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Mid-Holocene drought and lake-level change at Elk Lake, Clearwater County, Minnesota: Evidence from CHIRP seismic-reflection data

机译:明尼苏达州克利尔沃特县麋湖中全新世中期干旱和湖面变化:来自CHIRP地震反射数据的证据

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Despite many studies of Holocene paleoclimate records from small lakes in the mid-continent of North America, direct estimates of lake-level changes associated with mid-Holocene aridity are rare. Varved sediments from Elk Lake, Clearwater County, Minnesota, are among the best studied in terms of paleoenvironmental proxies, yet the sedimentary architecture of those sediments has not been previously studied and the hydrological responses of the lake - changes in level and volume - are poorly known. High-resolution seismic-reflection (CHIRP) profiles of Elk Lake reveal complex sedimentary basins in the lake, a pattern of nearshore onlap of sediments onto older substrates, and the focusing of sediments into several deep basins. Biogenic gas obscures sediments in the deepest parts of the basins, but beneath the rest of the lake, a three-part Holocene sequence is clear. The transitions between these parts are correlated with lithological changes defined in earlier core studies. Sediments of the modern stage are less focused than those of the prairie lake stage. A prominent erosional unconformity occurs within the Holocene sequence, separating sediments from the prairie and modern stages of the lake. Erosion associated with this unconformity extends to a depth of 18.2 m below the modern water surface, at which point the unconformity grades into a conformable horizon within the sequence in the deep basins of the lake. This transition is an analog of the onlap of modern sediments onto older substrates, which occurs at a depth of about 8.2 m. The configuration of the erosional unconformity and its modern analog indicates a lake-level fall in the mid Holocene of 10.0 m. At its mid-Holocene minimum, the lake was 39% of its present size and 30% of its present volume, providing quantitative evidence to aid in constraining and evaluating reconstructions of mid-Holocene aridity in the mid-continent of North America.
机译:尽管对北美中部大陆小湖的全新世古气候记录进行了许多研究,但很少有人直接估计与全新世干旱有关的湖面变化。就古环境代理而言,明尼苏达州克利尔沃特县麋鹿湖的曲折沉积物是研究最好的沉积物之一,但这些沉积物的沉积构造尚未得到过研究,该湖的水文响应(水位和体积的变化)较差。众所周知。麋鹿湖的高分辨率地震反射(CHIRP)资料揭示了该湖中复杂的沉积盆地,近岸沉积物向较老基质上的沉积重叠模式以及沉积物集中到几个深层盆地中。生物气体掩盖了盆地最深处的沉积物,但在湖的其余部分之下,则由三部分组成的全新世序列清晰可见。这些部分之间的过渡与早期岩心研究中定义的岩性变化有关。与草原湖阶段相比,现代阶段的沉积物集中度较低。全新世序列内发生了明显的侵蚀不整合,将沉积物从大草原和现代湖泊中分离出来。与这种不整合面相关的侵蚀延伸到现代水面以下18.2 m的深度,此时不整合面被划分为湖泊深水盆地中序列内的合适层位。这种过渡类似于现代沉积物在较旧基底上的重叠,发生在约8.2 m的深度。侵蚀不整合面的构造及其现代模拟表明,全新世中期的湖面塌陷为10.0 m。湖泊处于全新世中期最低时,其面积仅为其当前面积的39%,占其当前体积的30%,提供了定量证据,以帮助限制和评估北美中部大陆上全新世干旱的重建。

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