<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.clim-past-discuss.net/inc/cpd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>5</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cpd-5-1493-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/1493/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/1493/2009/cpd-5-1493-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/1493/2009/cpd-5-1493-2009.pdf</fulltext_pdf>
	<start_page>1493</start_page>
	<end_page>1520</end_page>
	<publication_date>2009-05-25</publication_date>
	<article_title content_type="html">Synchronous variations of precipitation and temperature at Lake Qinghai, NE Tibetan Plateau during the past 800 years and their relations to solar activity: evidence from Li/Ca ratios and &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O values of ostracod shells</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>Z. Zhu</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Chen</name>
			<email>chenjingan@vip.skleg.cn</email>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>J. Li</name>
		</author>
		<author numeration="4" affiliations="1,2">
			<name>Y. Zeng</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>J. Li</name>
		</author>
		<author numeration="6" affiliations="1,2">
			<name>J. Wang</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>L. Qi</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">The State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China</affiliation>
		<affiliation numeration="2" content_type="html">Graduate School of Chinese Academy of Sciences,Beijing 100049, China</affiliation>
		<affiliation numeration="3" content_type="html">The State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China</affiliation>
	</affiliations>
	<abstract content_type="html">Variations of precipitation and temperature at Lake Qinghai, NE Tibetan Plateau
on decadal scales during the past 800 years were reconstructed based on the oxygen
isotope values and Li/Ca ratios from ostracod shells of the single species &lt;i&gt;Eucypris
inflata&lt;/i&gt;. Higher temperature relates to lower Li/Ca ratios; higher precipitation relates
to lower &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O values, and &lt;i&gt;vice versa&lt;/i&gt;. The good correlation between Li/Ca ratios and &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O
values of ostracod shells indicates that temperature variations corresponded well with
precipitation variations on decadal scales during the past 800 years. Variations of
precipitation and temperature are synchronous with variations of solar activity
reconstructed from the atmospheric &lt;sup&gt;14&lt;/sup&gt;C concentration in tree rings and the &lt;sup&gt;10&lt;/sup&gt;Be
concentration in ice cores. These findings suggest that, on decadal scales solar
activity may be responsible for the synchronous variations of precipitation and
temperature at Lake Qinghai, NE Tibetan Plateau during the past 800 years.
Keywords: Precipitation variations; Temperature variations; &lt;i&gt;Eucypris inflata&lt;/i&gt;;
Li/Ca; &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O; Synchronous variations; Lake Qinghai; Solar activity.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Bard, E., Raisbeck, G., Yiou, F., and Jouzel, J.: Solar irradiance during the last 1200 years based on cosmogenic nuclides, Tellus, 52B, 985–992, 2000. </reference>
		<reference numeration="2" content_type="text"> Broecker, W. S. and Peng, T. H.: Tracers in the Sea, Eldigio Press, New York, 1982. </reference>
		<reference numeration="3" content_type="text"> Chen, J. A., Wan, G. J., Wang, F. S., Huang, R. G., Zhang, F., Zhang, D. D., and Schmidt, R.: Environmental records of carbon in recent lake sediments, Sci. China (Ser. D), 45, 875–884, 2002. </reference>
		<reference numeration="4" content_type="text"> Chen, J. A., Wan, G. J., Zhang, D. D., Chen, Z. L., Xu, J. Y., Xiao, T. F., and Huang, R. G.: The &quot;Little Ice Age&quot; recorded by sediment chemistry in Lake Erhai, Southwest China, The Holocene, 15, 925–931, 2005. </reference>
		<reference numeration="5" content_type="text"> Chivas, A. R., De Deckker, P., and Shelley, J. M. G.: Strontium content of ostracods indicates lacustrine paleosalinity, Nature, 316, 251–253, 1985. </reference>
		<reference numeration="6" content_type="text"> Craig, H.: The measurement of oxygen isotope palaeotemperatures, in: Stable Isotopes in Oceanographic Studies and Palaeotemperatures, edited by: Tongiorg, E., Consiglio Nazionale delle Ricerche, Pisa, 161–182, 1965. </reference>
		<reference numeration="7" content_type="text"> Crowley, T. J.: Causes of climate change over the past 1000 years, Science, 289, 270–276, 2000. </reference>
		<reference numeration="8" content_type="text"> Dean, J. A.: Lange&apos;s handbook of chemistry, McGraw–Hill, New York, 1992. </reference>
		<reference numeration="9" content_type="text"> Epstein, S., Buchsbaum, R., Lowestam, H. A., and Urey, H. C.: Revised carbonate water isotopic temperature scale, Geol. Soc. Am. Bull., 64, 1315–1326, 1953. </reference>
		<reference numeration="10" content_type="text"> Fleitmann, D., Burns, S. J., Mudelsee, M., Neff, U., Kramers, J., Mangini, A., and Matter, A.: Holocene forcing of the Indian monsoon recorded in a stalagmite from southern Oman, Science, 300, 1737–1739, 2003. </reference>
		<reference numeration="11" content_type="text"> Fleitmann, D., Burns, S. J., Neff, U., Mudelsee, M., Mangini, A., and Matter, A.: Palaeoclimatic interpretation of high-resolution oxygen isotope profiles derived from annually laminated speleothems from southern Oman, Quaternary Sci. Rev., 23, 935–945, 2004. </reference>
		<reference numeration="12" content_type="text"> Fritz, P., Anderson, T. W., Lewis, C. F. M.: Late Quaternary climatic trends and history of Lake Erie from stable isotope studies, Science, 190, 267–269, 1975. </reference>
		<reference numeration="13" content_type="text"> Grafenstein, U. V., Erlernkeuser, H., and Trimborn, P.: Oxygen and carbon isotopes in modern fresh-water ostracod valves: assessing vital effect and autecological effects of interest for paleoclimate studies, Palaeogeogr. Palaeocl., 148, 133–152, 1999. </reference>
		<reference numeration="14" content_type="text"> Hall, J. M. and Chan, L. H.: Li/Ca in multiple species of benthic and planktonic foraminifera: Thermocline, latitudinal, and glacial-interglacial variation, Geochim. Cosmochim. Ac., 68, 529–545, 2004. </reference>
		<reference numeration="15" content_type="text"> Henderson, A. C. G., Holmes, J. A., Zhang, J. W., Leng, M. J., and Carvalho, L. R.: A carbon- and oxygen-isotope record of recent environmental change from Lake Qinghai, NE Tibetan Plateau, Chinese Sci. Bull., 48, 1463–1468, 2003. </reference>
		<reference numeration="16" content_type="text"> Henderson, A. C. G. and Holmes, J. A.: Palaeolimnological evidence for environmental change over the past millennium from Lake Qinghai sediments: A review and future research prospectives, Quaternary Int., 194, 134–147, 2009. </reference>
		<reference numeration="17" content_type="text"> Heyvaert, A. C: The biogeochemistry and palaeolimnology of sediments from Lake Tahoe, California–Nevada, Doctoral dissertation of University of California, 1998. </reference>
		<reference numeration="18" content_type="text"> Hodell, D. A., Brenner, M., Curtis, J. H., and Guilderson, T.: Solar forcing of drought frequency in the Maya lowlands, Science, 292, 1367–1370, 2001. </reference>
		<reference numeration="19" content_type="text"> Holmes, J. A.: Trace element and stable-isotope geochemistry of non-marine ostracod shells in quaternary palaeoenvironmental reconstruction, J. Paleolimnol., 15, 223–235, 1996. </reference>
		<reference numeration="20" content_type="text"> Hong, Y. T., Hong, B., Lin, Q. H., Zhu, Y. X., Shibata, Y., Hirota, M., Uchida, M., Leng, X. T., Jiang, H. B., Xu, H., Wang, H., and Yi, L.: Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene, Earth Planet Sci. Lett., 211, 369–378, 2003. </reference>
		<reference numeration="21" content_type="text"> Hong, Y. T., Wang, Z. G., Jiang, H. B., Lin, Q. H., Hong, B., Zhu, Y. X., Wang, Y., Xu, L. S., Leng, X. T., and Li, D. H.: A 6000-year record of changes in drought and precipitation in northeastern China based on $\delta^13$C time series from peat cellulose, Earth Planet Sci. Lett., 185, 111–119, 2001. </reference>
		<reference numeration="22" content_type="text"> Huh, Y., Chan, L. H., Zhang, L., and Edmond, J. M.: Lithium and its isotopes in major world rivers: implications for weathering and the oceanic budget, Geochim. Cosmochim. Ac., 62, 2039–2051, 1998. </reference>
		<reference numeration="23" content_type="text"> Ji, J. F., Shen, J., Balsam, W., Chen, J., Liu, L. W., and Liu, X. Q.: Asian monsoon oscillations in the northeastern Qinghai-Tibet Plateau since the late glacial as interpreted from visible reflectance of Qinghai Lake sediments, Earth Planet Sci. Lett., 233, 61–70, 2005. </reference>
		<reference numeration="24" content_type="text"> Leng, M. J. and Marshall, J. D.: Palaeoclimate interpretation of stable isotope data from lake sediment archives, Quaternary Sci. Rev., 23, 811–831, 2004. </reference>
		<reference numeration="25" content_type="text"> Li, X. Z., Liu, W. G., Zhang, P. X., An, Z. S., and Zhang, L.: Species, valve size, and pretreatment effects on $\delta^18$O and $\delta^13$C values of ostracod valves from Lake Qinghai, Qinghai-Tibet Plateau, Chem. Geol., 246, 124–134, 2007. </reference>
		<reference numeration="26" content_type="text"> Lister, G. S., Kelts, K., Chen, K. Z., Yu, J. Q., and Niessen, F.: Lake Qinghai, China: closed-basin lake levels and the oxygen isotope record for ostracode since the latest Pleistocene, Palaeogeogr. Palaeocl., 84, 141–162, 1991. </reference>
		<reference numeration="27" content_type="text"> Liu, X. D., Sun, L. G., Wei, G. J., Wang, Y. H., Yan, H., Liu, K. X., and Wu, X. H.: A 1100-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, J. Paleolimnol., 40, 987–1002, 2008. </reference>
		<reference numeration="28" content_type="text"> Liu, X. H., Qin, D. H., Shao, X. M., Chen, T., and Ren, J. W.: Temperature variations during the last millennium in Mid-Qilian Mountain inferred from tree rings, Sci. China (Ser. D), 34, 89–95, 2004. </reference>
		<reference numeration="29" content_type="text"> Liu, X. Q., Shen, J., Wang, S. M., Wang, Y. B., and Liu, W. G.: Southwest monsoon changes indicated by oxygen isotope of ostracode shells from sediments in Qinghai Lake since the last Glacial, Chinese Sci. Bull., 52, 539–544, 2007. </reference>
		<reference numeration="30" content_type="text"> Liu, X. Q., Shen, J., Wang, S. M., Yang, X. D., Tong, G. B., and Zhang, E. L.: A 16 000-year pollen record of Qinghai Lake and its paleoclimate and paleoenvironment, Chinese Sci. Bull., 47, 1931–1937, 2002. </reference>
		<reference numeration="31" content_type="text"> Liu, Y., An, Z. S., Ma, H. Z., Cai, Q. F., Liu, Z. Y., Kutzbach, J. K., Shi, J. F., Song, H. M., Sun, J. Y., Yi, L., Li, Q., Yang, Y. K., and Wang, L.: Precipitation variations in the northeastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the Northern Hemisphere temperature, Sci. China (Ser. D), 49, 408–420, 2006. </reference>
		<reference numeration="32" content_type="text"> LZBCAS (Lanzhou Branch of Chinese Academy of Sciences): Evolution of recent environment in Qinghai Lake and its prediction, Science Press, Beijing, 1994 (in Chinese). </reference>
		<reference numeration="33" content_type="text"> Magny, M.: Holocene climate variability as reflected by mid-European lake-level fluctuations and its probable impact on prehistoric human settlements, Quatern. Int., 113, 65–79, 2004. </reference>
		<reference numeration="34" content_type="text"> Marriott, C. S., Henderson, G. M., Belshaw, N. S., and Tudhope, A. W.: Temperature dependence of $\delta^7$Li, $\delta^44$Ca and Li/Ca during growth of calcium carbonate, Earth Planet Sc. Lett., 222, 615–624, 2004a. </reference>
		<reference numeration="35" content_type="text"> Marriott, C. S., Henderson, G. M., Crompton, R., Staubwasser, M., and Shaw, S.: Effect of mineralogy, salinity, and temperature on Li/Ca and Li isotope composition of calcium carbonate, Chem. Geol., 212, 5–15, 2004b. </reference>
		<reference numeration="36" content_type="text"> Montagna, P., McCulloch, M., Mazzoli, C., Silenzi, S., and Schiaparelli, S.: Li/Ca ratios in the Mediterranean non-tropical coral \textitCladocora caespitosa as a potential paleothermometer, Geophys. Res. Lett., 8, 3695–3696, 2006. </reference>
		<reference numeration="37" content_type="text"> Muscheler, R., Joos, F., Beer, J., Muller, S. A., Vonmoos, M., and Snowball, I.: Solar activity during the last 1000 yr inferred from radionuclide records, Quaternary Sci. Rev., 26, 82–97, 2007. </reference>
		<reference numeration="38" content_type="text"> Parker, S. C., Titiloye, J. O., and Watson, G. W.: Molecular modelling of carbonate minerals-studies of growth and morphology, Philoso. T. R. Soc. A., 344, 37–48, 1993. </reference>
		<reference numeration="39" content_type="text"> Reid, G. C.: Solar total irradiance variations and the global sea surface temperature record, J. Geophys. Res., 96, 2835–2844, 1991. </reference>
		<reference numeration="40" content_type="text"> Shao, X. M., Huang, L., Liu, H. B., Liang, E. Y., Fang, X. Q., and Wang, L. L.: Reconstruction of precipitation variations from tree rings in recent 1000 years in Delingha, Qinghai, Sci. China (Ser. D), 48, 939–949, 2005. </reference>
		<reference numeration="41" content_type="text"> Shen, J., Liu, X. Q., Wang, S. M., and Matsumoto, M.: Palaeoclimatic changes in the Qinghai Lake area during the last 18 000 years, Quatern. Int., 136, 131–140, 2005. </reference>
		<reference numeration="42" content_type="text"> Solanki, S. K., Usoskin, I. G., Schussler, M., and Beer, J.: Unusual activity of the Sun during recent decades compared to the previous 11 000 years, Nature, 43, 1084–1087, 2004. </reference>
		<reference numeration="43" content_type="text"> Stuiver, M.: Oxygen and carbon isotope ratios of fresh water carbonates as climatic indicators, J. Geophys. Res., 75, 5247–5257, 1970. </reference>
		<reference numeration="44" content_type="text"> Stuiver, M., Braziunas, T. F., Grootes, P. M., and Zielinski, G. A.: Is there evidence for solar forcing of climate in the GISP2 oxygen isotope record?, Quaternary Res. Rev., 48, 259–266, 1997. </reference>
		<reference numeration="45" content_type="text"> Stuiver, M., Reimer, P. J., Bard, E., Beck, J. W., Burr, G. S., Hughen, K. A., Kromer, B., McCormac, G., Plicht, J., and Spurk, M.: INTCAL 98 radiocarbon age calibration, 24 000-0 cal BP, Radiocarbon, 40, 1041–1083, 1998. </reference>
		<reference numeration="46" content_type="text"> Talbot, M. R.: A review of the palaeohydrological interpretation of carbon and oxygen isotopic ratios in primary lacustrine carbonates, Chem. Geol., 80, 261–279, 1990. </reference>
		<reference numeration="47" content_type="text"> Tan, M., Hou, J. S., and Liu, T. S.: Sun-coupled climate connection between Eastern Asia and Northern Atlantic, Geophys. Res. Lett., 31, 1–3, 2004. </reference>
		<reference numeration="48" content_type="text"> Liangcheng Tan, , Yanjun Cai, , Liang Yi, , Zhisheng An, , and Li Ai, : Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity, Clim. Past, 4, 19–28, 2008. </reference>
		<reference numeration="49" content_type="text"> Titiloye, J. O., Parker, S. C., and Mann. S.: Atomistic simulation of calcite surfaces and the influence of growth additives on their morphology, J. Cryst. Growth, 131, 533–545, 1993. </reference>
		<reference numeration="50" content_type="text"> Tomascak, P. B., Hemming, N. G., and Hemming, S. R.: The lithium isotopic composition of waters of the Mono Basin, California, Geochim. Cosmochim. Ac., 67, 601–611, 2003. </reference>
		<reference numeration="51" content_type="text"> Usoskin, I. G., Solanki, S. K., and Schussler, M.: Millennium-scale sunspot number reconstruction: evidence for an usually active Sun since the 1940s, Phys. Rev. Lett., 91, 211101–211104, 2003. </reference>
		<reference numeration="52" content_type="text"> Wang, S. M. and Dou, H. S.: Lakes in China, Science Press, Beijing, 1998 (in Chinese). </reference>
		<reference numeration="53" content_type="text"> Wang, Y. J., Cheng, H., Edwards, R. L., He, Y. Q., Kong, X. G., An, Z. S., Wu, J. Y., Kelly, M. J., Dykosko, C. A., and Li, X. D.: The Holocene Asian monsoon: Links to solar changes and North Atlantic climate, Science, 308, 854–857, 2005. </reference>
		<reference numeration="54" content_type="text"> Wei, K. and Gasse, F.: Oxygen isotopes in lacustrine carbonates of West China revisited: implications for post glacial changes in summer monsoon circulation, Quaternary Sci. Rev., 18, 1315–1334, 1999. </reference>
		<reference numeration="55" content_type="text"> Xiao, S. B., Li, A. C., Liu, J. P., Chen, M. H., Xie, Q., Jiang, F. Q., Li, T. G., Xiang, R., and Chen, Z.: Coherence between solar activity and the East Asian winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea, Palaeogeogr. Palaeocl., 237, 293–304, 2006. </reference>
		<reference numeration="56" content_type="text"> Xu, H., Ai, L., Tan, L. C., and An, Z. S.: Geochronology of a surface core in the northern basin of Lake Qinghai: Evidence from $^210$Pb and $^137$Cs radionuclides, Chinese J. Geochem., 25, 301–306, 2006a. </reference>
		<reference numeration="57" content_type="text"> Xu, H., Ai, L., Tan, L. C., and An, Z. S.: Stable isotopes in bulk carbonates and organic matter in recent sediments of Lake Qinghai and their climatic implications, Chem. Geol., 235, 262–275, 2006b. </reference>
		<reference numeration="58" content_type="text"> Xu, H., Hou, Z. H., Ai, L., and Tan, L. C.: Precipitation at Lake Qinghai, NE Qinghai-Tibet Plateau, and its relation to Asian summer monsoons on decadal/interdecadal scales during the past 500 years, Palaeogeogr. Palaeocl., 254, 541–549, 2007. </reference>
		<reference numeration="59" content_type="text"> Xu, H., Liu, X. Y., and Hou, Z. H.: Temperature variations at Lake Qinghai on decadal scales and the possible relation to solar activities, J. Atmos. Sol.-Terr. Phy., 70, 138–144, 2008. </reference>
		<reference numeration="60" content_type="text"> Yao, T. D., Yang, M. X., and Kang, X. C.: Comparative study of the climate changes in the past 2000 years by using ice core and tree ring records, Quaternary Sci. Rev., 21, 514–519, 2001 (in Chinese with English abstract). </reference>
		<reference numeration="61" content_type="text"> Yu, J. Q. and Kelts, K. R.: Abrupt changes in climatic conditions across the Late-glacial/Holocene on the N. E. Tibet-Qinghai Plateau: evidence from Lake Qinghai, China, J. Paleolimnol., 28, 195–206, 2002. </reference>
		<reference numeration="62" content_type="text"> Yu, Z. C. and Ito, E.: Possible solar forcing of century-scale drought frequency in the northern Great Plain, Geology, 27, 263–266, 1999. </reference>
		<reference numeration="63" content_type="text"> Zhang, D. E., Li, X. Q., and Liang, Y. Y.: Complement of the Chinese Drought/Flood index during 1993–2000, J. Appl. Meteorol. Sci., 14, 379–383, 2003a (in Chinese with English abstract). </reference>
		<reference numeration="64" content_type="text"> Zhang, E. L., Shen, J., Wang, S. M., Yin, Y., Zhu, Y. X., and Xia, W. L.: Quantitative reconstruction of the paleosalinity at Qinghai Lake in the past 900 years, Chinese Sci. Bull., 49, 730–734, 2004. </reference>
		<reference numeration="65" content_type="text"> Zhang, J. W., Jin, M., Chen, F. H., Battarbee, R. W., and Henderson, A. C. G.: High-resolution precipitation variations in the Northeastern Tibetan Plateau over the past 800 years documented by sediment cores of Qinghai Lake, Chinese Sci. Bull., 48, 1451–1456, 2003b. </reference>
		<reference numeration="66" content_type="text"> Zhang, L., Sun, Z. C., An, Z. S., Liu, W. G., and Li, X. Z.: A preliminary distribution characteristic analysis on different water bodies ostracod from Lake Qinghai area, NW China, Acta. Micropalaeont. Sin., 23, 425–436, 2006 (in Chinese with English abstract). </reference>
		<reference numeration="67" content_type="text"> Zhang, P. X., Zhang, B. Z., Qian, G. M., Li, H. J., and Xu, L. M.: The study of paleoclimatic parameter of Qinghai Lake since Holocene, Quaternary Sci. Rev., 3, 225–237, 1994 (in Chinese with English abstract). </reference>
		<reference numeration="68" content_type="text"> Zhang, P. Z., Cheng, H., Edwards, R. L., Chen, F. H., Wang, Y. J., Yang, X. L., Liu, J., Tan, M., Wang, X. F., Liu, J. H., An, C. L., Dai, Z. B., Zhou, J., Zhang, D. Z., Jia, J. H., Jin, L. Y., and Johnson, K. R.: A test of climate, Sun and culture relationships from an 1810-year Chinese cave record, Science, 322, 940–942, 2008. </reference>
		<reference numeration="69" content_type="text"> Zheng, S. H., Hou, F. G., and Ni, B. N.: Study on the hydrogen and oxygen stable isotopes in precipitation in China, Chinese Sci. Bull., 13, 39–41, 1983 (in Chinese). </reference>
		<reference numeration="70" content_type="text"> Zhu, Z. J., Chen, J. A., Li, J., Zeng, Y., Li, J., Wang, J. F., and Qi, L.: Palaeoenvironmental implications of Li/Ca ratios of ostracod shells from Lake Qinghai during the past 800 years, in preparation, 2009. </reference>
	</references>
</article>

