Lithology of the long sediment record recovered by the ICDP Dead Sea Deep Drilling Project (DSDDP)
Lithology of the long sediment record recovered by the ICDP Dead Sea Deep Drilling Project (DSDDP)
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ICDP 死海深钻项目 (DSDDP) 恢复的长沉积物记录的岩性
DOI：
10.1016/j.quascirev.2014.08.013
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发表时间：
2014
影响因子：
4
通讯作者：
Goldstein
中科院分区：
文献类型：
--
作者：
Neugebauer;Brauer;Schwab;Waldmann;Kitagawa;Torfstein;Dulski;Ariztegui;Ben-Avraham;Goldstein
从全新世死海及其更新世前体沉积的沉积剖面是黎凡特地区气候，环境和地震历史的优秀档案。然而，以前的大部分工作都是在现今死海边缘暴露的湖相沉积物序列上进行的，这些沉积物只有在湖面水位上升到这些阶地以上时才沉积（例如在末次冰期），并且由于过去的主要湖面变化而通常是不连续的。只有在盆地的最深处才可能出现连续的沉积，因此，在ICDP计划框架内，在2010-2011年冬季，在死海深海钻探项目（DSDDP）范围内，在死海北方盆地完成了一次深海钻探。已从两个深钻孔和几个短钻孔中获得约720米的沉积物岩心。最长的剖面（5017-1）显示在水深300 m处，达到湖底以下455 m（blf，即全球平均海平面以下1175 m），大约包括最近220-240 ka。该记录涵盖了阿莫拉（倒数第二次冰期）的上部、末次间冰期的萨姆拉、末次冰期的利桑和全新世的泽埃利姆组，以及两个完整的冰期-间冰期旋回。因此，首次从死海盆地中回收了MIS 6/5、5/4和2/1过渡期间沉积的连续沉积物，这些沉积物在当今湖岸露头的沉积物中没有代表。本文提供了深盆长剖面（5017-1）的基本岩性资料（包括连续磁化率和地球化学扫描资料）和基本地层学资料（包括第一年代学资料）。这里提出的结果（a）集中在深盆地沉积物与主要的岸上地层单位的相关性，从而提供了一个独特的综合地层框架，区域古环境重建，（B）突出死海深层沉积档案记录水文变化的突出潜力，在间冰期，冰期和过渡期。
The sedimentary sections that were deposited from the Holocene Dead Sea and its Pleistocene precursors are excellent archives of the climatic, environmental and seismic history of the Levant region. Yet, most of the previous work has been carried out on sequences of lacustrine sediments exposed at the margins of the present-day Dead Sea, which were deposited only when the lake surface level rose above these terraces (e.g. during the Last Glacial period) and typically are discontinuous due to major lake level variations in the past. Continuous sedimentation can only be expected in the deepest part of the basin and, therefore, a deep drilling has been accomplished in the northern basin of the Dead Sea during winter of 2010–2011 within the Dead Sea Deep Drilling Project (DSDDP) in the framework of the ICDP program. Approximately 720 m of sediment cores have been retrieved from two deep and several short boreholes. The longest profile (5017-1), revealed at a water depth of ∼300 m, reaches 455 m below the lake floor (blf, i.e. to ∼1175 m below global mean sea level) and comprises approximately the last 220–240 ka. The record covers the upper part of the Amora (penultimate glacial), the Last Interglacial Samra, the Last Glacial Lisan and the Holocene Ze'elim Formations and, therewith, two entire glacial–interglacial cycles. Thereby, for the first time, consecutive sediments deposited during the MIS 6/5, 5/4 and 2/1 transitions were recovered from the Dead Sea basin, which are not represented in sediments outcropping on the present-day lake shores. In this paper, we present essential lithological data including continuous magnetic susceptibility and geochemical scanning data and the basic stratigraphy including first chronological data of the long profile (5017-1) from the deep basin. The results presented here (a) focus on the correlation of the deep basin deposits with main on-shore stratigraphic units, thus providing a unique comprehensive stratigraphic framework for regional paleoenvironmental reconstruction, and (b) highlight the outstanding potential of the Dead Sea deep sedimentary archive to record hydrological changes during interglacial, glacial and transitional intervals.
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死海盆地最后一个间冰期萨姆拉湖的地层学、沉积环境和水平重建
影响因子：
2.3
作者：
N. Waldmann;M. Stein;D. Arizteguí;A. Starinsky
通讯作者：
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DOI：
--
发表时间：
2000
期刊：
Radiocarbon: An International Journal of Cosmogenic Isotope Research
影响因子：
--
作者：
M. Stein;S. Goldstein;Alexandra Schramm
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Alexandra Schramm
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DOI：
--
发表时间：
2009
期刊：
影响因子：
--
作者：
Sushma Prasad;J. Negendank;M. Stein
通讯作者：
M. Stein
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DOI：
--
发表时间：
2009
期刊：
影响因子：
--
作者：
S. A. Ghazleh;S. Kempe
通讯作者：
S. Kempe
影响因子：
4
作者：
Fronval, T;Jansen, E;Sejrup, HP
通讯作者：
Sejrup, HP