黄土沉积的局部差异与尘源的关系:Novo Orahovo黄土古土壤序列的关键研究(塞尔维亚伏伊伏丁那)

IF 2.3 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Quaternary Pub Date : 2023-03-16 DOI:10.3390/quat6010023
S. Marković, J. Vandenberghe, Zoran M. Perić, Dávid Filyó, Tamás Bartyik, M. Radaković, Q. Hao, Rastko S. Marković, T. Lukić, N. Tomić, M. Gavrilov, Aleksandar Antić, I. Cvijanovic, G. Sipos
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引用次数: 0

摘要

塞尔维亚北部的Novo Orahovo砖厂保存着晚更新世黄土-古土壤单元的典型模式。所提出的初步发光年表支持了全球同位素海洋气候重建的年代地层解释。磁化率和沉积学证据和海洋氧同位素地层学显示出普遍的相似性。这些记录为巴奇卡黄土高原东侧的灰尘堆积机制提供了新的见解,并为该地区提供了新新的古环境信息。它们代表着从东部巴纳特山麓的薄黄土状沉积物向喀尔巴阡盆地东南部和中部更厚、似乎更完整的黄土段建立连环的重要一步。来自Nova Orahovo黄土记录的粒度数据解释了灰尘沉积的区域差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Local Differentiation in the Loess Deposition as a Function of Dust Source: Key Study Novo Orahovo Loess Paleosol Sequence (Vojvodina, Serbia)
Typical patterns of the Late Pleistocene loess–paleosol units are preserved in the Novo Orahovo brickyard, Northern Serbia. Presented preliminary luminescence chronology supports the chronostratigraphic interpretations of global isotopic marine climate reconstructions. Magnetic susceptibility and sedimentological evidence exhibit general similarities with the marine oxygen-isotope stratigraphy. These records provide new insights into the dust accumulation regimes over the eastern side of the Bačka loess plateau and offer new paleoenvironmental information for the region. They represent an important step forward towards the establishment of a catena from the thin loess-like sediments of the Banat foothills in the east towards the thicker and seemingly more complete loess sections of the southeastern and central Carpathian Basin. Grain-size data from the loess record of Nova Orahovo explain the regional differentiation in dust deposition.
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来源期刊
Quaternary
Quaternary GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.30
自引率
4.30%
发文量
44
审稿时长
11 weeks
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