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Evidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO2 in the Taylor Dome, Dome C and DML ice cores

✍ Scribed by Eric Monnin; Eric J Steig; Urs Siegenthaler; Kenji Kawamura; Jakob Schwander; Bernhard Stauffer; Thomas F Stocker; David L Morse; Jean-Marc Barnola; Blandine Bellier; Dominique Raynaud; Hubertus Fischer


Book ID
116451680
Publisher
Elsevier Science
Year
2004
Tongue
English
Weight
409 KB
Volume
224
Category
Article
ISSN
0012-821X

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