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末次间冰期第12至11阶段奥赫里德湖(东地中海地区)的古火活动。

Paleofire activity at Lake Ohrid (Eastern Mediterranean region) during MIS 12-11.

作者信息

Koutsodendris Andreas, Kousis Ilias, Pross Jörg

机构信息

Institute of Earth Sciences, Heidelberg University, Im Neuenheimer Feld 234, 69120 Heidelberg, Germany.

出版信息

Data Brief. 2025 Feb 10;59:111384. doi: 10.1016/j.dib.2025.111384. eCollection 2025 Apr.

Abstract

We present microcharcoal data from Lake Ohrid (Eastern Mediterranean region) that span the time period from c. 484 to 367 ka and extend over the extreme glacial-interglacial cycle corresponding to Marine Isotope Stages (MIS) 12-11. The data represent raw counts of microcharcoal particles that were categorized into three sizes, i.e., 10-50 µm, 50-150 µm, and >150 µm. The data have a temporal resolution of c. 450 years and were generated on samples previously used for palynological analysis. Furthermore, we have calculated the concentration of microcharcoal particles per g of dry sediment, which was estimated based on the addition of a known number of marker spores to each sample. Comparisons of the microcharcoal data with pollen-based temperature and precipitation reconstructions from Lake Ohrid yield insight into the paleofire intensity in SE Europe under extreme glacial and extreme interglacial conditions of the Middle Pleistocene. The dataset contributes to a better understanding of the vulnerability of Mediterranean forest ecosystems to naturally triggered fires.

摘要

我们展示了来自奥赫里德湖(东地中海地区)的微木炭数据,其时间跨度约为48.4万年至36.7万年,涵盖了与海洋同位素阶段(MIS)12 - 11相对应的极端冰期 - 间冰期循环。这些数据代表了微木炭颗粒的原始计数,这些颗粒被分为三种大小,即10 - 50微米, 50 - 150微米, 以及大于150微米。数据的时间分辨率约为450年,是在先前用于孢粉学分析的样本上生成的。此外,我们计算了每克干沉积物中微木炭颗粒的浓度,这是通过向每个样本中添加已知数量的标记孢子来估算的。将微木炭数据与基于奥赫里德湖花粉的温度和降水重建进行比较,有助于深入了解中更新世极端冰期和极端间冰期条件下东南欧的古火灾强度。该数据集有助于更好地理解地中海森林生态系统对自然引发火灾的脆弱性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ca79/11875829/caed84c4dfbb/gr1.jpg

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