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柴达木贝壳堤剖面元素地球化学与环境演变 被引量:20
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作者 张文翔 张虎才 +5 位作者 雷国良 杨伦庆 牛洁 常凤琴 杨明生 樊红芳 《第四纪研究》 CAS CSCD 北大核心 2008年第5期917-928,共12页
通过对柴达木盆地察尔汗古湖贝壳堤沉积物中酸溶与残留(酸不溶)组分中常、微量元素及其元素对的分析,并结合酸溶与残留组分中常、微量元素相关性对比,讨论了贝壳堤剖面元素地球化学指标和沉积环境之间的关系,指出酸溶组分中的常量、微... 通过对柴达木盆地察尔汗古湖贝壳堤沉积物中酸溶与残留(酸不溶)组分中常、微量元素及其元素对的分析,并结合酸溶与残留组分中常、微量元素相关性对比,讨论了贝壳堤剖面元素地球化学指标和沉积环境之间的关系,指出酸溶组分中的常量、微量元素及其元素对可以作为湖泊和古气候演化良好的代用指标;残留组分中的元素及元素对与原岩及其风化程度紧密相关,因此,酸溶组分与残留组分中的常量和微量元素在对于环境响应模式存在一定差异,应该将二者分开研究以避免对元素所携带环境信号解译的偏差。根据元素地球化学指标重建了43.5~22.4cal.kaB.P.(39.7~17.5kaB.P.14C年代)柴达木盆地察尔汗古湖高湖面期间古气候与环境演变过程:43.5~31.7kaB.P.期间酸溶组分中元素含量总体较低,残留组分中元素含量相对较高,且湿润度值((Fe2O3+Al2O3)/(MgO+CaO),或H)处于高值段,而Ca/Mg,Fe/Mn和Rb/Sr则处于低值段,指示了温暖湿润的气候环境,古湖泊水体增加;其中37.8~31.7kaB.P.期间酸溶组分中元素含量多出现最低值,残留组分中元素含量富集,H值较高,而Ca/Mg,Fe/Mn和Rb/Sr此段均值最小,表明此时为环境的最适宜期,此期间降雨充沛,湖泊处于高湖面;在31.7~22.4kaB.P.期间酸溶组分中元素含量普遍较高,残留组分中元素含量相对富集,且Ca/Mg,Fe/Mn和Rb/Sr处于高值段波动,H值处在低值段,指示气候环境恶化,降水逐渐减少,古湖泊水体萎缩;在约22.4kaB.P.气候快速恶化,形成石盐结晶,高湖面历史结束。柴达木盆地该期高湖面及其演化过程可与腾格里沙漠和额济纳盆地-巴丹吉林沙漠高湖面记录进行对比,揭示了大范围气候变化的历史。 展开更多
关键词 察尔汗湖 贝壳堤剖面 元素地球化学 环境演变
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Branched aliphatic alkanes of shell bar section in Qarhan Lake,Qaidam Basin and their paleoclimate significance 被引量:14
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作者 ZHANG HuCai CHANG FengQin +6 位作者 LI Bin LEI GuoLiang CHEN Yue ZHANG WenXiang NIU Jie FAN HongFang YANG MingSheng 《Chinese Science Bulletin》 SCIE EI CAS 2007年第9期1248-1256,共9页
Biomarkers of paleolake deposits from Qarhan Salt Lake in Qaidam Basin,northwest China were sys-tematically analyzed and the A―C series compounds of branched aliphatic alkanes with quaternary substituted carbon atom(... Biomarkers of paleolake deposits from Qarhan Salt Lake in Qaidam Basin,northwest China were sys-tematically analyzed and the A―C series compounds of branched aliphatic alkanes with quaternary substituted carbon atom(BAQCs) were identified. The homologous distinguished three series,A―C,were identified as 5,5-diethylalkanes,6,6-diethylalkanes and 5-butyl,5-ethylalkanes series,and their relative abundance was A > B > C. Series A and C were characterized by odd carbon numbers,whereas series B was characterized by even carbon numbers. The high values of series A corresponded with the high values of series B and C. Therefore,it can be concluded that series A,B and C possess a similar biological origin. The abundance of series A was relatively low in the lower part of the section compared with that in the upper part,implying that these series originated from bacteria and/or algae more prevalent in fresh-mesohaline water,and such kinds of bacteria and/or algae are most likely to be thermophilous species. The A25/nC25 ratio differences in the section show that such branched aliphatic alkanes can be treated as one kind of environmental change proxy for paleolake evolution and may provide important information for the climate reconstruction of the Late Pleistocene. 展开更多
关键词 柴达木盆地 察尔汗盐湖 贝壳堤剖面 侧链脂族烷 古气候意义
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