Tesi Tommaso, Muschitiello Francesco, Mollenhauer Gesine, Miserocchi Stefano, Langone Leonardo, Ceccarelli Chiara, Panieri Giuliana, Chiggiato Jacopo, Nogarotto Alessio, Hefter Jens, Ingrosso Gianmarco, Giglio Federico, Giordano Patrizia, Capotondi Lucilla
Istituto di Scienze Polari, Consiglio Nazionale delle Ricerche ISP-CNR, 40129 Bologna, Italy.
Department of Geography, University of Cambridge, Cambridge CB2 3EN, UK.
Sci Adv. 2021 Nov 26;7(48):eabj2946. doi: 10.1126/sciadv.abj2946. Epub 2021 Nov 24.
The recent expansion of Atlantic waters into the Arctic Ocean represents undisputable evidence of the rapid changes occurring in this region. Understanding the past variability of this “Atlantification” is thus crucial in providing a longer perspective on the modern Arctic changes. Here, we reconstruct the history of Atlantification along the eastern Fram Strait during the past 800 years using precisely dated paleoceanographic records based on organic biomarkers and benthic foraminiferal data. Our results show rapid changes in water mass properties that commenced in the early 20th century—several decades before the documented Atlantification by instrumental records. Comparison with regional records suggests a poleward expansion of subtropical waters since the end of the Little Ice Age in response to a rapid hydrographic reorganization in the North Atlantic. Understanding of this mechanism will require further investigations using climate model simulations.
近期大西洋海水向北冰洋的扩张是该地区正在发生快速变化的无可争议的证据。因此,了解这种“大西洋化”过去的变化情况对于从更长的时间尺度看待现代北极变化至关重要。在此,我们利用基于有机生物标志物和底栖有孔虫数据的精确测年古海洋学记录,重建了过去800年沿弗拉姆海峡东部的大西洋化历史。我们的结果表明,水体性质的快速变化始于20世纪初——比仪器记录记载的大西洋化早了几十年。与区域记录的对比表明,自小冰期结束以来,亚热带水域因北大西洋快速的水文重组而向极地扩张。要理解这一机制,需要利用气候模型模拟进行进一步研究。