A last deglacial climate dataset comprising ice core data, marine data, and stalagmite data

Zhi Liu,Shaopeng Huang,Zhangdong Jin

doi:10.1016/j.dib.2018.11.008

Zhi Liu, Shaopeng Huang + Show 1 more

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https://doi.org/10.1016/j.dib.2018.11.008

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Abstract

In this data article, a dataset of paleoclimatic records ranging from 22 to 9 thousand years before present is reported, which is related to the research article entitled “Breakpoint lead-lag analysis of the last deglacial climate change and atmospheric CO2 concentration on global and hemispheric scales” published in the journal of Quaternary International by Liu et al. (2018). In the dataset, 4 δ18O records derived from Greenlandic ice cores, 2 δD records and 7 δ18O records derived from Antarctic ice cores, 32 UK’37 records and 26 Mg/Ca records derived from marine deposits, and 17 δ18O records derived from cave stalagmites were collected and collated. General and statistical characteristics of these 88 proxy records are showed here. All of the data are stored in separate Microsoft Excel spreadsheets that are available for researchers.

Highlights

For data article “A last deglacial climate dataset comprising ice core data, marine data, and stalagmite data” by Zhi Liu, Shaopeng Huang, and Zhangdong Jin (DIB-D-18-02152)
We confirm that there are no conflicts of interest associated with this publication and there has been no significant financial support for this work that could have influenced its outcome
We confirm that we have given due consideration to the protection of intellectual property associated with this work and that there are no impediments to publication, including the timing of publication, with respect to intellectual property

Summary

Introduction

For data article “A last deglacial climate dataset comprising ice core data, marine data, and stalagmite data” by Zhi Liu, Shaopeng Huang, and Zhangdong Jin (DIB-D-18-02152). We confirm that there are no conflicts of interest associated with this publication and there has been no significant financial support for this work that could have influenced its outcome.

Results

Conclusion