|国家科技期刊平台
首页|期刊导航|生态学报|孢粉记录的晚全新世以来大兴安岭北部多年冻土泥炭地演化及其影响因素

孢粉记录的晚全新世以来大兴安岭北部多年冻土泥炭地演化及其影响因素OA北大核心CHSSCDCSTPCD

Evolution of permafrost peatland and its influencing factors in the northern Greater Khingan Mountains recorded by palynology since the Late Holocene

中文摘要英文摘要

当前泥炭所揭示的区域古植被、古气候与环境变化相关工作已广泛开展,然而对于泥炭地本身演化的研究却很少涉及,尤其是对于大兴安岭北部多年冻土泥炭地演化及其影响因素仍不清晰,阻碍了人们对这一特殊类型泥炭地历史动态和未来发展趋势的认知.为此基于大兴安岭北部多年冻土泥炭岩芯孢粉证据,利用AMS14C测年技术,重建了区域3500 cal a BP以来植被与气候历史,并与其他古气候指标进行对比,从而揭示区域泥炭地演化及其影响因素.结果表明:3500-2900 cal a BP植被以松属、喜暖乔木及水龙骨科为主,气候温暖湿润成为泥炭孕育期;2900-2250 cal a BP植被以松属、喜暖乔木及蒿属为主,气候温暖潮湿成为泥炭发育启动期;2250-1650 cal a BP植被以松属、桦属及水龙骨科为主,气候寒冷湿润成为泥炭发育旺盛期;1650-1150 cal a BP植被以松属和蒿属为主,气候寒冷干燥成为泥炭发育减缓和停滞期;1150-750 cal a BP阔叶林和湿地植被扩张,气候温暖湿润成为泥炭发育再次启动期,完成由富营养沼泽到中营养沼泽类型的转变;750 cal a BP至今植被以松属、桤木属及莎草科为主,气候寒冷湿润成为泥炭发育再次旺盛期,中营养沼泽开始向贫营养沼泽类型过渡.造成多年冻土泥炭地演化的主导因素并不是地质地貌变动和人类活动,而是来自气候变化及其驱动下多年冻土环境的改变,因此气候变化才是影响多年冻土泥炭地演化的主动力,未来多年冻土泥炭地变化取决于全球气候的发展.

At present,extensive research has already been conducted on regional ancient vegetation,paleoclimate and environmental changes revealed by peat.However,evolution of peatland itself is rarely involved,and especially the evolution process of permafrost peatland and its influencing factors are still unclear in the northern Greater Khingan Mountains(GKM),which hinders our understanding of the historical dynamics and future development trends of this special type of peatland.To address this,based on palynology evidence from permafrost peat cores in the northern GKM and using AMS14 C dating technique,the vegetation and climate history of the region since 3500 cal a BP have been reconstructed.This history was then compared with other paleoclimate indicators to reveal the evolutionary process of the regional peatland and its influencing factors.The results indicated that:From 3500-2900 cal a BP,the vegetation mainly consisted of Pinus,thermophilic broad-leaved forest,and Polypodiaceae,warm and wet climate was the peat incubation period.From 2900-2250 cal a BP,the vegetation mainly consisted of Pinus,thermophilic broad-leaved forest,and Artemisia,warmer and humid climates led to an initiation of peat developmental initiation period.From 2250-1650 cal a BP,the vegetation mainly consisted of Pinus,Betula and polypodiaceae,cold and wet climates led to an initiation of peat prosperity period.From 1650-1150 cal a BP,the vegetation mainly consisted of Pinus,and Artemisia,cold and dry climate led to a slowdown or stagnation of peat development period.From 1150-750 cal a BP,broad-leaved forests and wetland vegetation expansion,warm and wet climate caused peat to development period again,completed the transition from low swamp to medium swamp.Since 750 cal a BP,the vegetation mainly consisted of Pinus,Alnus and Cyperaceae,cold and wet climate as a period of peat prosperity period again,medium swamp began to transit to high swamp.The analysis reveals that the dominant factors causing the evolution of permafrost peatland are not geological landform and human activities,but rather the changes in the permafrost environment driven by climate change.Therefore,climate change is the primary force determining the evolution of permafrost peatland,and future changes in these peatlands will depend on the development of the global climate.

刘锐;赵林;谢远云;刘立新;吴少强;臧淑英

哈尔滨师范大学寒区地理环境监测与空间信息服务黑龙江省重点实验室,哈尔滨 150025南京信息工程大学地理科学学院,南京 210044

大兴安岭孢粉晚全新世多年冻土泥炭地演化气候与环境变化

Greater Khingan MountainspollenLate Holocenepermafrostpeatland evolutionclimate and environmental changes

《生态学报》 2024 (018)

7991-8002 / 12

科技基础资源调查专项(2022FY100701);国家自然科学基金联合基金重点项目(U20A2082);国家自然科学基金(41971151);哈尔滨师范大学博士研究生创新基金(HSDBSCX2022-07)

10.20103/j.stxb.202401280255

评论