1) d13C-CO2 and d15N-N2 isotope ratios in EDC, EDML and Talos Dome ice cores measured by sublimation extraction
Cobertura |
MINIMUM DEPTH, ice/snow: 192.200 m * MAXIMUM DEPTH, ice/snow: 1853.835 m |
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Data(s) |
30/03/2016
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Formato |
text/tab-separated-values, 1114 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.859209 doi:10.1594/PANGAEA.859209 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.859181 Eggleston, Sarah; Schmitt, Jochen; Bereiter, Bernhard; Schneider, Robert; Fischer, Hubertus (2016): Evolution of the stable carbon isotope composition of atmospheric CO2 over the last glacial cycle. Paleoceanography, 31, n/a-n/a, doi:10.1002/2015PA002874 Schneider, Robert (2011): Quantifying past changes of the global carbon cycle based on d13C02 measurements in Antarctic ice cores. Inauguraldissertation of the Faculty for Philosophical and Natural Science of the University of Bern; Department of Climate and Environmental Physics Physics Department, University of Bern, 231 pp, http://baselbern.swissbib.ch/Record/268240108 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #Core; corrected; delta 13C, carbon dioxide, atmospheric; delta 13C, standard error; delta 15N, gas; delta 15N, standard deviation; DEPTH, ice/snow; EPICA; European Project for Ice Coring in Antarctica; Gas age; Quality flag; Reference/source; Replicates; TALDICE; Talos Dome Ice Core |
Tipo |
Dataset |