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晚中新世-上新世黄土高原佳县红粘土剖面碳同位素记录与C4植被演化

, PP. 791-800

Keywords: 红粘土,无机碳同位素,C4植被扩张,区域干旱化,降雨季节性加强

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Abstract:

新生代C4植被开始扩张的年代、过程和驱动机制是全球古气候变化研究的焦点问题。中国黄土高原的黄土-红粘土剖面保存了连续的古生态演化记录,是研究这一关键科学问题的理想载体。本文选择黄土高原北部佳县厚达64m的红粘土剖面(8.2~2.7Ma),对190个层位的次生方解石矿物进行了无机碳同位素测试,由此分析了晚中新世-上新世末的C4植被扩张和演化过程。C4植被持续增长与全球冰盖的扩张基本一致,表明气候变冷很可能导致了黄土高原区域气候的干旱化与降雨季节性的增强。C4植被的扩张存在明显的3个阶段,分别以6.6Ma和3.6Ma为界限,每一次扩张增加10%左右,暗示了全球性的构造事件对黄土高原植被演化的控制。此外,佳县红粘土剖面呈现10次持续时间为10~20万年的碳同位素正漂移事件,平均每40万年发生一次,说明40万年轨道周期也控制着C4植被的演化。

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