长白山区晚更新世以来孢粉-古植被古气候重建及其与植被关系综述
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摘要
长白山区分布的泥炭地与玛珥湖是孢粉的良好载体,适宜开展晚更新世以来孢粉分析重建古植被与古气候研究以对该区未来气候变化进行准确预测。几十年来,该研究经历了从定性描述—半定量重建—定量重建的三个阶段。随着对研究剖面样本采集密度的增加,研究者们也得以观察到更多气候变化事件,尝试提出了气候周期性变化规律,并初步探索了气候变化驱动机制;同时,为了提高定量重建古植被、古气候的准确性,对长白山区也开展了现代孢粉植被关系研究,并取得了一定成果。相信随着对现代孢粉植被关系认识的加深,古植被、古气候重建精度的提高,研究者能够更准确地预测未来气候变化。
The Changbai Mountains,Northeast China provides are suitable location for spore-pollen analysis to reconstruct paleo-vegetation and paleo-climate since the Late Pleistocene and to accurately predict future climate change of this region,where the wide distribution of peat-lands and maar lakes provides good carriers of spore-pollen.Over the past decades,the research has experienced three stages from qualitative description,semi-quantitative reconstruction to quantitative reconstruction.With the increase in the sample collections of the sediment cores,the researchers were able to disclose more climate events,the periodical climate patterns,and the mechanism of climate change.Meanwhile,in order to improve the accuracy of quantitative reconstruction on paleo-vegetation and paleo-climate,in The Changbai Mountains carried out research was also on the relationship between modern spore-pollen and vegetation.With the progress of the understanding of the relationship between modern spore-pollen and vegetation,researchers can not only make more accurate reconstructions of paleo-vegetaion and paleo-climate,but also propose better predictions of future climate change.
The Changbai Mountains,Northeast China provides are suitable location for spore-pollen analysis to reconstruct paleo-vegetation and paleo-climate since the Late Pleistocene and to accurately predict future climate change of this region,where the wide distribution of peat-lands and maar lakes provides good carriers of spore-pollen.Over the past decades,the research has experienced three stages from qualitative description,semi-quantitative reconstruction to quantitative reconstruction.With the increase in the sample collections of the sediment cores,the researchers were able to disclose more climate events,the periodical climate patterns,and the mechanism of climate change.Meanwhile,in order to improve the accuracy of quantitative reconstruction on paleo-vegetation and paleo-climate,in The Changbai Mountains carried out research was also on the relationship between modern spore-pollen and vegetation.With the progress of the understanding of the relationship between modern spore-pollen and vegetation,researchers can not only make more accurate reconstructions of paleo-vegetaion and paleo-climate,but also propose better predictions of future climate change.
引文
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李永化,尹怀宁,张小咏等,2003.东北地区5 000ab.p.-4 700ab.p.左右的降温事件及对考古文化的影响.云南地理环境研究,15(1):12-18
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李建勇,许清海,曹现勇等,2011.长白山针阔叶混交林花粉通量及垂直散布特征年际变化研究.第四纪研究,31(1):171-179
李永飞,李春海,介冬梅等,2016.长白山北坡表土花粉组合及数量分析.微体古生物学报,33(3):293-303
杨永兴,王世岩,2002.小兴安岭东部9.0ka b.p.以来沼泽发育与古环境演变研究.山地学报,20(2):129-134
杨永兴,王世岩,2003.8.0ka b.p.以来三江平原北部沼泽发育和古环境演变研究.地理科学,23(1):32-38
张丽艳,许清海,李月丛等,2009.长白山针阔叶混交林带花粉通量及垂直散布年际对比.古生物学报,48(2):222-227
周昆叔,陈硕民,叶永英等,1977.吉林省敦化地区沼泽的调查及其花粉分析.地质科学,12(2):129-139
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夏玉梅,2000.大小兴安岭泥炭的孢粉记录及演变过程研究.微体古生物学报,17(2):218-227
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