塞尔维亚泰特尔黄土高原 ~350 ka 到 250 ka 之间的冰川-间冰期 Malacofauna 记录

IF 2.3 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Quaternary Pub Date : 2024-06-14 DOI:10.3390/quat7020028
M. Radaković, Bojan Gavrilović, M. Gavrilov, Rastko S. Marković, Qingzhen Hao, Randall Schaetzl, C. Zeeden, Binggui Cai, Zoran M. Perić, Aleksandar Antić, T. Lukić, Slobodan B. Marković
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引用次数: 0

摘要

我们展示了塞尔维亚 Veliki Surduk 关键黄土剖面 L3 黄土单元(以及部分 S3 古沉积)内的软体动物群数据。该剖面与海洋同位素阶段(MIS)8 和 MIS 9 晚期相关,因此时间跨度为约 350 至 250 ka。Veliki Surduk 黄土-古溶岩序列(LPS)位于 Titel 黄土高原西北边缘,由约 30 米的沉积物组成。我们的研究重点是 5.4 米厚的沉积区间,每 20 厘米取样一次,每次取样约 2 千米。在黄土序列中发现了九种软体动物:Granaria frumentum、Helicopsis striata、Pupilla trilicata、Chondrula tridens、Pupilla muscorum、Succinella oblonga、Punctum pygmaeum、Vallonia costata 和 Vitrina pellucida,以及一些未确定的蛞蝓类群(Limacidae、Agriolimacidae 和 Milacidae)。大部分蜗牛群出现在 MIS 9 与 MIS 8 之间的过渡时期,这表明当时的气候大多比较干燥,栖息地类似于开阔的大草原。在古壤土 S3 层上部 L3 单元以下发现的动物群表明该地区气候干旱。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Glacial–Interglacial Malacofauna Record from the Titel Loess Plateau, Serbia, between ~350 and 250 ka
We present data on molluscan fauna within the L3 loess unit (and partially within the S3 paleosol) from the key loess section of Veliki Surduk in Serbia. The section correlates to Marine Isotope Stage (MIS) 8 and late MIS 9 and, thus, spans the time frame from ~350 to 250 ka. The Veliki Surduk loess–paleosol sequence (LPS) is located on the northwestern margin of the Titel loess plateau and comprises ~30 m of sediments. Our focus is on a 5.4 m thick sedimentary interval, which was sampled at 20 cm increments, each sample covering approximately 2 ky. Nine mollusk species were identified in the loess sequence: Granaria frumentum, Helicopsis striata, Pupilla triplicata, Chondrula tridens, Pupilla muscorum, Succinella oblonga, Punctum pygmaeum, Vallonia costata, and Vitrina pellucida, as well as a few unidentified slug taxa (Limacidae, Agriolimacidae, and Milacidae). The majority of the snail assemblage occurs at the transition between MIS 9 and MIS 8, suggesting a mostly dry climate and an open and steppe-like habitat. The fauna identified in the upper part of the paleosol layer S3, below the L3 unit, indicated aridification.
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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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