Diagnosing the origin of isotopically light carbon in the South Atlantic during the last deglaciation: An oceanic or geologic source?

诊断上次冰消期期间南大西洋同位素轻碳的起源：海洋还是地质来源？

• 批准号: 1404915
• 负责人: David Lund
• 金额: $ 30.67万
• 依托单位: University of Connecticut
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2014
• 资助国家: 美国
• 起止时间: 2014-06-01 至 2017-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1404915&HistoricalAwards=false
• 关键词: Diagnosing; origin; isotopically; light; carbon

The largest increase in atmospheric CO2 in the recent geologic past occurred during the last deglaciation (from 20,000 to 10,000 years ago). As the large Northern Hemisphere ice sheets melted, atmospheric CO2 levels rose by ~30%. Despite extensive research, the underlying cause of the CO2 change has yet to be fully explained. Recent ice core results show that the CO2 rise coincided with a negative carbon isotopic excursion. Similar although larger carbon isotope anomalies occurred at surface and intermediate depths in multiple ocean basins, pointing to an oceanic source. The largest documented changes occurred from ~1 to 2 km in the Atlantic, suggesting that processes at mid-depth in this basin played a key role in the CO2 rise. Identifying the origin of the carbon isotope signal is essential to unraveling the mechanisms that drove atmospheric CO2 variability in the recent geologic past. The primary goal of this project is to use data from the Southwest Atlantic to diagnose the source of the carbon isotope anomalies during the deglaciation. The researcher team will use a depth transect of high resolution sediment cores from the Brazil Margin to evaluate the relative timing of surface and deep water signals. The team will also use radiocarbon and other chemical analyses of microfossils to infer the origin of the carbon isotope anomaly. Work will focus on testing two competing hypotheses, one that calls for carbon originating from the abyssal ocean and the other that invokes carbon from a geological reservoir. The results could transform our understanding of the climate system by constraining the source of carbon isotopic minima and therefore the driver of atmospheric CO2 variability on glacial-interglacial timescales. The educational broader impacts of the proposed work include the participation of a graduate student and two undergraduates who will pursue independent research projects that complement the overall goals of the project.

在最近的地质历史中，大气中二氧化碳的最大增加发生在最后一次冰川消退期间（从20，000年到10，000年前）。 随着北方大冰原的融化，大气中的二氧化碳水平上升了30%。 尽管进行了广泛的研究，但二氧化碳变化的根本原因尚未得到充分解释。 最近的冰芯结果表明，二氧化碳的上升与碳同位素的负偏移相吻合。 在多个洋盆的表层和中层深度也出现了类似的碳同位素异常，但异常量较大，表明有海洋来源。 有记录的最大变化发生在大西洋1至2公里处，这表明该盆地中深度的过程在CO2上升中发挥了关键作用。 确定碳同位素信号的来源对于揭示最近地质历史中驱动大气CO2变化的机制至关重要。该项目的主要目标是利用来自西南大西洋的数据来诊断冰川消退期间碳同位素异常的来源。 研究小组将使用巴西边缘高分辨率沉积物岩心的深度断面来评估表层和深层水信号的相对时间。 研究小组还将使用放射性碳和其他微体化石的化学分析来推断碳同位素异常的起源。 工作将侧重于检验两个相互竞争的假设，一个假设认为碳来自深海，另一个假设认为碳来自地质储层。这些结果可以通过限制碳同位素最小值的来源来改变我们对气候系统的理解，从而限制冰川-间冰期时间尺度上大气CO2变化的驱动因素。 拟议工作的教育更广泛的影响包括一名研究生和两名本科生的参与，他们将从事补充项目总体目标的独立研究项目。