Marine Isotope Stage 11 in the eastern Mediterranean Sea: Nearest analog to the present day?

地中海东部海洋同位素第 11 阶段:与当今最接近的类似物?

基本信息

项目摘要

Marine isotopic Stage 11 (MIS11), some 400,000 years ago, provides the closest analog to the Holocene in terms of the configuration of the Earth¿s orbit around the Sun and the resulting strength and variability of solar insolation. Understanding the climate of MIS11 will thus aid in assessment of human impact on global climate and of the future of the present warm period. The Mediterranean acts as an amplifier of climate signals, responding to forcing from both the North, via the North Atlantic Oscillation and from the South, through shifts of the Intertropical Convergence Zone. This unique potential of the region to record different facets of MIS11 climate has never been explored. In this project, we will generate the first high-resolution multi-proxy records from eastern Mediterranean ODP and Meteor cores, reconstructing the hydrography, climate and ecosystems of the region across the MIS11. We specifically aim to study the pattern of climate fluctuation during MIS11 as an analog of what might have been expected during the Holocene (MIS1) without human overprint. We will also determine when and how this Holocene-like interglacial ended and whether the plunge into a new ice age could have been predicted from precursor signals or events. Our results will help in evaluating scenarios of future climate change in this densely populated region, with obvious benefits to society in Mediterranean countries.
海洋同位素第11阶段(MIS11),大约40万年前,提供了最接近全新世的地球绕太阳轨道的配置以及由此产生的太阳日射强度和变化。因此,了解MIS11的气候将有助于评估人类对全球气候的影响以及目前温暖期的未来。地中海充当气候信号的放大器,通过北大西洋涛动和热带辐合带的移动对来自北方的强迫作出反应。该地区记录MIS11气候不同方面的独特潜力从未被探索过。在这个项目中,我们将从东地中海ODP和Meteor核心生成第一个高分辨率的多代理记录,重建整个MIS11地区的水文,气候和生态系统。我们的具体目标是研究MIS11期间的气候波动模式,作为在没有人类叠加的情况下可能预期的全新世(MIS1)的模拟。我们还将确定这类全新世间冰期何时以及如何结束,以及是否可以从前兆信号或事件中预测到新的冰河时代。我们的研究结果将有助于评估这个人口稠密地区未来气候变化的情景,对地中海国家的社会有明显的好处。

项目成果

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Professor Dr. Michal Kucera, Ph.D.其他文献

Professor Dr. Michal Kucera, Ph.D.的其他文献

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{{ truncateString('Professor Dr. Michal Kucera, Ph.D.', 18)}}的其他基金

Habitat partitioning among cryptic species of planktonic foraminifera in the Caribbean Sea and its consequences for the calibration and interpretation of paleoceanographic proxies (FOCS)
加勒比海浮游有孔虫神秘物种的栖息地划分及其对古海洋学代理(FOCS)校准和解释的影响
  • 批准号:
    194025893
  • 财政年份:
    2011
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Global synthesis of surface conditions and climate trends during the MIS11 interglacial (GLOSINT11)
MIS11 间冰期期间地表条件和气候趋势的全球综合 (GLOSINT11)
  • 批准号:
    178676072
  • 财政年份:
    2010
  • 资助金额:
    --
  • 项目类别:
    Priority Programmes
Ozeanographie und Geodynamik im NW Atlantik und Baffinbai - Koordinatorantrag MSM 9
西北大西洋和巴芬湾的海洋学和地球动力学 - 协调员申请 MSM 9
  • 批准号:
    65308561
  • 财政年份:
    2008
  • 资助金额:
    --
  • 项目类别:
    Priority Programmes
Ozeanography, marine micropaleontology and genetics of benthic and planktonic foraminifera in the Artic environment of the Labrador Sea and Baffin Bay (MSM 9/2)
拉布拉多海和巴芬湾北极环境中底栖和浮游有孔虫的海洋学、海洋微古生物学和遗传学(MSM 9/2)
  • 批准号:
    65226506
  • 财政年份:
    2008
  • 资助金额:
    --
  • 项目类别:
    Priority Programmes
Transfer-function approach to temperature and salinity reconstructions in the Red Sea: Constraining sea-level estimates and monitoring ITCZ variability during the last four glacial cycles
红海温度和盐度重建的传递函数方法:限制海平面估计并监测最近四个冰川周期期间 ITCZ 的变化
  • 批准号:
    24163754
  • 财政年份:
    2006
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Evolutionary and ecological significance of cryptic diversity in foraminifera: the extent and structure of genetic diversity in planktonic foraminifera
有孔虫隐秘多样性的进化和生态意义:浮游有孔虫遗传多样性的程度和结构
  • 批准号:
    21029077
  • 财政年份:
    2006
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Marine Isotope Stage 11 in the eastern Mediterranean Sea: Nearest analog to the present day?
地中海东部海洋同位素第 11 阶段:与当今最接近的类似物?
  • 批准号:
    13882877
  • 财政年份:
    2005
  • 资助金额:
    --
  • 项目类别:
    Infrastructure Priority Programmes

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  • 批准号:
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调查海洋氧同位素第 11 阶段气候突变事件的原因和结构
  • 批准号:
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细化海洋同位素阶段 5a 和 5c 峰值海平面的范围:冰川均衡调整 3D 建模的见解
  • 批准号:
    1927326
  • 财政年份:
    2019
  • 资助金额:
    --
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Reconstruction of decadal to orbital-scale climate variability during Marine Isotope Stage 9 using precisely dated multi-proxy speleothem records from Central Europe – Part II
使用来自中欧的精确日期多代理洞穴记录重建海洋同位素阶段 9 期间十年至轨道尺度的气候变化 - 第二部分
  • 批准号:
    418149488
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    2019
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Reconstructions of Antarctic sea-ice at the peak of the last interglacial (marine isotope stage 5e)
末次间冰期高峰期南极海冰的重建(海洋同位素阶段 5e)
  • 批准号:
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Variability in the Atlantic Meridional Overturning Circulation During Marine Isotope Stage 3
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    2016
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    --
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南半球海洋同位素阶段M2(~3.3 Ma):限制上新世中期温暖期短期冰川事件的气候驱动因素。
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