Re-organization of ocean circulation during the Miocene transition from Greenhouse to Icehouse: The role of the Indian Ocean

中新世从温室到冰室过渡期间海洋环流的重组：印度洋的作用

• 批准号: 319889890
• 负责人: Professor Dr. Wolfgang Kuhnt
• 金额: --
• 依托单位: Arbeitsgruppe Marine Mikropaläontologie
• 依托单位国家: 德国
• 项目类别: Infrastructure Priority Programmes
• 财政年份: 2016
• 资助国家: 德国
• 起止时间: 2015-12-31 至 2019-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/319889890?language=en
• 关键词: Re; organization; ocean; circulation; during

We will test the overarching hypothesis that the boundary conditions for the modern global ocean-atmosphere circulation were established during the middle-late Miocene in a stepwise manner, involving threshold changes in inter-ocean heat and carbon transfer. To achieve this goal, we will create continuous, high resolution, orbitally tuned deep water paleoceanographic (benthic stable isotope supplemented by benthic Mg/Ca) time series for the middle to late Miocene interval in the newly drilled Site U1443 in the central Indian Ocean. Previous low-resolution studies indicated that the bottom water saturation state in Indian Ocean deep and intermediate waters experienced a maximum during the Miocene Climate Optimum and decreased stepwise during the late Miocene in line with declining atmospheric pCO2 levels, global cooling and cryosphere expansion. The complete record of Site U1443 is ideally suited to assess changes in inter-ocean heat and carbon gradients and, thus, to evaluate the global extent of large-scale deep ocean carbon isotope changes and their phase relationship to benthic oxygen isotope fluctuations. In particular, we intend to test the hypotheses that the deep Indian Ocean played a crucial role in the storage and transfer of heat and carbon during the middle-late Miocene climate transition and, thus, mediated the transition between different equilibrium states of the ocean/climate system.

我们将测试的总体假设，现代全球海洋-大气环流的边界条件是在中新世中晚期逐步建立的，涉及到海洋间热量和碳转移的阈值变化。为了实现这一目标，我们将创建连续的，高分辨率的，轨道调谐深水古海洋（底栖稳定同位素补充底栖镁/钙）时间序列中晚中新世的间隔在新钻探的站点U1443在印度洋中部。以前的低分辨率研究表明，在印度洋深水和中层沃茨的底层水饱和度状态经历了一个最大的中新世气候最佳和逐步下降，在晚中新世与大气pCO 2水平下降，全球冷却和冰冻圈扩张。U1443站点的完整记录非常适合于评估大洋间热量和碳梯度的变化，从而评估大规模深海碳同位素变化的全球范围及其与海底氧同位素波动的相位关系。特别是，我们打算测试的假设，深印度洋在中晚中新世气候转变过程中的热量和碳的储存和传输中发挥了至关重要的作用，从而介导了海洋/气候系统的不同平衡状态之间的过渡。

项目成果

The Middle to Late Miocene “Carbonate Crash” in the Equatorial Indian Ocean

• DOI: 10.1029/2018pa003482
• 发表时间: 2019-05
• 期刊: Paleoceanography and Paleoclimatology
• 影响因子: 3.5
• 作者: J. Lübbers;W. Kuhnt;A. Holbourn;C. Bolton;E. Gray;Y. Usui;K. Kochhann;S. Beil;N. Andersen