmental change (climate, etc.), the result of changes in the variability of local or regional environments, or some yet-unrecognized mechanism. These efforts have proceeded either by correlating broad-scale patterns of human evolutionary patterns with the global beat of climate variability as recorded in the continuous records of deep-sea sediment cores or, by correlating regional shifts in the fossil and archaeological record with more local patterns of environmental change, inferred from outcrop records of ancient soils, lake beds and non-hominin fossils. PIs argue for a new research direction linking the earth science and anthropology communities in addressing this central question about human origins, combining the strengths of both of the approaches above, and avoiding some of their inherent weaknesses. Their plan promotes a concerted effort to obtain drill core records from near-continuous sedimentary sequences located close to areas of critical importance for understanding hominin evolution, focused around critical time intervals for their key question above. Drill cores will provide a record that will vastly improve understanding of environmental history in the places and times where various species of our near-relatives lived. Obtaining such records from on land will provide a more detailed and resolved record than what we can currently infer from deep sea core records. Finally, because the largest number of critical events in man's evolutionary history occurred in Africa, such a drilling campaign should start in that continent. Few scientific questions can be more central to humanity than understanding where we have come from as a species, and how our environment has shaped our biological and technological evolution. Results from this proposal will pave the way for a new direction for helping researchers address these questions and will foster a new avenue for earth science/anthropology collaborations. This international drilling program has important science training opportunities for involving early-career American and African scientists in all aspects of the project. Several students will be involved in the seismic site survey exercises leading up to the workshop, and some students who are likely to join the program in post-graduate work would be able to attend the workshop. This award is co-funded by NSF's Office of International Science and Engineering.

研究所提议调查如何利用大陆科学钻探作为了解人类起源的环境背景的工具。这一融合地球科学和古人类学的新研究方向将涉及从位于陆地上的湖床获得沉积物钻孔岩芯样本，这些湖床靠近对了解人类进化至关重要的地区。他们的工作将集中在过去350万年中人类起源的关键时间间隔。在研究的第一阶段，他们将获得肯尼亚和埃塞俄比亚四个关键地点的关键现场调查和地下数据，这对未来钻井计划的成功至关重要，该计划将由稍后的提案资助。他们还要求为一个钻探研讨会提供部分资金，以考虑每个正在考虑的地点所带来的技术和科学机遇和挑战。之前的研究人员提出了一个关键问题，即为什么人类及其近亲的进化显示出脉冲模式，具有明确的广泛物种形成或灭绝，文化变迁和地理扩张的时期，其间穿插着似乎发生相对较小变化的长时期。这是任一方向的环境变化（气候等）的广泛强迫效应的结果吗？局部或区域环境变化的结果，或一些尚未认识到的机制。 这些努力要么通过将大规模的人类进化模式与深海沉积物岩心连续记录中记录的全球气候变化相关联，要么通过将化石和考古记录中的区域变化与从古土壤、湖床和非人类化石的露头记录中推断出的更局部的环境变化模式相关联。PI主张一个新的研究方向，将地球科学和人类学社区联系起来，解决关于人类起源的这个核心问题，结合上述两种方法的优点，并避免一些固有的弱点。他们的计划促进了一项协调一致的努力，以获得来自接近连续沉积序列的岩心记录，这些沉积序列位于对了解人类进化至关重要的区域附近，重点关注上述关键问题的关键时间间隔。钻井岩心将提供一个记录，将大大提高对环境历史的理解，在地方和时间，我们的近亲生活的各种物种。从陆地上获得这样的记录将提供比我们目前从深海岩心记录中推断出的更详细和更清晰的记录。最后，由于人类进化史上最大数量的关键事件发生在非洲，这样的钻探活动应该从非洲大陆开始。 对于人类来说，没有什么科学问题比了解我们作为一个物种从哪里来，以及我们的环境如何塑造了我们的生物和技术进化更重要。 这项建议的结果将为帮助研究人员解决这些问题的新方向铺平道路，并将为地球科学/人类学合作开辟新的途径。这一国际钻探项目为美国和非洲的早期职业科学家参与项目的各个方面提供了重要的科学培训机会。一些学生将参与地震现场调查演习导致研讨会，和一些学生谁是可能加入该计划的研究生工作将能够参加研讨会。该奖项由NSF国际科学与工程办公室共同资助。