非洲东南纳塔尔海谷MIS12期以来的物质来源和古气候变化：IODP U1474孔黏土矿物记录
氧同位素（marine isotope stage，MIS）MIS12期以来的气候环境变化对非洲东南部古人类的迁徙和演化影响甚远。非洲东南外海纳塔尔海谷U1474孔由IODP 361航次获取，通过X射线衍射法（XRD）对前20 m共149个样品中的黏土矿物组成进行测试分析，结果显示自MIS12期以来U1474站位的黏土矿物组成以蒙脱石为主，平均含量为39.23%；其次为伊利石，平均含量为26.11%；高岭石平均含量为17.79%；绿泥石含量最低，平均含量为17.19%；伊利石的结晶度较好，为0.35°Δ2θ（＜0.4°Δ2θ)，而且化学指数较低，为0.30（＜0.43)。其组合特征意味着其主要...
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| Published in | Hăiyang dĭzhĭ yu dĭsĭjĭ dĭzhĭ Vol. 41; no. 4; pp. 142 - 156 |
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| Main Authors | , , , , |
| Format | Journal Article |
| Language | Chinese |
| Published |
Beijing
Marine Geology and Quaternary Geology
01.01.2021
自然资源部海底科学重点实验室,杭州310012 自然资源部第二海洋研究所,杭州310012%成都理工大学沉积地质研究院,成都610059 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0256-1492 |
| DOI | 10.16562/j.cnki.0256-1492.2021042001 |
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| Abstract | 氧同位素（marine isotope stage，MIS）MIS12期以来的气候环境变化对非洲东南部古人类的迁徙和演化影响甚远。非洲东南外海纳塔尔海谷U1474孔由IODP 361航次获取，通过X射线衍射法（XRD）对前20 m共149个样品中的黏土矿物组成进行测试分析，结果显示自MIS12期以来U1474站位的黏土矿物组成以蒙脱石为主，平均含量为39.23%；其次为伊利石，平均含量为26.11%；高岭石平均含量为17.79%；绿泥石含量最低，平均含量为17.19%；伊利石的结晶度较好，为0.35°Δ2θ（＜0.4°Δ2θ)，而且化学指数较低，为0.30（＜0.43)。其组合特征意味着其主要由非洲东南部三大河流携带输入（图盖拉河、林波波河和赞比西河）。U1474孔黏土矿物组成和参数变化自MIS12期以来的变化指示了非洲东南部的气候变化，其变化有着明显的冰期-间冰期旋回特征，可划分为5个阶段，每个阶段冰期寒冷干燥，间冰期相对温暖湿润。在每个时期呈现出一定的亚轨道的气候波动异常，常有冷暖、干湿波动的情形，这可能受到区域大气环流和临近海流（如厄加勒斯流）的影响。 |
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| AbstractList | 氧同位素（marine isotope stage，MIS）MIS12期以来的气候环境变化对非洲东南部古人类的迁徙和演化影响甚远。非洲东南外海纳塔尔海谷U1474孔由IODP 361航次获取，通过X射线衍射法（XRD）对前20 m共149个样品中的黏土矿物组成进行测试分析，结果显示自MIS12期以来U1474站位的黏土矿物组成以蒙脱石为主，平均含量为39.23%；其次为伊利石，平均含量为26.11%；高岭石平均含量为17.79%；绿泥石含量最低，平均含量为17.19%；伊利石的结晶度较好，为0.35°Δ2θ（＜0.4°Δ2θ)，而且化学指数较低，为0.30（＜0.43)。其组合特征意味着其主要由非洲东南部三大河流携带输入（图盖拉河、林波波河和赞比西河）。U1474孔黏土矿物组成和参数变化自MIS12期以来的变化指示了非洲东南部的气候变化，其变化有着明显的冰期-间冰期旋回特征，可划分为5个阶段，每个阶段冰期寒冷干燥，间冰期相对温暖湿润。在每个时期呈现出一定的亚轨道的气候波动异常，常有冷暖、干湿波动的情形，这可能受到区域大气环流和临近海流（如厄加勒斯流）的影响。 P736.21; 氧同位素(marine isotope stage,MIS)MIS12期以来的气候环境变化对非洲东南部古人类的迁徙和演化影响甚远.非洲东南外海纳塔尔海谷U1474孔由IODP 361航次获取,通过X射线衍射法(XRD)对前20 m共149个样品中的黏土矿物组成进行测试分析,结果显示自MIS12期以来U1474站位的黏土矿物组成以蒙脱石为主,平均含量为39.23％;其次为伊利石,平均含量为26.11％;高岭石平均含量为17.79％;绿泥石含量最低,平均含量为17.19％;伊利石的结晶度较好,为0.35°Δ2θ ＜0.4°Δ2θ),而且化学指数较低,为0.30 ＜0.43).其组合特征意味着其主要由非洲东南部三大河流携带输入(图盖拉河、林波波河和赞比西河).U1474孔黏土矿物组成和参数变化自MIS12期以来的变化指示了非洲东南部的气候变化,其变化有着明显的冰期-间冰期旋回特征,可划分为5个阶段,每个阶段冰期寒冷干燥,间冰期相对温暖湿润.在每个时期呈现出一定的亚轨道的气候波动异常,常有冷暖、干湿波动的情形,这可能受到区域大气环流和临近海流(如厄加勒斯流)的影响. |
| Author | HU Bingyao ZHANG Yongcong LONG Feijiang SONG Haonan HAN Xibin |
| AuthorAffiliation | 自然资源部海底科学重点实验室,杭州310012;自然资源部第二海洋研究所,杭州310012%成都理工大学沉积地质研究院,成都610059 |
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| Author_FL | HU Bingyao ZHANG Yongcong LONG Feijiang SONG Haonan HAN Xibin |
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| Copyright | Copyright Marine Geology and Quaternary Geology 2021 Copyright © Wanfang Data Co. Ltd. All Rights Reserved. |
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| DOI | 10.16562/j.cnki.0256-1492.2021042001 |
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| Keywords | 物质来源;古气候;黏土矿物;冰期-间冰期旋回;氧同位素MIS12期;纳塔尔海谷 |
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| Publisher | Marine Geology and Quaternary Geology 自然资源部海底科学重点实验室,杭州310012 自然资源部第二海洋研究所,杭州310012%成都理工大学沉积地质研究院,成都610059 |
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| Snippet | 氧同位素（marine isotope stage，MIS）MIS12期以来的气候环境变化对非洲东南部古人类的迁徙和演化影响甚远。非洲东南外海纳塔尔海谷U1474孔由IODP 361航次获取，通过X射线衍射法（XRD）对前20... P736.21; 氧同位素(marine isotope stage,MIS)MIS12期以来的气候环境变化对非洲东南部古人类的迁徙和演化影响甚远.非洲东南外海纳塔尔海谷U1474孔由IODP 361航次获取,通过X射线衍射法(XRD)对前20... |
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| SubjectTerms | Atmospheric circulation Carbon Chlorite Clay Clay minerals Climate change Environmental changes Expeditions Fluctuations Glacial periods Ice ages Illite Illites Interglacial periods Isotopes Kaolinite Mineral assemblages Mineral composition Mineralogy Minerals Ocean currents Rivers Science Sea level Sediment samplers Sediment samples Smectites Spectrum allocation Spectrum analysis Valleys Vegetation X-ray diffraction |
| Title | 非洲东南纳塔尔海谷MIS12期以来的物质来源和古气候变化：IODP U1474孔黏土矿物记录 |
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