Collaborative Research: P2C2--The Oligocene-Miocene Boundary: Carbon-Dioxide (CO2) Sensitivity and Ice Sheet Hysteresis

合作研究：P2C2——渐新世-中新世边界：二氧化碳（CO2）敏感性和冰盖磁滞

• 批准号: 1203792
• 负责人: David Pollard
• 金额: $ 9.83万
• 依托单位: Pennsylvania State Univ University Park
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2012
• 资助国家: 美国
• 起止时间: 2012-06-01 至 2015-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1203792&HistoricalAwards=false
• 关键词: Collaborative; Research; P2C2; Oligocene; Miocene

The project is a study of an extreme, short-lived climate oscillation that occurred at the Oligocene-Miocene boundary about 23 million years ago. The event is characterized by a 150,000-year oscillation in the stable oxygen isotope composition (delta18O) of benthic foraminifera, generally thought to reflect a rapid advance and retreat in the Antarctic ice sheet, as well as a perturbation in the global carbon cycle and evidence of biotic impacts in marine and terrestrial systems. The magnitude of the event and its short duration are unusual and in apparent contradiction to our understanding of ice sheet behavior. The researchers will use proxy measurements of past climate and general circulation model simulations to address four overarching questions: What were the primary drivers of the event: carbon cycle dynamics and atmospheric carbon dioxide (CO2), orbits? What was the magnitude of the event in terms of temperature and ice volume change? Could Northern Hemispheric ice sheets have grown, given near-modern atmospheric CO2 levels at the time, and if so, what is their impact on the benthic delta18O signal? How can a polar-centered, terrestrial ice sheet experience such variability if CO2 levels remained as low as suggested by proxy records? The broader impacts include graduate student mentoring, participation in an important summer school focused on past climate history, and the development of undergraduate education modules for climate history.

该项目是对大约2300万年前在渐新世-中新世边界发生的一种极端的、短暂的气候振荡的研究。这次事件的特点是底栖有孔虫的稳定氧同位素组成(Delta18O)出现了15万年的振荡，通常被认为反映了南极冰盖的快速进退，以及全球碳循环的扰动和海洋和陆地系统生物影响的证据。这次事件的规模和持续时间很短，这显然与我们对冰盖行为的理解相矛盾。研究人员将使用过去气候和大气环流模型模拟的替代测量来解决四个首要问题：这次事件的主要驱动因素是什么：碳循环动力学和大气二氧化碳(CO2)，轨道？就温度和冰量变化而言，这次事件的强度是多少？考虑到当时接近现代的大气二氧化碳水平，北半球的冰盖可能已经增长了吗？如果是这样的话，它们对海底Delta18O信号的影响是什么？如果二氧化碳水平仍然像代理记录所建议的那样低，以极地为中心的陆地冰盖如何经历这种变化？更广泛的影响包括研究生指导，参加一个以过去气候历史为重点的重要暑期学校，以及开发气候历史本科教育模块。