Collaborative Research: The Tropical Temperature History of the Cretaceous Greenhouse Interval Inferred from Tanzanian "Glassy" Foraminifera

合作研究：从坦桑尼亚“玻璃”有孔虫推断白垩纪温室区间的热带温度历史

• 批准号: 0643522
• 负责人: Liviu Giosan
• 金额: --
• 依托单位: Woods Hole Oceanographic Institution
• 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: 2007-04-15 至 2010-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0643522&HistoricalAwards=false
• 关键词: Collaborative; Research; Tropical; Temperature; History

A wealth of fossil data (terrestrial and marine) from northern and southern high latitudes provide dramatic evidence that the Cretaceous was warm. However, these fossils provide incomplete snapshots of Cretaceous climate as their occurrences are discontinuous and their distributions do not provide a quantitative measure of Earth's temperature. A more continuous history of Earth's temperature change during the Cretaceous can be inferred from delta18-O ratios preserved in the Calcium Carbonate (CaCO3) shells of foraminifera. Unfortunately, interpreting paleotemperatures from delta18-O measurements is complicated by diagenesis and uncertainties regarding the delta18-O composition of contemporary seawater. Discovery of new sites that yield Cretaceous foraminifera with truly exceptional preservation has helped address diagenetic concerns, and parallel analyses of magnesium-calcium (Mg/Ca) ratios can help separate seawater and temperature effects on measured delta18-O values. This proposal requests funds to collect, isolate, and analyze exceptionally well preserved foraminifera from up to 1150 m of Late Cretaceous cores from four key stratigraphic intervals at four localities in coastal Tanzania. Results generated will greatly improve temporal and spatial control of the Cretaceous tropical temperature record. Such improvement is necessary to advance our understanding of the linkages between climate forcing mechanisms, ocean circulation, and patterns of biotic evolution and extinction in the Cretaceous greenhouse world. In combination with climate model experiments, this grant will test hypotheses regarding greenhouse climate dynamics including tropical temperature history, purported greenhouse glacial episodes, and the degree to which tropical and 'global' temperatures co-vary. This project focuses on 1) delta18-O analyses of exceptionally well-preserved foraminifera across Late Cretaceous intervals of extreme warmth and relative cold including glacial intervals, 2) parallel measurements of Mg/Ca in selected samples to help constrain changes in seawater composition, and 3) climate model experiments and data-model comparisons that will allow better evaluation of model sensitivity to Carbon Dioxide (CO2). Broader Impacts: The project involves partners from the United States (Smithsonian Museum of Natural History, University of Missouri-Columbia, and Woods Hole Oceanographic Institution), the United Kingdom (Cardiff University, Bristol University, Southampton University, and University College London), the Republic of Ireland (Trinity College Dublin), and the Tanzania Petroleum Development Corporation. The project has held regular science meetings and has enhanced the involvement of Tanzanian scientists. Graduate and undergraduate students are involved in all phases of this research, and the analyses are done at an NSF-funded stable isotope facility. Local Tanzanians are hired to support many aspects of field work. An additional benefit is improvement in the knowledge of the structural geology and stratigraphy of the southeast coastal region of Tanzania, which is useful for Tanzanian environmental policy decisions including possible hydrocarbon potential and drilling of shallow water wells.

来自北方和南方高纬度地区的大量化石数据（陆地和海洋）提供了白垩纪温暖的有力证据。然而，这些化石提供了白垩纪气候的不完整快照，因为它们的出现是不连续的，而且它们的分布不能提供地球温度的定量测量。白垩纪期间地球温度变化的更连续的历史可以从保存在有孔虫的碳酸钙（CaCO 3）壳中的δ 18-O比率推断出来。不幸的是，解释古温度从三角洲18-O测量是复杂的成岩作用和不确定性有关的三角洲18-O组成的当代海水。发现新的地点，产生白垩纪有孔虫与真正特殊的保护，有助于解决成岩问题，和镁钙（Mg/Ca）比的平行分析，可以帮助分离海水和温度的影响，测得的delta 18-O值。该提案要求提供资金，以收集、分离和分析坦桑尼亚沿海四个地点四个关键地层间隔中长达1150米的晚白垩世岩心中保存异常完好的有孔虫。所产生的结果将大大改善白垩纪热带温度记录的时间和空间控制。这种改进是必要的，以促进我们对气候强迫机制，海洋环流和白垩纪温室世界的生物进化和灭绝模式之间的联系的理解。结合气候模型实验，该赠款将测试有关温室气候动力学的假设，包括热带温度历史，所谓的温室冰川事件，以及热带和“全球”温度共同变化的程度。该项目的重点是：1）在晚白垩世极端温暖和相对寒冷的时期（包括冰川期）对保存非常完好的有孔虫进行delta 18-O分析，2）在选定的样本中平行测量Mg/Ca，以帮助限制海水成分的变化，以及3）气候模型实验和数据模型比较，这将有助于更好地评估模型对二氧化碳（CO2）的敏感性。更广泛的影响：该项目的合作伙伴来自美国（史密森尼自然历史博物馆、密苏里-哥伦比亚大学和伍兹霍尔海洋学研究所）、联合王国（卡迪夫大学、布里斯托大学、南安普顿大学和伦敦大学学院）、爱尔兰共和国（Trinity学院都柏林）和坦桑尼亚石油开发公司。该项目定期举行科学会议，并加强了坦桑尼亚科学家的参与。研究生和本科生参与了这项研究的所有阶段，分析是在NSF资助的稳定同位素设施中完成的。当地的坦桑尼亚人被雇用来支持实地工作的许多方面。另一个好处是提高了对坦桑尼亚东南沿海地区结构地质和地层学的认识，这对坦桑尼亚的环境政策决策，包括可能的碳氢化合物潜力和浅水威尔斯钻井是有用的。