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Subdecadal-scale vegetation responses to a previously unknown late-Allerød climate fluctuation and Younger Dryas cooling at Lake Meerfelder Maar (Germany)

机译:Meerfelder Maar湖(德国)对以前未知的晚期Allerød气候波动和年轻的Dryas降温的年代际尺度植被响应

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摘要

Lake Meerfelder Maar (MFM) is the northernmost Western European sediment record with annual laminations across the Younger Dryas (YD), and the onset of the YD in the record of MFM has previously been defined as an increase in non-arboreal pollen abundance at ca. 12 680 varve a BP. Here we present a palynological record at unprecedented subdecadal resolution for MFM, covering the Allerød–YD transition. Our results show a fluctuation in pollen accumulation rates (PARs) before the onset of the YD, with lower rates between ca. 12 725 and 12 685 varve a BP. The fluctuation in PARs occurs simultaneous with a previously undescribed short fluctuation in sediment composition and varve thickness, as well as with changes in biogeochemical proxies. The combined evidence indicates signs of climatic instability ca. 45 years before the onset of the YD. The PAR records of Betula and Pinus furthermore show earlier and more abrupt changes at the onset of the YD than the percentage-records do. Finally, heliophilous herbaceous taxa show a delayed increase following the onset of the YD of ca. 145 years. This paper illustrates the potential to identify previously unrecognized climate variability and vegetation change when using subdecadal-resolution analyses.
机译:Meerfelder Maar湖(MFM)是西欧最北端的沉积物记录,在Younger Dryas(YD)上有年叠层,并且MFM记录中YD的出现以前被定义为在约200摄氏度时非树状花粉的丰度增加。 。 12 680 BP。在这里,我们以MFM前所未有的年代际分辨率呈现了古生物学记录,涵盖了Allerød-YD过渡。我们的结果表明,YD发病前花粉积累率(PARs)出现波动,而在约3到6年之间较低。 12 725和12 685使BP脉动。 PAR的波动与先前未描述的沉积物成分和瓣膜厚度的短暂波动以及生物地球化学代理的变化同时发生。综合证据表明气候不稳定的迹象。 YD发病前45年。与百分率记录相比,桦树和松树的PAR记录在YD发病时显示出更早,更突然的变化。最后,嗜盐的草本类群显示出随着ca的YD的开始而延迟的增加。 145年。本文说明了使用年代际分辨率分析来识别以前无法识别的气候变化和植被变化的潜力。

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