青海湖近800年来沉积物介形虫Li/Ca比值的古环境指示意义
PALAEOENVIRONMENTAL IMPLICATIONS OF LI/CA RATIOS OF OSTRACOD SHELLS FROM LAKE QINGHAI DURING THE PAST 800YEARS
查看参考文献28篇
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文摘
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当前古气候研究的热点是获取最近2 000a来连续的高分辨率自然记录. 为了解决湖泊沉积代用指标中古温度指标的难题,通过对青海湖沉积物单一种属介形虫壳体胖真星介(Eucypris inflata)Li/Ca比值的测定,结合已有的~(210)Pb和~(137)Cs测定的沉积物沉积速率[1],成功恢复了青海湖底层水的古温度变化序列. 将Li/Ca比值曲线与气象记录以及邻近地区都兰和祁连山树轮宽度指数恢复的温度变化序列对比,发现介形虫壳体Li/Ca比值与温度呈明显的负相关变化, Li/Ca比值高,温度低, Li/Ca比值低,温度高,表明介形虫Li/Ca比值是一种有效的古温度指示剂 |
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其他语种文摘
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Acquiring continuous and high resolution natural records in recent 2000years is the hotspot in palaeoclimate research. In order to resolve the problem of temperature proxy as an indicator for lake sedimentation, based on the Li/Ca ratios of shells of a single ostracod species Eucypris inflate retrieved from the Lake Qinghai sediments, together with the existing sedimentation rate data derived from ~(210) Pb and ~(137) Cs from Xu et al.(2006),we have successfully reconstructed the variation in temperature during the past 800-years for the Lake Qinghai. By Comparison of ostracod Li/Ca ratios with temperatures inferred from meteorologic records and tree ring widths in Dulan and Qilianshan,we found that Li/Ca ratios of ostracod shells negatively correlate with temperatures. Higher temperatures correspond to lower Li/Ca ratios, and vice versa, suggesting that ostracod Li/Ca ratio probably is an effective proxy for bottom water temperature |
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来源
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海洋地质与第四纪地质
,2010,30(4):115-121 【核心库】
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关键词
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胖真星介
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Li/Ca比值
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温度
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有效代用指标
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青海湖
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地址
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1.
中国科学院地球化学研究所, 环境地球化学国家重点实验室;;重庆市矿产地质与环境地质重点实验室;;煤炭资源与安全开采国家重点实验室, 贵阳, 550002
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重庆地质矿产研究院, 重庆, 400042
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中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵阳, 550002
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中国科学院地球化学研究所, 环境地球化学国家重点实验室;;重庆市矿产地质与环境地质重点实验室, 贵阳, 550002
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中国科学院地球化学研究所, 矿床地球化学国家重点实验室, 贵阳, 550002
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语种
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中文 |
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ISSN
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0256-1492 |
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学科
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地质学 |
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基金
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国家自然科学基金项目
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国家973计划
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文献收藏号
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CSCD:3982846
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参考文献 共
28
共2页
|
|
1.
Xu H. Geochronology of a surface core in the northern basin of Lake Qinghai: Evidence from ~(210) Pb and ~(137)Cs radionuclides.
Chinese Journal of Geochemistry,2006,25:301-306
|
CSCD被引
14
次
|
|
|
|
|
2.
PAGES.
Palaeoclimates of the Northern and Southern Hemispheres,1995:1-92
|
CSCD被引
1
次
|
|
|
|
|
3.
Chivas A R. Strontium content of ostracods indicates lacustrine paleosalinity.
Nature,1985,316:251-253
|
CSCD被引
24
次
|
|
|
|
|
4.
Yu Z C. A 2 100-year traceelement and stable isotope record and decadal resolution from Rice Lake in the Northern Great Palins,USA.
The Holocene,2002,12:605-617
|
CSCD被引
4
次
|
|
|
|
|
5.
Liu X D. A 1 100-year palaeoenvironmental record inferred from stable isotope and trace element compositions of ostracode and plant caryopses in sediments of Cattle Pond, Dongdao Island, South China Sea.
Journal of Paleolimnology,2008,40:987-1002
|
CSCD被引
9
次
|
|
|
|
|
6.
Zhang J W. An 850-year ostracod-shell trace-element record from Sugan Lake, northern Tibetan Plateau, China: Implications for interpreting the shell chemistry in high-Mg/Ca waters.
Quaternary International,2009,194:119-133
|
CSCD被引
3
次
|
|
|
|
|
7.
胡广. 利用介形类壳体Sr,Mg重建古环境受自生碳酸盐矿物的限制及机理探讨.
中国科学D辑,2008,38:177-186
|
CSCD被引
7
次
|
|
|
|
|
8.
张恩楼. 近0.9 ka来青海湖湖水盐度的定量恢复.
科学通报,2004,49:697-701
|
CSCD被引
30
次
|
|
|
|
|
9.
Lister G S. Lake Qinghai, China: closed-basin lake levels and the oxygen isotope record for ostracode since the latest Pleistocene.
Palaeogeography, Palaeoclimatology, Palaeoecology,1991,84:141-162
|
CSCD被引
125
次
|
|
|
|
|
10.
Marriott C S. Effect of mineralogy, salinity, and temperature on Li/Ca and Li isotope composition of calcium carbonate.
Chemical Geology,2004,212:5-15
|
CSCD被引
19
次
|
|
|
|
|
11.
Montagna P. Li/Ca ratios in the Mediterranean non-tropical coral Cladocora caespitosa as a potential paleothermometer.
Geophysical Research Letters,2006,8:3695-3697
|
CSCD被引
2
次
|
|
|
|
|
12.
Shen J. Palaeoclimatic changes in the Qinghai Lake area during the last 18 000years.
Quaternary International,2005,136:131-140
|
CSCD被引
221
次
|
|
|
|
|
13.
Xu H. Stable isotopes in bulk carbonates and organic matter in recent sediments of Lake Qinghai and their climatic implications.
Chemical Geology,2006,235:262-275
|
CSCD被引
52
次
|
|
|
|
|
14.
Xu H. Precipitation at Lake Qinghai, NE Qinghai-Tibet Plateau, and its relation to Asian summer monsoons on decadal/interdecadal scales during the past 500 years.
Palaeogeography, Palaeoclimatology, Palaeoecology,2007,254:541-549
|
CSCD被引
15
次
|
|
|
|
|
15.
王苏民.
中国湖泊志,1998:472-474
|
CSCD被引
5
次
|
|
|
|
|
16.
Marriott C S. Temperature dependence of δ7 Li,δ44 Ca and Li/Ca during growth of calcium carbonate.
Earth and Planetary Science Letters,2004,222:615-624
|
CSCD被引
18
次
|
|
|
|
|
17.
Henderdon A C G. A carbonand oxygen-isotope record of recent environmental change from Qinghai Lake,NE Tibetan Plateau.
Chinese Science Bulletin,2003,48:1463-1468
|
CSCD被引
1
次
|
|
|
|
|
18.
Liu X Q. Southwest monsoon changes indicated by oxygen isotope of ostracode shells from sediments in Qinghai Lake since the last Glacial.
Chinese Science Bulletin,2007,52:539-544
|
CSCD被引
34
次
|
|
|
|
|
19.
Hall J M. Li/Ca in multiple species of benthic and palnktonic foraminifera: Thermocline, latitudinal, and glacialinterglacial variation.
Geochimica et Cosmochimica Acta,2004,68:529-545
|
CSCD被引
3
次
|
|
|
|
|
20.
Titiloye J O. Atomistic simulation of calcite surfaces and the influence of growth additives on their morphology.
Journal of Crystal Growth,1993,131:533-545
|
CSCD被引
7
次
|
|
|
|
|
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