Relationship between calcium and atmospheric dust recorded in Guliya ice core

2004 ◽  
Vol 49 (7) ◽  
pp. 706-710 ◽  
Author(s):  
Tandong Yao ◽  
Guangjian Wu ◽  
Jianchen Pu ◽  
Keqin Jiao ◽  
Cuilan Huang
2021 ◽  
Vol 15 (4) ◽  
pp. 2109-2114
Author(s):  
Shugui Hou ◽  
Wangbin Zhang ◽  
Ling Fang ◽  
Theo M. Jenk ◽  
Shuangye Wu ◽  
...  

Abstract. There is considerable controversy regarding the age ranges of Tibetan ice cores. The Guliya ice core was reported to reach as far back as ∼760 ka (kiloannum, i.e. 1000 years), whereas chronologies of all other Tibetan cores cover at most the Holocene. Here we present ages for two new ice cores reaching bedrock, from the Zangser Kangri (ZK) glacier in the northwestern Tibetan Plateau and the Shulenanshan (SLNS) glacier in the western Qilian Mountains. We estimated bottom ages of 8.90±0.570.56 ka and 7.46±1.461.79 ka for the ZK and SLNS ice core respectively, further constraining the time range accessible by Tibetan ice cores to the Holocene.


2019 ◽  
Vol 13 (6) ◽  
pp. 1743-1752 ◽  
Author(s):  
Shugui Hou ◽  
Wangbin Zhang ◽  
Hongxi Pang ◽  
Shuang-Ye Wu ◽  
Theo M. Jenk ◽  
...  

Abstract. Ice cores from the Tibetan Plateau (TP) are widely used for reconstructing past climatic and environmental conditions that extend beyond the instrumental period. However, challenges in dating and interpreting ice core records often lead to inconsistent results. The Guliya ice core drilled from the northwestern TP suggested a cooling trend during the mid-Holocene based on its decreasing δ18O values, which is not observed in other Tibetan ice cores. Here we present a new high-resolution δ18O record of the Chongce ice cores drilled to bedrock ∼30 km away from the Guliya ice cap. Our record shows a warming trend during the mid-Holocene. Based on our results as well as previously published ice core data, we suggest that the apparent discrepancy between the Holocene δ18O records of the Guliya and the Chongce ice cores may be attributed to a possible misinterpretation of the Guliya ice core chronology.


2007 ◽  
Vol preprint (2008) ◽  
pp. 1
Author(s):  
S. Kaspari ◽  
P. A. Mayewski ◽  
M. Handley ◽  
S. Kang ◽  
S. Hou ◽  
...  

1999 ◽  
Vol 29 ◽  
pp. 136-140
Author(s):  
Wang Ninglian ◽  
Yao Tandong ◽  
Qin Dahe ◽  
L. G. Thompson ◽  
E. Mosley-Thompson ◽  
...  

AbstractA 36C1 peak has been found at about 37 ka BP in the Guliya ice core, drilled from the Qinghai-Tibetan Plateau. This peak is indicative of enhanced cosmogenic isotope production in the atmosphere, rather than a change in accumulation rate. Comparison with the records of 10Be and 36C1 in ice cores from Antarctica and Greenland indicates that peaks of the cosmogenic isotopes are global, and that they can be used as time markers for dating ice cores. Interestingly, the 37 ka BP global event coincided with a cold period.


1998 ◽  
Vol 43 (10) ◽  
pp. 841-844 ◽  
Author(s):  
Ninglian Wang ◽  
Tandong Yao ◽  
L. G. Thompson

2007 ◽  
Vol 112 (D10) ◽  
Author(s):  
Teppei J. Yasunari ◽  
Takayuki Shiraiwa ◽  
Syosaku Kanamori ◽  
Yoshiyuki Fujii ◽  
Makoto Igarashi ◽  
...  

2010 ◽  
Vol 44 (25) ◽  
pp. 2980-2989 ◽  
Author(s):  
Shichang Kang ◽  
Yulan Zhang ◽  
Yongjun Zhang ◽  
Bjorn Grigholm ◽  
Susan Kaspari ◽  
...  

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