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松嫩平原北部全新世黑土剖面孢粉组合及其对环境演化的制约

刘凯 宋运红 杨凤超 戴慧敏 许江 韩晓萌 梁帅

地质通报2023,Vol.42Issue(12):2121-2131,11.
地质通报2023,Vol.42Issue(12):2121-2131,11.DOI:10.12097/j.issn.1671-2552.2023.12.008

松嫩平原北部全新世黑土剖面孢粉组合及其对环境演化的制约

Palynological assemblages of Holocene typical black soil profile from northern Songnen Plain and its restricts to environmental evolution

刘凯 1宋运红 1杨凤超 2戴慧敏 1许江 1韩晓萌 1梁帅1

作者信息

  • 1. 中国地质调查局沈阳地质调查中心,辽宁 沈阳 110034||自然资源部黑土地演化与生态效应重点实验室,辽宁沈阳 110034||辽宁省黑土地演化与生态效应重点实验室,辽宁沈阳 110034
  • 2. 中国地质调查局沈阳地质调查中心,辽宁 沈阳 110034
  • 折叠

摘要

Abstract

Paleoclimate and paleoenvironmental evolution is one of the most critical issues in the study of the formation and evolution of black soil.Reconstruction of paleo-vegetation,paleo-climate and paleo-environment,and prediction of the evolution of the climate and environment in the black soil area have become hot spots in black soil research.Fifteen sporopollen samples were collected from a typical black soil profile in the Keshan County of the northern Songnen Plain for pollen research,and total organic carbon in some soil samples from the same stratum was AMS14 C dating.Systematic analysis,identification,and research have shown that three sporo-pollen assemblages from bottom to top were developed in the black soil profile of Keshan County.The lower pollen assemblage is represented by Planted Poaceae-Echinate Asteraceae-Tamarix-Polypodiaceae,the middle pollen assemblage is represented by Tamarix-Chenopodium-Polypodiaceae-Echinate Asteraceae,and the upper pollen assemblage is represented by Pinus-Chenopodium.Comprehensive Quaternary geology and geomorphology,pollen,AMS14C,and element geochemistry analysis all suggest that the typical black soil was mainly formed in the Great Warm Period since the 7500 a B.P.of the Middle Holocene.Which formed in the warm and semi-humid climate of the Songnen Plain,the vegetation is mainly grassland vegetation with herbaceous shrubs.Neotectonic movement is the main internal driving force that controls the evolution of the natural environment in the typical black soil area.The Late Pleistocene yellow clay is the parent material of the typical black soil in the Keshan black soil area,and the development process of the black soil is the process of of soil blackening.

关键词

松嫩平原北部/典型黑土/AMS14C/孢粉组合/古气候/全新世/克山县/环境地质调查工程

Key words

the northern Songliao Plain/typical black soil/AMS14C/palynological assemblage/Paleoclimate/Holocene/Keshan County/environment geological survey engineering

分类

天文与地球科学

引用本文复制引用

刘凯,宋运红,杨凤超,戴慧敏,许江,韩晓萌,梁帅..松嫩平原北部全新世黑土剖面孢粉组合及其对环境演化的制约[J].地质通报,2023,42(12):2121-2131,11.

基金项目

中国地质调查局项目《松辽平原黑土地生态地质调查》(编号:DD20221779) (编号:DD20221779)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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