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首页> 外文期刊>The holocene >Late-Holocene climatic record from a glacial lake in Ladakh range, Trans-Himalaya, India
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Late-Holocene climatic record from a glacial lake in Ladakh range, Trans-Himalaya, India

机译:来自拉达克的冰川湖的全新世 - 气候记录,印度跨纪喜马拉雅山脉

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A multi-proxy study using mineral magnetism, sediment texture, total organic content, palynofacies and diatoms was conducted in one of the highest proglacial lake situated at North Pulu (5098 m a.s.l.) of Ladakh sector of NW Himalaya - a high-altitude cold arid desert. This study presents climatic variations that occurred between 5412 and 419 cal. yr BP (C-14 AMS chronology). Directly recharged by meltwater from Khardung glacier, this proglacial lake provides a complete record of past climatic variability due to continuous sedimentation and this attribute makes it an exceptionally important geochronological archive for climatic studies. This first high-resolution palaeolimnology record from Karakoram Himalayas shows intermittent warm and cold periods in which the cold events are short but sudden events recorded at 5700, 4600, 4400, 4200, 3800, 3500, 3000, 1800-1700, 1200, 910, 840 and 770-710 cal. yr BP. Between 5412 and 4840 cal. yr BP, an oxic lake condition existed with freeze-thaw action, prominent weathering, more sediment generation and less organic productivity. The following period till 4410 cal. yr BP was cold and dry, a transition phase to the next warmer phase. Between 4410 and 2064 cal. yr BP, climate ameliorated to somewhat moderate warm climate and relatively high lake levels. Glacial melting due to a warm climate resulted in high TOC%, and well-preserved OM indicating reducing conditions in the lake system. From 2064 to 1711 cal. yr BP cold conditions and from 1272 to 1182 cal. yr BP warmer conditions are seen with large appearance in Amphora ovalis indicating increased nutrients input and moderate water levels. This was followed by warmer climatic conditions between 1182 and 958 cal. yr BP. LIA in the region is experienced between 958 and 644 cal. yr BP with anoxic condition. Between 644 and 419 cal. yr BP, climatic condition was again warmer comparatively. However, this warming was not so severe and only had a regional impact.
机译:使用矿物质磁性,沉积物纹理,总有机含量,帕锡和硅藻的多功能研究是在北普拉·米拉梅拉的Ladakh Sector的最高Puroglacial湖中进行的一种 - 高空冷干旱沙漠。本研究提出了5412和419 Cal之间发生的气候变化。 YR BP(C-14 AMS年代学)。由于连续沉淀,这款Proglacial Lake通过哈达康冰川直接充电,这是由于连续沉淀而完全记录过去气候变异性,并且该属性使其成为气候研究的异影学档案。这首来自Karakoram Himalayas的第一个高分辨率古典主义记录显示间歇性温暖和冷的时期,其中冷事件短但突发的事件记录在5700,4600,4400,4200,3800,3500,3000,1800-1700,1200,910, 840和770-710 Cal。 yr bp。在5412到4840之间。 YR BP,具有冻融作用的氧湖状况,突出的风化,更多的沉积物,有机生产率更少。以下期间到4410 Cal。 YR BP冷且干燥,过渡阶段到下一个较温暖的阶段。在4410到2064年之间。 YR BP,气候改善了一些温和的气候和相对高的湖泊。由于温暖的气候导致冰川熔化导致高TOC%,并且保存完好的OM表明湖泊系统中的减少条件。从2064到1711 cal。 YR BP冷条件和1272至1182 Cal。在Amphora ovalis中看到YR BP加热条件,表明增加营养素输入和中等水平。接下来是1182和958克拉之间的温暖气候条件。 yr bp。该地区的LIA在958和644年之间进行了验证。 YR BP具有缺氧条件。在644到419年之间。 YR BP,气候条件再次加热。然而,这种变暖并不那么严重,只有区域影响。

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