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- W3147543537 abstract "尽管更新世红 paleosols 在华南是广泛地分布式的，因为强烈捱过， paleoenvironmental 解释证明了困难。这里，我们从分子的石块和磁性联合数据重建在为在东南中国的红 paleosols 的 pedogenic 紧张的变化的一个记录。磁性的深度分发模式显示那降低(更高)但是更高(更低) HIRM (努力等温的残余的磁化)和 SIRM 的价值(浸透等温的残余的磁化)/与成土作用的紧张有紧密的关系，特别开发得好的网状的静脉的出现，它为以有细密纹理的 SP ( superparamagnetic ) /SD (单个领域)的成本的反铁磁性的矿物质的存在绝对负责 ferrimagnetic 矿物质。n 链烷， n-alkanols，和 n-alkanoic 酸的碳分发模式在成土作用期间反映微生物的占优势的贡献到有机物，它响应极其热潮湿的条件为强壮的微生物引起的活动提供直接证据当时白粗糙的网状的静脉出现。我们的结果证明提高的东亚夏天季风的存在在氧化物主导的捱过政体，和成土作用起了一个关键作用，并且微生物引起的活动。在分子的比率和磁性的变化被用来证明红 paleosols 在对东亚夏天季风的进化的惹人注目的反应经历了土壤形成的三个阶段：(1 ) 自从中间的更新世最有效；(2 ) 自从 270 ka 左右中等有效；(3 ) 自从最后最不有效冰川。我们的研究提供重要证据理解怎么红 paleosols espond 到全球变化自从中间的更新世。" @default.
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- W3147543537 date "2013-01-01" @default.
- W3147543537 modified "2023-10-18" @default.
- W3147543537 title "Red Palaeosols Development in Response to the Enhanced East Asia Summer Monsoon since the Mid-Pleistocene in South China： Evidence Derived from Magnetic Properties and Molecular Fossil Records" @default.
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