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| 趋磁细菌及磁小体对黄土-古土壤序列磁化率贡献的模拟实验研究 | |
| 引用本文： | 彭先芝,贾蓉芬,李荣森,戴顺英,刘东生.趋磁细菌及磁小体对黄土-古土壤序列磁化率贡献的模拟实验研究[J].第四纪研究,2002,22(2):188-194. |
| 作者姓名： | 彭先芝 贾蓉芬 李荣森 戴顺英 刘东生 |
| 作者单位： | [1]中国科学院广州地球化学研究所，有机地球化学国家重点实验室，广州510640 [2]中国科学院武汉病毒所，武汉430071 |
| 基金项目： | 国家自然科学基金项目 (批准号 :4 96 72 1 36 )，中国科学院西安黄土与第四纪实验室 (批准号 :LLQG970 1 ) |
| 摘 要： | 选择西峰和段家坡两个黄土剖面,对磁化率变化显著的L6-S5-L5层段,通过对样品中的趋磁细菌(MB)用相同的培养基富集及生长培养,初步定量模拟了MB和磁小体(MSs)对黄土-古土壤序列磁化率的贡献。富集培养MB后,段家坡剖面样品磁化率表现出不同程度的增高,最大达116.4%(DS5-1)。以古土壤样品XS5-1、DS5-1为介质生长培养MB,DS5-1磁化率的增长与接种的菌液量呈近似线性关系。此外,生长培养后古土壤样品频率磁化率与FeO/Fe2O3比值呈现出相似的变化趋势,证实了磁小体的形成。由此表明:1)MB和MSs是影响黄土剖面磁化率的因素之一,受气候和地质环境等因素的影响,不同地区黄土剖面MB的生长和MSs的形成存在差异,因此对磁化率的贡献也不尽相同;2)MSs是黄土-古土壤序列中超细粒磁性物质的组成部分。当气候环境比较适宜MSs形成及保存时,MSs在黄土剖面中超细粒(≤50nm)磁性组分中比重会相应增高,对磁化率和频率磁化率的影响也更为突出。 |
| 关 键 词： | 趋磁细菌 磁小体 黄土-古土壤序列 磁化率 模拟实验 |
| 收稿时间： | 2000-01-20 |
| 修稿时间： | 2000年1月20日 |
SIMULATION EXPERIMENTS OF MB AND MSS CONTRIBUTIONS TO THE MAGNETIC SUSCEPTIBILITY OF CHINESE LOESS-PALEOSOL SEQUENCES |
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| Institution: | 1. State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640| 2. Wuhan Institute of virus, Chinese Academy of Sciences, Wuhan 430071; 3. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029 |
| Abstract: | samples were collected from the L 6 S 5 L 5 layers at Xifeng and Duanjiapo sections on the Chinese Loess Plateau. Based on the enrichment and growth culture of the magnetotactic bacteria (MB), contribution of MB and magnetosomes (MSs) to the susceptibility of the Chinese loess-paleosol sequences was simulated. Susceptibility of most samples became enhanced after MB enrichment by the same culture, with the maximum of 116.4% (DS 5-1 ). Linear relationship is shown between the susceptibility of DS 5-1 and the volume of inoculating MB after 10 days of MB culture. In addition, the frequency dependent susceptibility of samples changes resembles the variations of FeO/Fe 2O 3 after MB culture. The above results suggest that: 1) MB and MSs are among the factors affecting the susceptibility of Chinese loess. However, due to the spatial difference in climate and other conditions, MB growth and MSs formation in Chinese loess in different sites are not the same, and therefore the contribution of MB and MSs to susceptibility is also somewhat different; 2) MSs is one of components of superfine magnetic material in loess-paleosol sequences. If the climate is suitable for MSs formation and preservation, the contribution of MSs to the frequency dependent susceptibility is more important. |
| Keywords: | magnetotactic bacteria magnetosomes simulating experiments susceptibility loess-paleosol sequences |
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