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

基本信息

批准号：
1203910
负责人：
Robert DeConto
金额：
$ 60.37万
依托单位：
University of Massachusetts Amherst
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 2016-05-31
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=1203910&HistoricalAwards=false
关键词：
Collaborative Research P2C2 Oligocene Miocene

项目摘要

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 万年前渐新世-中新世边界发生的极端、短暂的气候振荡的研究。该事件的特点是底栖有孔虫的稳定氧同位素组成（delta18O）出现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证据海洋和陆地系统的生物影响。这次事件的规模和持续时间很短，这是不寻常的，并且明显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代理测量来解决四个首要问题：该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，该事件的严重程度是多少？鉴于当时接近现代的大气二氧化碳水平，北半球冰盖是否会增长？如果是这样，它们对底栖 delta18O 信号有何影响？如果二氧化碳水平保持在代理记录所示的低水平，那么以极地为中心的陆地冰盖怎么会经历这种变化呢？更广泛的影响包括研究生指导、参加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。