[1]赵红艳,冷雪天,王升忠.长白山地泥炭分布、沉积速率与全新世气候变化[J].山地学报,2002,(05):513.
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长白山地泥炭分布、沉积速率与全新世气候变化()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2002年05期
页码:
513
栏目:
山地学报
出版日期:
2002-10-28

文章信息/Info

作者:
赵红艳;冷雪天;王升忠
东北师范大学泥炭沼泽研究所;东北师范大学泥炭沼泽研究所;东北师范大学泥炭沼泽研究所 吉林长春130024 ;吉林长春130024 ;吉林长春130024
关键词:
泥炭; 气候变化; 长白山地
文献标志码:
A
摘要:
本文阐述了长白山地泥炭分布规律 ,计算了泥炭厚度累积速率和碳累积速率。早全新世泥炭仅在南部局地沉积 ,速率较小 ,中全新世沉积普遍 ,速率最大 ,晚全新世继续沉积 ,速率较大 ;相应地 ,气候上早全新世开始转暖 ,偏凉 ,中全新世温暖湿润 ,晚全新世偏冷、偏湿。这一结论与孢粉分析、同位素和泥炭地层分析结果一致

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更新日期/Last Update: 2002-10-28