The palaeoenvironmental significance of δ13C of stalagmite BW-1 from Beijing, China during Younger Dryas intervals inferred from the grey level profile-Reference-Cited by-同舟云学术

The palaeoenvironmental significance of δ13C of stalagmite BW-1 from Beijing, China during Younger Dryas intervals inferred from the grey level profile

Published:2013-07-19 Issue:1 Volume:43 Page:243-250
ISSN:0300-9483
Container-title:Boreas
language:en
Short-container-title:Boreas

Author:

Duan Wuhui¹²,Tan Ming¹,Ma Zhibang¹,Cheng Hai³⁴

Affiliation:

1. Key Laboratory of Cenozoic Geology Environment, Institute of Geology and Geophysics; Chinese Academy of Sciences; Beijing 100029 China

2. University of Chinese Academy of Sciences; Beijing 100049 China

3. Institute of Global Environmental Change; Xi'an Jiaotong University; Xi'an 710049 China

4. Department of Earth Sciences; University of Minnesota; Minneapolis MN 55455 USA

Publisher

Wiley

Subject

Geology,Archaeology,Ecology, Evolution, Behavior and Systematics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/bor.12034/fullpdf

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3. High resolution δ18O and δ13C records from an annually laminated Scottish stalagmite and relationship with last millennium climate;Baker;Global and Planetary Change,2011

4. Biomass effects on stalagmite growth and isotope ratios: a 20th century analogue from Wiltshire, England;Baldini;Earth and Planetary Science Letters,2005

5. Temporal and spatial variations in the discharge and dissolved organic carbon of drip waters in Beijing Shihua Cave, China;Ban;Hydrological Processes,2008

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