D. Hodell, J. Nicholl, T. Bontognali, Steffan Danino, J. Dorador, J. Dowdeswell, J. Einsle, H. Kuhlmann, B. Martrat, M. J. Mleneck-Vautravers, F. Rodríguez-Tovar, U. Röhl
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引用次数: 120
摘要
这项研究使用了在德国不来梅大学海洋环境科学中心的XRF岩心扫描仪实验室获得的数据。这项研究使用了国际海洋探索计划（IODP）提供的样本。这项研究的资金由英国自然环境研究委员会（NERC）提供给霍德尔。NERC放射性碳基金会支持了两个放射性碳日期，Wally Broecker在科默家庭基金会的资助下慷慨支持了其余日期。Rodriguez Tovar和Dorador的研究由CGL2015-66835-P项目资助。B.M.感谢CSIC Ramon y Cajal博士后项目RYC-2013-14073的支持。J.F.E.感谢ERC高级拨款320750-纳米磁。
Anatomy of Heinrich Layer 1 and its role in the last deglaciation
This research used data acquired at the XRF Core Scanner Lab at the MARUM–Center for Marine Environmental Sciences, University of Bremen, Germany. This research used samples provided by the International Ocean Discovery Program (IODP). Funding for this research was provided by the UK Natural Environmental Research Council (NERC) to Hodell. The NERC Radiocarbon Facility supported two radiocarbon dates, and Wally Broecker generously supported the remainder with funding from the Comer Family Foundation. Research by Rodriguez-Tovar and Dorador was financed by Project CGL2015-66835-P. B.M. acknowledges support from the CSIC-Ramon y Cajal postdoctoral programme RYC-2013-14073. J.F.E. would like to acknowledge funding under ERC Advanced grant 320750- Nanopaleomagnetism.
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