Collaborative Research: Investigation of pCO2 Changes Since the Pliocene Based on Alkenone Carbon Isotopes

合作研究：基于烯酮碳同位素研究上新世以来的 pCO2 变化

• 批准号: 0727306
• 负责人: Mark Pagani
• 金额: --
• 依托单位: Yale University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2007
• 资助国家: 美国
• 起止时间: 2007-08-01 至 2010-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0727306&HistoricalAwards=false
• 关键词: Collaborative; Research; Investigation; pCO2; Changes

Collaborative Research: Investigation of pCO2 Changes Since the Pliocene Based on Alkenone Carbon IsotopesMark Pagani/A. Christina RaveloYale University/UC Santa CruzAbstractThis proposal seeks to reconstruct atmospheric pCO2 across the Pliocene/Pleistocene climate transition of the last 5 million years, which will provide a framework to test possible causes of the Plio-Pleistocene climatic transition. The primary objective of this proposal is to test the hypothesis that the pattern of warming during the early Pliocene warm period, as well as the subsequent cooling, was forced by a corresponding increase and decrease in pCO2. The PI's will evaluate pCO2 changes by reconstructing records of the total carbon isotopic fractionation that occurs during algal photosynthesis (Ep). The approach will be to extract and determine the carbon isotopic (d13C) values of haptophyte-derived long-chain ketone biomarkers (alkenones) obtained from a globally distributed set of DSDP and ODP cores. In addition, the carbon isotopic and Mg/Ca composition of one or more species of planktonic foraminifers will be analyzed from the same sample to constrain changes in the carbon isotopic composition of seawater and surface temperatures respectively. The difference between the d13C of alkenones and of the coeval near-surface dwelling planktonic foraminifera represents the approximate carbon isotopic fractionation that occurs during photosynthetic carbon fixation specific to alkenone-producing haptophyte algae. This technique has been used to reconstruct the magnitude of pCO2 change during the Cenozoic and is considered one of the most reliable paleo- pCO2 proxies presently available. Broader impacts include the bi-coastal collaboration between two major U.S. institutions, participation in the project by two undergraduates and a post-doc, and PI Pagani's participatetion in a middle and high school education program that will incorporate the results of this study into presentations to students and interns in the program.

合作研究：基于烯烃碳同位素mark Pagani/A的上新世以来pCO2变化研究摘要本研究旨在重建过去500万年上新世/更新世气候过渡时期的大气二氧化碳分压，这将为测试上新世-更新世气候过渡的可能原因提供一个框架。该提案的主要目的是验证上新世早期暖期的变暖模式以及随后的变冷是由二氧化碳分压的相应增减所迫的假设。PI将通过重建藻类光合作用（Ep）过程中发生的总碳同位素分馏记录来评估二氧化碳分压的变化。该方法将提取并确定从全球分布的DSDP和ODP岩心中获得的由植物衍生的长链酮生物标志物（烯酮）的碳同位素（d13C）值。此外，还将从同一样品中分析一种或多种浮游有孔虫的碳同位素和Mg/Ca组成，以分别约束海水和表面温度的碳同位素组成变化。烯酮与同时期近地表浮游有孔虫d13C的差异代表了产生烯酮的海藻在光合作用固碳过程中所特有的碳同位素分馏。该技术已被用于重建新生代pCO2的变化幅度，被认为是目前可用的最可靠的古pCO2代用物之一。更广泛的影响包括美国两大主要机构之间的两岸合作，两名本科生和一名博士后参与该项目，以及PI Pagani参与一个初中和高中教育项目，该项目将把这项研究的结果纳入对项目学生和实习生的演讲中。