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Corrigendum to “δ18O, δ13C, elemental content and depositional features of a stalagmite from Yelang Cave reflecting climate and vegetation changes since late Pleistocene in central Guizhou, China [Qua
Min Zhao; Hong-Chun Li; Chuan-Chou Shen; Su-Chen Kang; Chun-Yen Chou
2022
Source PublicationQuaternary International
Volume640Pages:96-97
Abstract

 

 

DOI10.1016/j.quaint.2022.09.002
URL查看原文
Indexed BySCI
Language英语
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/13649
Collection环境地球化学国家重点实验室
Affiliation1.Department of Geosciences, National Taiwan University, Taipei, 10617, Taiwan
2.State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou, 550081, China
3.High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei, 10617, Taiwan
Recommended Citation
GB/T 7714
Min Zhao,Hong-Chun Li,Chuan-Chou Shen,等. Corrigendum to “δ18O, δ13C, elemental content and depositional features of a stalagmite from Yelang Cave reflecting climate and vegetation changes since late Pleistocene in central Guizhou, China [Qua[J]. Quaternary International,2022,640:96-97.
APA Min Zhao,Hong-Chun Li,Chuan-Chou Shen,Su-Chen Kang,&Chun-Yen Chou.(2022).Corrigendum to “δ18O, δ13C, elemental content and depositional features of a stalagmite from Yelang Cave reflecting climate and vegetation changes since late Pleistocene in central Guizhou, China [Qua.Quaternary International,640,96-97.
MLA Min Zhao,et al."Corrigendum to “δ18O, δ13C, elemental content and depositional features of a stalagmite from Yelang Cave reflecting climate and vegetation changes since late Pleistocene in central Guizhou, China [Qua".Quaternary International 640(2022):96-97.
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