globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:5354190
论文题名:
东北哈尼泥炭腐殖化度记录的全新世气候变化
其他题名: Holocene Climate Changes Recorded by Peat Humification from Hani Peat Bog in Northeast China
作者: 肖河; 黄庭; 程胜高; 胡忠霞; 刘晓彤; 周莹
刊名: 地质科技情报
ISSN: 1000-7849
出版年: 2015
卷: 34, 期:1, 页码:67-71
语种: 中文
中文关键词: 哈尼泥炭地 ; 泥炭腐殖化度 ; 全新世 ; 气候变化
英文关键词: Hani peat bog ; peat humification ; Holocene ; climate change
WOS学科分类: GEOLOGY
WOS研究方向: Geology
中文摘要: 泥炭作为一种环境信息载体,在全球变化的研究中具有重要的作用。东北地区的哈尼泥炭地位于全球气候变化的敏感区域,研究意义更加显著。运用碱提取溶液吸光度法对东北哈尼泥炭腐殖化度进行了测定,结合~(14)C测年数据,与泥炭纤维素delta~(18)O时间序列相比较,较好地恢复了全新世哈尼地区的古气候状况,指出了哈尼地区的全新世气候演变的5个阶段:111.5~9.8kaBP气候温暖阶段;29.8~9.0kaBP气候急剧降温寒冷阶段;39.0~4.8kaBP气候温暖阶段;44.8~1.8kaBP气候冷暖交替波动阶段;51.8~0kaBP气候寒冷阶段。
英文摘要: As one of the environmental information records,peat plays an important role in global climate change research.Hani peat bog in northeastern China is located in sensitive ranges of global climate change,so it is more remarkable for studying.In this study,used alkali extraction method to measure the humification of Hani peat,combined with C~(14) dating data and compared it withdelta~(18) O time series of Hani peat cellulose,the Holocene climate changes of Hani area were rebuilt well.And the Holocence climate changes were divided into five stages:(1)11.5-9.8 kaBP with warm climate;(2)9.8-9.0 kaBP with the climate of sharply cooling and cold;(3)9.0-4.8 kaBP with cold and warm climate;(4)4.8-1.8 kaBP with the climate of fluctuations between cold and warm;(5)1.8-0 kaBP with cold climate.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/156939
Appears in Collections:气候变化事实与影响

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作者单位: (武汉)中国地质大学环境学院, 武汉, 湖北 430074, 中国

Recommended Citation:
肖河,黄庭,程胜高,等. 东北哈尼泥炭腐殖化度记录的全新世气候变化[J]. 地质科技情报,2015-01-01,34(1):67-71
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