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Global Change Abstracts The Swiss Contribution - SCNAT

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<strong>Global</strong> <strong>Change</strong> <strong>Abstracts</strong> – <strong>The</strong> <strong>Swiss</strong> <strong>Contribution</strong> | Short List of all <strong>Abstracts</strong><br />

1. Flaje-Kiefern (Krusne Hory Mountains): Late Glacial and Holocene vegetation development<br />

(08.1-336)<br />

Jankovska V, Kunes P, van der Knaap W O<br />

Microgram level radiocarbon (C-14) determination on carbonaceous particles in ice (08.1-337)<br />

Jenk T M, Szidat S, Schwikowski M, Gäggeler H W, Wacker L, Synal H A, Saurer M<br />

Orbital and millennial Antarctic climate variability over the past 800,000 years (08.1-338)<br />

Jouzel J, Masson Delmotte V, Cattani O, Dreyfus G, Falourd S, Hoffmann G, Minster B, Nouet J, Barnola J M,<br />

Chappellaz J, Fischer H, Gallet J C, Johnsen S, Leuenberger M, Loulergue L, Lüthi D, Oerter H, Parrenin F, Raisbeck<br />

G, Raynaud D, Schilt A, Schwander J, Selmo E, Souchez R, Spahni R, Stauffer B, Steffensen J P, Stenni B, Stocker T<br />

F, Tison J L, Werner M, Wolff E W<br />

Applying SAR-IRSL methodology for dating fine-grained sediments from lake El’gygytgyn, northeastern<br />

Siberia (08.1-339)<br />

Juschus O, Preusser F, Melles M, Radtke U<br />

Unfractionated excess air: <strong>The</strong> result of incomplete dissolution of entrapped air? (08.1-340)<br />

Klump S, Cirpka O A, Kipfer R<br />

Excess air as a potential tracer for paleohydrological conditions (08.1-341)<br />

Klump S, Grundl T, Purtschert R, Kipfer R<br />

Bedrock landsliding, river incision, and transience of geomorphic hillslope-channel coupling:<br />

Evidence from inner gorges in the <strong>Swiss</strong> Alps (08.1-342)<br />

Korup O, Schlunegger F<br />

Millenial scale variations of the isotopic composition of atmospheric oxygen over Marine Isotopic<br />

Stage 4 (08.1-343)<br />

Landais A, Masson Delmotte V, Combourieu Nebout N, Jouzel J, Blunier T, Leuenberger M, Dahl Jensen D, Johnsen<br />

S<br />

Ages for the Big Stone Moraine and the oldest beaches of glacial Lake Agassiz: Implications for deglaciation<br />

chronology (08.1-344)<br />

Lepper K, Fisher T G, Hajdas I, Lowell T V<br />

Variable Be-10 fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?<br />

(08.1-345)<br />

Ljung K, Bjorck S, Muscheler R, Beer J, Kubik P W<br />

Characterizing carbon isotopic variability in Sphagnum (08.1-346)<br />

Loader N J, Mccarroll D, van der Knaap W O, Robertson I, Gagen M<br />

Detailed record of the mid-Oxfordian (Late Jurassic) positive carbon- isotope excursion in two<br />

hemipelagic sections (France and Switzerland): A plate tectonic trigger? (08.1-347)<br />

Louis Schmid B, Rais P, Bernasconi S M, Pellenard P, Collin P Y, Weissert H<br />

Impact of methane seeps on the local carbon-isotope record: a case study from a Late Jurassic<br />

hemipelagic section (08.1-348)<br />

Louis Schmid B, Rais P, Logvinovich D, Bernasconi S M, Weissert H<br />

Plate tectonic trigger of changes in pCO(2) and climate in the Oxfordian (Late Jurassic): Carbon isotope<br />

and modeling evidence (08.1-349)<br />

Louis Schmid B, Rais P, Schäffer P, Bernasconi S M, Weissert H<br />

New constraints on the gas age-ice age difference along the EPICA ice cores, 0-50 kyr (08.1-350)<br />

Loulergue L, Parrenin F, Blunier T, Barnola J M, Spahni R, Schilt A, Raisbeck G, Chappellaz J<br />

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