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Reconstruction of Holocene environmental changes in Southern Kurils (North-Western Pacific) based on palaeolake sediment proxies from Shikotan Island

机译:基于实丹岛古湖沉积物代理重建南部千岛(西北太平洋)全新世环境变化

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We investigated a well-dated sediment section of a palaeolake situated in the coastal zone of Shikotan Island (Lesser Kurils) for organic sediment-geochemistry and biotic components (diatoms, chironomids, pollen) in order to provide a reconstruction of the palaeoenvironmental changes and palaeo-events (tsunamis, sea-level fluctuations and landslides) in Holocene. During the ca 8000 years of sedimentation the changes in organic sediment-geochemistry and in composition of the diatoms and chironomids as well as the shifts in composition of terrestrial vegetation suggest that the period until ca 5800 cal yr BP was characterized by a warm and humid climate (corresponds to middle Holocene optimum) with climate cooling thereafter. A warm period reconstructed from ca 900 to at least ca 580 cal yr BP corresponds to a transition to a Nara-Heian-Kamakura warm stage and can be correlated to a Medieval Warm Period. After 580 cal yr PB, the lake gradually dried out and climatic signals could not be obtained from the declining lacustrine biological communities, but the increasing role of spruce and disappearance of the oak from the vegetation give evidences of the climate cooling that can be correlated with the LIA. The marine regression stages at the investigated site are identified for ca 6200-5900 (at the end of the middle Holocene transgression), ca 5500-5100 (Middle Jomon regression or Kemigawa regression), and ca 1070-360 cal yr BP (at the end of Heian transgression). The lithological structure of sediments and the diatom compositions give evidences for the multiple tsunami events of different strengths in the Island. Most remarkable of them can be dated at around ca 7000, 6460, 5750, 4800, 950 cal yr BP. The new results help to understand the Holocene environmental history of the Southern Kurils as a part of the Kuril-Kamchatka and Aleutian Marginal Sea-Island Arc Systems in the North-Western Pacific region.
机译:我们调查了位于Shikotan岛(Lesser Kurils)沿海地区古湖的一个良好的沉积物剖面,以了解有机沉积物-地球化学和生物成分(硅藻,奇虫,花粉),以便重建古环境变化和古环境。全新世的大事件(海啸,海平面涨落和山体滑坡)。在大约8000年的沉积过程中,有机沉积物-地球化学的变化以及硅藻和钟质类的组成以及陆地植被组成的变化表明,直到大约5800 cal BP的时期都是温暖湿润的气候。 (对应于全新世中期最佳),然后进行气候降温。从大约900 cal BP重建到至少大约580 yr BP的暖期对应于向Nara-Heian-Kamakura暖期的过渡,并且可以与中世纪暖期相关。在580年PB浓度之后,湖泊逐渐干dried,无法从湖泊生物群落的下降中获得气候信号,但是橡树云杉和橡树从植被中消失的作用日益增强,这提供了与气候降温有关的证据。 LIA。在研究地点的海洋退回阶段被确定为大约6200-5900(在中新世海侵末期),大约5500-5100(中间乔蒙回归或Kemigawa回归)和大约1070-360 cal yr BP(在平安时代的末日)。沉积物的岩性结构和硅藻组成为该岛内不同强度的多次海啸事件提供了证据。其中最杰出的可以追溯到大约7000、6460、5750、4800和950 cal BP。新的结果有助于了解作为西北太平洋地区的千岛—堪察加半岛和阿留申边缘海岛屿弧系统的一部分的千岛南部全新世环境历史。

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