| 福建屏南天湖山泥炭腐殖化度记录的早全新世以来气候变化 |
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| 引用本文： | 胡凡根,李志忠,姜修洋,靳建辉,张辉,赵倩,马鹏.福建屏南天湖山泥炭腐殖化度记录的早全新世以来气候变化[J].亚热带资源与环境学报,2011,6(3):31-39. |
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| 作者姓名： | 胡凡根 李志忠 姜修洋 靳建辉 张辉 赵倩 马鹏 |
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| 作者单位： | 福建师范大学地理科学学院,福州,350007 |
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| 基金项目： | 福建省公益类科研院所专项基金 |
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| 摘 要： | 以14C测年为基础，构建了天湖山泥炭剖面的年代序列，通过对研究区泥炭腐殖化度与有机质的分析研究，发现两者呈现出很好的相关性，共同记录了研究区约9．5kaBP以来的气候变化，可划分出3个主要阶段：1）早期（9．5 ka BP-6．3 ka BP）泥炭腐殖化度最低，指示气候湿热，其中7．9ka BP-6．3kaBP为整个剖...
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| 关 键 词： | 泥炭 腐殖化度 全新世 古气候 福建天湖山 |
Holocene Climate Change Recorded in Peat Humification on Tianhu Mountain in Northern Fujian Province |
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| Abstract: | The age series of a peat profile at Tianhu Mountain in northern Fujian province was construtted on the basis of radiocarbon date. The geography location of the profile in the southern subtropic is sensitive to global climate changes. The age series shows that the peat profile formed mainly since 9. 5ka BP. According to the analysis of the peat humification and organic content of the profile, we find that both of the proxies show well correlation and make a clear identification of climatic shifts in Holocene. Holocene climate changes can be divided into three phases in the region ： 1 ） lower humification phase （9.5 ka BP-6. 3 ka BP） with the lowest during 7.9 ka BP-6.3 ka BP, which suggests hot and moist climate, and may be corresponding to the Holocene optimum of the studied area ; 2） low humification phase （6.3 ka BP -2. 8 ka BP）, indicating a warm and moist climate state; 3） the latest phase （since 2. 8 ka BP） of high humification with large fluctuation, reflecting a dry and cool climate condition. In addition, using red noise spectrum analysis with the redfit 3.8 organic record show some aquasi-periods of 948 a, 268 a, 342 a consistent with solar activity cycles, which suggested that summer monsoon climate change was probably sensitive to the secular solar activity. |
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| Keywords: | peat humification Holocene paleaoclimate Tianhu Mountain in Fujian province |
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