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兴凯湖沉积物磁化率和色度反映的28 kaBP以来区域古气候环境演化

吴健 沈吉

吴健, 沈吉. 兴凯湖沉积物磁化率和色度反映的28 kaBP以来区域古气候环境演化[J]. 海洋地质与第四纪地质, 2009, 29(3): 123-131. doi: 10.3724/SP.J.1140.2009.03123
引用本文: 吴健, 沈吉. 兴凯湖沉积物磁化率和色度反映的28 kaBP以来区域古气候环境演化[J]. 海洋地质与第四纪地质, 2009, 29(3): 123-131. doi: 10.3724/SP.J.1140.2009.03123
WU Jian, SHEN Ji. PALEOENVIRONMENTAL AND PALEOCLIMATIC CHANGES REFLECTED BY DIFFUSE REFLECTANCE SPECTROSCOPY AND MAGNETIC SUSCEPTIBILITY FROM XINGKAI LAKE SEDIMENTS[J]. Marine Geology & Quaternary Geology, 2009, 29(3): 123-131. doi: 10.3724/SP.J.1140.2009.03123
Citation: WU Jian, SHEN Ji. PALEOENVIRONMENTAL AND PALEOCLIMATIC CHANGES REFLECTED BY DIFFUSE REFLECTANCE SPECTROSCOPY AND MAGNETIC SUSCEPTIBILITY FROM XINGKAI LAKE SEDIMENTS[J]. Marine Geology & Quaternary Geology, 2009, 29(3): 123-131. doi: 10.3724/SP.J.1140.2009.03123

兴凯湖沉积物磁化率和色度反映的28 kaBP以来区域古气候环境演化


doi: 10.3724/SP.J.1140.2009.03123
详细信息
    作者简介:

    吴健(1965-),男,博士生,主要从事湖泊沉积与环境研究,E-mail:jianwu88@126.com

  • 基金项目:

    国家自然科学基金项目(40872117)

  • 中图分类号: P539.3

PALEOENVIRONMENTAL AND PALEOCLIMATIC CHANGES REFLECTED BY DIFFUSE REFLECTANCE SPECTROSCOPY AND MAGNETIC SUSCEPTIBILITY FROM XINGKAI LAKE SEDIMENTS

More Information
  • 摘要: 对兴凯湖长269 cm的沉积岩心的研究结果显示:沉积物的色度和磁化率特征可以较好地反映区域气候环境变化。沉积物明度分别与红度、磁化率、黏土和有机质含量之间及磁化率与黏土之间有很好的相关性;红度高值与明度低值对应暖湿气候环境,磁化率低值反映沉积物较粗的较低湖面,对应冷干气候。28 480~26 160 cal.aBP,湖区处于温湿气候时期;22 880~18 170 cal.aBP,岩心孢粉浓度很低,流域处于末次盛冰期疏桦林草原环境;18 170~12 650 cal.aBP处于Bølling/Older Dryas/Allerød暖期。岩心深度90~78 cm段,对应于新仙女木期;11 500~4 570 cal.aBP,进入全新世暖期,其中8 000~5 000 cal.aBP,本区处于全新世大暖期(气候适宜期);4 570~1 470 cal.aBP气候变为凉干;1 470 cal.aBP以来,流域又变为暖湿气候环境,同时,人类活动逐渐增强造成水土流失加剧。
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  • 收稿日期:  2009-01-13
  • 修回日期:  2009-04-07

兴凯湖沉积物磁化率和色度反映的28 kaBP以来区域古气候环境演化

doi: 10.3724/SP.J.1140.2009.03123
    作者简介:

    吴健(1965-),男,博士生,主要从事湖泊沉积与环境研究,E-mail:jianwu88@126.com

基金项目:

国家自然科学基金项目(40872117)

  • 中图分类号: P539.3

摘要: 对兴凯湖长269 cm的沉积岩心的研究结果显示:沉积物的色度和磁化率特征可以较好地反映区域气候环境变化。沉积物明度分别与红度、磁化率、黏土和有机质含量之间及磁化率与黏土之间有很好的相关性;红度高值与明度低值对应暖湿气候环境,磁化率低值反映沉积物较粗的较低湖面,对应冷干气候。28 480~26 160 cal.aBP,湖区处于温湿气候时期;22 880~18 170 cal.aBP,岩心孢粉浓度很低,流域处于末次盛冰期疏桦林草原环境;18 170~12 650 cal.aBP处于Bølling/Older Dryas/Allerød暖期。岩心深度90~78 cm段,对应于新仙女木期;11 500~4 570 cal.aBP,进入全新世暖期,其中8 000~5 000 cal.aBP,本区处于全新世大暖期(气候适宜期);4 570~1 470 cal.aBP气候变为凉干;1 470 cal.aBP以来,流域又变为暖湿气候环境,同时,人类活动逐渐增强造成水土流失加剧。

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