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Datasets of project "Talos Dome Ice Core"

Mostrando recursos 1 - 6 de 6

  1. delta 18O measured on ice core TALDICE on AICC2012 chronology

    Bazin, Lucie; Landais, Amaelle; Lemieux-Dudon, Bénédicte; Toyé Mahamadou Kele, H; Veres, Daniel; Parrenin, Frédéric; Martinerie, P; Ritz, Catherine; Capron, Emilie; Lipenkov, Vladimir Y; Loutre, M-F; Raynaud, Dominique; Vinther, Bo M; Svensson, A; Rasmussen, Sune O; Severi, Mirko; Blunier, Thomas; Leuenberger, Markus; Fischer, Hubertus; Masson-Delmotte, Valerie; Chappellaz, Jérôme A; Wolff, Eric W

  2. Methane measured on ice core TALDICE on AICC2012 chronology

    Bazin, Lucie; Landais, Amaelle; Lemieux-Dudon, Bénédicte; Toyé Mahamadou Kele, H; Veres, Daniel; Parrenin, Frédéric; Martinerie, P; Ritz, Catherine; Capron, Emilie; Lipenkov, Vladimir Y; Loutre, M-F; Raynaud, Dominique; Vinther, Bo M; Svensson, A; Rasmussen, Sune O; Severi, Mirko; Blunier, Thomas; Leuenberger, Markus; Fischer, Hubertus; Masson-Delmotte, Valerie; Chappellaz, Jérôme A; Wolff, Eric W

  3. AICC2012 chronology for ice core TALDICE

    Bazin, Lucie; Landais, Amaelle; Lemieux-Dudon, Bénédicte; Toyé Mahamadou Kele, H; Veres, Daniel; Parrenin, Frédéric; Martinerie, P; Ritz, Catherine; Capron, Emilie; Lipenkov, Vladimir Y; Loutre, M-F; Raynaud, Dominique; Vinther, Bo M; Svensson, A; Rasmussen, Sune O; Severi, Mirko; Blunier, Thomas; Leuenberger, Markus; Fischer, Hubertus; Masson-Delmotte, Valerie; Chappellaz, Jérôme A; Wolff, Eric W

  4. Iron (Fe) concentrations and fluxes in TALDICE ice core 0.6 to 314 ky BP

    Vallelonga, Paul; Barbante, Carlo; Cozzi, Giulio; Gabrieli, J; Schüpbach, Simon; Spolaor, Andrea; Turetta, C
    Atmospheric fluxes of iron (Fe) over the past 200 kyr are reported for the coastal Antarctic Talos Dome ice core, based on acid leachable Fe concentrations. Fluxes of Fe to Talos Dome were consistently greater than those at Dome C, with the greatest difference observed during interglacial climates. We observe different Fe flux trends at Dome C and Talos Dome during the deglaciation and early Holocene, attributed to a combination of deglacial activation of dust sources local to Talos Dome and the reorganisation of atmospheric transport pathways with the retreat of the Ross Sea ice shelf. This supports similar findings...

  5. Stable carbon isotope ratio of atmospheric CO2 of ice core Talos Dome, Bern sublimation

    Schmitt, Jochen; Schneider, Robert; Elsig, Joachim; Leuenberger, Daiana; Lourantou, Anna; Chappellaz, Jérôme A; Köhler, Peter; Joos, Fortunat; Stocker, Thomas F; Leuenberger, Markus; Fischer, Hubertus

  6. Visual stratigraphy of the TALDICE ice core with a linescanner

    Kipfstuhl, Sepp

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