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Distinct lake level lowstand in Lake Prespa (SE Europe) at the time of the 74 (75) ka Toba eruption

机译:74(75)ka Toba喷发时普雷斯帕湖(欧洲东南部)明显的湖面低水位

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The 74 (75) ka Toba eruption in Sumatra, Indonesia, is considered to be oneof the largest volcanic events during the Quaternary. Tephra from the Tobaeruption has been found in many terrestrial and marine sedimentary deposits,and acidity peaks related to the eruption have been used to synchronize icecore records from Greenland and Antarctica. Seismic profiles andsedimentological data from Lake Prespa on the Balkan Peninsula, SE Europe,indicate a lake level lowstand at 73.6 ± 7.7 ka based on ESR dating ofshells. Tephrostratigraphy, radiocarbon dating and tuning of the totalorganic carbon content with the NGRIP isotope record, corroborate that the lake levellowstand was a short-term event superimposed on the general cooling trend atthe end of MIS 5, most likely at the onset of the Greenland Stadial GS-20.Acknowledging that tectonic events or karst processes could have triggeredthis lake level lowstand, the chronological correspondence between thelowstand and the Toba eruption is intriguing. Therefore a Toba-drivenshort-term shift to aridity in the Balkan region, leading to lake levelchanges and triggering spatial expansion events in one of the lake's mostabundant benthic species, the carino mussel Dreissena presbensis,cannot be excluded.
机译:印度尼西亚苏门答腊岛74(75)ka Toba火山喷发被认为是第四纪期间最大的火山事件之一。在许多陆地和海洋沉积物中都发现了来自Tobaeruption的Tephra,并且已经使用了与喷发有关的酸度峰值来同步格陵兰岛和南极洲的冰芯记录。来自欧洲东南部巴尔干半岛普雷斯帕湖的地震剖面和沉积学数据表明,根据壳的ESR测年,湖面低水位为73.6±7.7 ka。岩相地层学,放射性碳测年和利用NGRIP同位素记录对总有机碳含量进行调整,证实了湖水位低位是短期事件,与MIS 5末期的总体降温趋势相叠加,很可能是在格陵兰Stadial GS爆发时发生的。 -20。认识到构造事件或岩溶过程可能触发了该湖水位低水位,低水位与多巴喷发之间的时间对应关系令人着迷。因此,不能排除由多巴驱动的巴尔干地区短期干旱转变,导致湖泊水位变化并触发湖泊中最丰富的底栖物种之一,食肉贻贝 Dreissena presbensis

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