RUI: Using opal and organic carbon as proxies for wind-driven upwelling during the onset and termination of the African Humid Period in a transect of African margin cores

RUI：使用蛋白石和有机碳作为非洲边缘核心样带非洲湿润期开始和结束期间风驱动上升流的代表

• 批准号: 1103262
• 负责人: Louisa Bradtmiller
• 金额: $ 13.74万
• 依托单位: Macalester College
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-08-15 至 2015-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1103262&HistoricalAwards=false
• 关键词: RUI; Using; opal; organic; carbon

Marine and terrestrial records from northern Africa have greatly enhanced our understanding of both the causes and effects of climate change in the geologic past. Specifically, proxy records of changes in paleoproductivity yield information about upwelling strength, and therefore wind strength along the North African margin. Changes in wind strength, in turn, have been shown to correlate with changes in the relative aridity of the Sahel: periods of increased precipitation in the past were periods of weaker trade winds and decreased upwelling, and vice verse. Today the population of the Sahel region is highly vulnerable to changes in effective precipitation, making it all the more important to understand the connections between aridity, wind-strength, and climate change, and how abruptly changes can occur.This work, led by an early career faculty member at Macalester College in Minnesota, focuses on the environmental changes associated with the African Humid Period (AHP, 11,000 to 5,000 years before present), a time when northern Africa was characterized by a much wetter environment than it is today. Specifically, the work will assess the timing and abruptness of changes in upwelling associated with the onset and termination of the AHP across a 20-degree span of latitudes along the northwest African margin. The lead researcher will determine changes in upwelling intensity using the percentages of opal and organic carbon preserved in sediment cores, and combine these data with 230Th data from a separately funded project to calculate fluxes of each constituent. These efforts will provide an extraordinarily rich and detailed dataset of proxies related to wind strength, upwelling, and aridity in the Sahel region throughout the deglaciation and the Holocene. In terms of broader impact, this project will offer the opportunity for a number of undergraduates at a small mid-western liberal arts college to engage in ocean sciences research. Funding also supports collaboration between two early career scientists.

来自北方非洲的海洋和陆地记录大大增强了我们对地质历史中气候变化的原因和影响的理解。具体而言，代理记录的古生产力的变化产生的信息上涌强度，因此风强度沿着北非边缘。风力的变化反过来又与萨赫勒地区相对干旱的变化相关：过去降水增加的时期是信风减弱和上升流减少的时期，反之亦然。今天，萨赫勒地区的人口极易受到有效降水变化的影响，因此了解干旱、风力和气候变化之间的联系以及变化如何突然发生变得更加重要。这项工作由明尼苏达州麦卡莱斯特学院的一名早期教师领导，重点关注与非洲湿润期相关的环境变化（AHP，距今11,000至5,000年前），当时北方非洲的特点是环境比今天潮湿得多。具体而言，这项工作将评估上升流的变化的时间和准确性与AHP的开始和终止跨越20度的纬度沿着西北非洲边缘。首席研究员将使用沉积物芯中保存的蛋白石和有机碳的百分比来确定上升流强度的变化，并将这些数据与来自单独资助的项目的230 Th数据结合联合收割机来计算每种成分的通量。这些努力将提供一个非常丰富和详细的数据集代理有关的风力，上升流，干旱在整个冰川消退和全新世萨赫勒地区。就更广泛的影响而言，该项目将为中西部一所小型文理学院的一些本科生提供从事海洋科学研究的机会。资金还支持两名早期职业科学家之间的合作。