Yunnan Key Laboratory of Plateau Geographical Processes and Environmental Change, Faculty of Geography, Yunnan Normal University, Kunming, 650500, China.
Chongqing Key Laboratory of Karst Environment, School of Geographical Sciences, Southwest University, Chongqing, 400715, China.
Sci Rep. 2021 Apr 30;11(1):9375. doi: 10.1038/s41598-021-88597-7.
Comprehensive comparison of paleoclimate change based on records constrained by precise chronology and high-resolution is essential to explore the correlation and interaction within earth climate systems. Here, we propose a new stalagmite-based multidecadal resolved Asian summer monsoon (ASM) record spanning the past thirty-seven thousand years (ka BP, before AD 1950) from Furong Cave, southwestern China. This record is consistent with the published Chinese stalagmite sequences and shows that the dominant controls of the ASM dynamics include not only insolation and solar activity but also suborbital-scale hydroclimate events in the high latitudes of the northern hemisphere, such as the Heinrich events, Bølling-Allerød (BA), and Younger Dryas (YD). Benefit from the unprecedented accurate chronology, the timings of these events are precisely dated, with uncertainties of, at most, 40 years (2σ). The onset of the weak ASM during the YD began at 12.92 ka BP and lasted for 430 years. The occurrence of the 200-yr Older Dryas during the BA period was dated from 13.87 to 14.06 ka BP. The durations of the three Heinrich (H) events, H1, H2, and H3, are 14.33-18.29, 23.77-24.48, and 28.98-30.46 ka BP, respectively. Furong record shows surprisingly variable onset transitions of 980, 210, and 40 years for the corresponding weak ASM events. These discrepancies suggest different influences of the H events on ASM dynamics. During the periods of H 1-3, the obvious difference between our Furong record and NGRIP δO record indicated the decoupling correlation between the mid-low latitudes and high latitudes. On the other hand, synchronous climate change in high and low latitudes suggests another possibility which different to the dominant role of Northern high latitudes in triggering global climate change. Our high quality records also indicate a plausible different correlation between the high and mid-low latitudes under glacial and inter-glacial background, especially for the ASM regimes.
为了探究地球气候系统内部的相关性和相互作用,基于精确年代和高分辨率记录对古气候变化进行全面比较至关重要。本研究提出了一个来自中国西南部芙蓉洞的全新、分辨率为多十年的亚洲夏季风(ASM)记录,该记录涵盖了过去 37000 年(公元 1950 年前)的时间。该记录与已发表的中国石笋序列一致,表明 ASM 动力的主要控制因素不仅包括太阳辐射和太阳活动,还包括北半球高纬度的亚轨道尺度气候事件,如 Heinrich 事件、Bølling-Allerød(BA)和 Younger Dryas(YD)。得益于前所未有的精确年代学,这些事件的时间得以精确确定,不确定性最多为 40 年(2σ)。YD 期间弱 ASM 的开始时间为 12.92 ka BP,持续了 430 年。BA 期间 200 年的 Older Dryas 发生时间为 13.87 至 14.06 ka BP。三个 Heinrich(H)事件,H1、H2 和 H3 的持续时间分别为 14.33-18.29、23.77-24.48 和 28.98-30.46 ka BP。芙蓉洞记录显示,对应弱 ASM 事件的起始转变具有令人惊讶的变异性,分别为 980、210 和 40 年。这些差异表明 H 事件对 ASM 动力的影响不同。在 H1-3 期间,我们的芙蓉洞记录与 NGRIP δO 记录之间的明显差异表明中低纬度与高纬度之间的解耦相关性。另一方面,高、低纬度的同步气候变化表明了另一种可能性,即与高纬在触发全球气候变化中的主导作用不同。我们的高质量记录还表明,在冰川和间冰期背景下,高纬和中低纬之间可能存在不同的相关性,特别是对于 ASM 制度。