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三江平原宝清地区晚更新世晚期以来孢粉组合及古气候

赵建 孔繁鹏 张苍江 张也 刘洪博 邵吉亮 张磊 董凯

地质与资源2026,Vol.35Issue(2):133-140,8.
地质与资源2026,Vol.35Issue(2):133-140,8.DOI:10.13686/j.cnki.dzyzy.2026.02.001

三江平原宝清地区晚更新世晚期以来孢粉组合及古气候

Spore-pollen assemblages and paleoclimate in Baoqing area of Sanjiang Plain since the late Late Pleistocene

赵建 1孔繁鹏 1张苍江 1张也 1刘洪博 1邵吉亮 1张磊 1董凯1

作者信息

  • 1. 中国地质调查局牡丹江自然资源综合调查中心,黑龙江牡丹江 157000||呼伦贝尔黑土地地球关键带野外科学观测研究站,内蒙古呼伦贝尔 021599
  • 折叠

摘要

Abstract

Based on the study of spore-pollen assemblages from PM03 profile in Longquan village of Longtou Town,Baoqing area,supported by chronological dating data,four pollen zones have been identified since the late Late Pleistocene.Pollen Zone Ⅰ(63.35-45.51 ka)is characterized by a savanna landscape,indicating a cool and dry climate.Pollen Zone Ⅱ(45.51-37.28 ka)consists of coniferous forests dominated by Pinus and Picea,suggesting a colder and somewhat more humid climate compared to the previous stage.Pollen Zone Ⅲ(37.28-23.56 ka)features a coniferous forest with a grassland landscape where herbs increased again,reflecting a cold and dry climate.Pollen Zone Ⅳ(23.56 ka to present)is marked by a sharp increase in Picea and a forest meadow landscape,with a climate that gradually transitioned to cold and wet.The climatic evolution in this area follows a sequence of cool-dry,cold-humid,cold-dry,and cold-wet,exhibiting an alternating pattern of cold-wet to warm-dry conditions.

关键词

孢粉组合/晚更新世/古气候/植被类型/三江平原

Key words

pollen assemblage/Late Pleistocene/paleoclimate/vegetation type/Sanjiang Plain

分类

天文与地球科学

引用本文复制引用

赵建,孔繁鹏,张苍江,张也,刘洪博,邵吉亮,张磊,董凯..三江平原宝清地区晚更新世晚期以来孢粉组合及古气候[J].地质与资源,2026,35(2):133-140,8.

基金项目

中国地质调查局项目"三江平原宝清地区黑土地地表基质层调查"(DD20211588)、"三江平原宝清湿地退化区1∶5万地表基质调查"(DD20242039) (DD20211588)

自然资源综合调查指挥中心科技创新基金资助项目"高强度利用下黑土地地表基质养分元素变化规律及机理研究"(KC20220002). (KC20220002)

地质与资源

1671-1947

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