The usefulness of the magnetic susceptibility of loess paleosol sequences for paleoclimate and stratigraphic studies: The case of the Quaternary Palouse loess, northwestern United States

IF 1.9 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL
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Abstract

Worldwide, Quaternary loess-paleosol sequences archive terrestrial paleoenvironmental information. The Palouse loess in the northwestern USA is one such deposit representing at least a million years of sediment accumulation. Loess paleosol sequences are often studied via the magnetic susceptibility of sediments and the changes in susceptibility with depth. However, since variations in magnetic susceptibility can have different underlying causes, the interpretation of the magnetic susceptibility of loess depends on factors specific to each major loess region. We measured the magnetic susceptibility of sediments along depth profiles in a well-studied exposure of the Palouse loess in eastern Washington, USA (the “CLY-2 site,” 46.3131° N, 118.4874° W, WGS84). Our measurements show that the magnetic susceptibility of sediments in the Palouse loess varies systematically and predictably with depth and can be correlated with other magnetic susceptibility profiles at the outcrop scale and at the regional scale. We also measured changes in grain size, elemental abundance, mineralogy, and other magnetic properties to determine the most likely cause of the magnetic susceptibility signal. Based on these results, variations in magnetic susceptibility in the Palouse are likely driven mostly by changes in coarse sediment supply and accumulation of tephra rather than changes in weathering. Magnetic susceptibility is useful as an inexpensive, non-destructive tool for stratigraphic correlation of Quaternary loess deposits in the Palouse, especially in combination with paleosol stratigraphic markers and known tephra deposits.

黄土古沉积序列的磁感应强度对古气候和地层研究的作用:美国西北部第四纪帕卢斯黄土的案例
在全球范围内,第四纪黄土-页岩沉积序列记录了陆地古环境信息。美国西北部的帕劳斯黄土就是这样一种沉积物,代表了至少一百万年的沉积积累。人们通常通过沉积物的磁感应强度以及磁感应强度随深度的变化来研究黄土古沉积序列。然而,由于磁感应强度的变化可能有不同的根本原因,因此对黄土磁感应强度的解释取决于每个主要黄土地区的特定因素。我们在美国华盛顿州东部帕劳斯黄土的一个经过充分研究的出露区("CLY-2 地点",北纬 46.3131°,西经 118.4874°,WGS84)测量了沉积物沿深度剖面的磁感应强度。我们的测量结果表明,帕卢斯黄土中沉积物的磁感应强度随深度的变化是系统的、可预测的,并可与露头尺度和区域尺度上的其他磁感应强度剖面相关联。我们还测量了粒度、元素丰度、矿物学和其他磁性特征的变化,以确定磁感应强度信号最可能的成因。根据这些结果,帕劳斯地区磁感应强度的变化很可能主要是由粗沉积物供应量的变化和凝灰岩的堆积而不是风化作用的变化引起的。磁感应强度是一种廉价、非破坏性的工具,可用于帕劳斯第四纪黄土沉积的地层关联,特别是与古沉积地层标记和已知的凝灰岩沉积相结合时。
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来源期刊
Quaternary International
Quaternary International 地学-地球科学综合
CiteScore
5.60
自引率
4.50%
发文量
336
审稿时长
3 months
期刊介绍: Quaternary International is the official journal of the International Union for Quaternary Research. The objectives are to publish a high quality scientific journal under the auspices of the premier Quaternary association that reflects the interdisciplinary nature of INQUA and records recent advances in Quaternary science that appeal to a wide audience. This series will encompass all the full spectrum of the physical and natural sciences that are commonly employed in solving Quaternary problems. The policy is to publish peer refereed collected research papers from symposia, workshops and meetings sponsored by INQUA. In addition, other organizations may request publication of their collected works pertaining to the Quaternary.
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