干旱区生态环境知识资源中心(Arid): 安徽宣城红土微生物GDGTs分布特征及其古环境意义

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	安徽宣城红土微生物GDGTs分布特征及其古环境意义
其他题名	Distributions and Paleo-Environment Implications of Microbial GDGTs from Red Earth Profile in Xuancheng,Anhui Province
	马瑞元 1; 彭红霞 1; 张林 1; 顾延生 2; 胡圣虹 3
来源期刊	地球科学
ISSN	1000-2383
出版年	2015
卷号	40 期号:5 页码:863-869
中文摘要	中国南方更新世红土是古气候环境变化研究非常重要的载体之一,红土微生物类脂分子是其古气候环境研究的有效指标,但其在红土中的古气候意义需要更进一步的挖掘和明确.选取处于气候变化敏感地带并且已有很好年代学基础的安徽宣城红土剖面进行详细的野外调查和系统的样品采集,利用改善后的碱式水解法提取红土微生物类脂分子,通过对比分析、比较印证等方法对其中的甘油二烷基链甘油四醚(glycerol dialkyl glycerol tetraethers,简称GDGTs)进行系统研究.宣城剖面GDGTs分布特征显示:剖面下部各指标呈旋回性变化、而上部相对稳定,表明形成初期环境比较动荡,而后期成土环境相对稳定;土壤pH为7.0~8.0,推测其物源主要来源于北方干旱区或长江中下游干涸河滩沉积;BIT指标反映宣城地区在130ka BP左右气候极为干旱.结果表明,红土中微生物类脂物GDGTs能够定量、高分辨率地重建安徽宣城的古气候环境,具有重要的研究意义.
英文摘要	Abundant information about paleo-environment,paleo-climate and paleolithic culture can be obtained from the red earth in southern China.However,the vermicular paleosol is proposed to be incapable of interpretating the original information about the past climate and envrionment changes owing to the intensive pedogenesis in the tropical-subtropical area.Therefore, previous studies on bio-climatic approaches including pollen,spore fossils and phytoliths are also believed to be not suitable for such kind of stratigraphy.Despite that some studies show the microbial molecular fossils are useful in the paleo-environment reconstruction,but their implications in red earth need to be further explored and confirmed.It is necessary to introduce some new methods to extract the detailed biological information in the red earth.In this study,we collected red earth samples from the Xuancheng section,Anhui Province in the Middle-Lower Reaches of the Yangtze River,which is well-dated and sensitive to climate change.Microbial lipids in the red earth are extracted by employing alkaline hydrolysis combined with the field survey and the laboratory investigation.The characteristics of the microbial lipids,especially glycerol dialkyl glycerol tetraethers (GDGTs)are investigated.The distributions of GDGTs from the Xuancheng profile show that all GDGT-derived proxies in the lower part of profile fluctuates frequently,whereas they are relatively stable in the upper part,which indicates that the paleoenvironment changed frequently during the early period of this profile but the later soil environment was relatively stable.The CBT-inferred soil pH ranges from 7.0to 8.0,indicating that the soil parent material likely comes from the arid areas in northwestern China or alternatively from the dry river sediments in the Middle-Lower Reaches of the Yangtze River.The low BIT values suggest that it was very dry at 130ka BP in the Xuancheng region.
中文关键词	红土 ; 古环境 ; 气候学 ; 环境微生物学
英文关键词	GDGTs red earth GDGTs paleo-environment climatology environmental microbiology
语种	中文
国家	中国
收录类别	CSCD
WOS类目	MINERALOGY
WOS研究方向	Mineralogy
CSCD记录号	CSCD:5422443
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/232500
作者单位	1.(武汉)中国地质大学公共管理学院, 武汉, 湖北 430074, 中国; 2.(武汉)中国地质大学环境学院, 武汉, 湖北 430074, 中国; 3.(武汉)中国地质大学地球科学学院, 武汉, 湖北 430074, 中国
推荐引用方式 GB/T 7714	马瑞元,彭红霞,张林,等. 安徽宣城红土微生物GDGTs分布特征及其古环境意义[J],2015,40(5):863-869.
APA	马瑞元,彭红霞,张林,顾延生,&胡圣虹.(2015).安徽宣城红土微生物GDGTs分布特征及其古环境意义.地球科学,40(5),863-869.
MLA	马瑞元,et al."安徽宣城红土微生物GDGTs分布特征及其古环境意义".地球科学 40.5(2015):863-869.