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Items: 4

1.

Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years.

Loulergue L, Schilt A, Spahni R, Masson-Delmotte V, Blunier T, Lemieux B, Barnola JM, Raynaud D, Stocker TF, Chappellaz J.

Nature. 2008 May 15;453(7193):383-6. doi: 10.1038/nature06950.

PMID:
18480822
2.

Changing boreal methane sources and constant biomass burning during the last termination.

Fischer H, Behrens M, Bock M, Richter U, Schmitt J, Loulergue L, Chappellaz J, Spahni R, Blunier T, Leuenberger M, Stocker TF.

Nature. 2008 Apr 17;452(7189):864-7. doi: 10.1038/nature06825.

PMID:
18421351
3.

Orbital and millennial Antarctic climate variability over the past 800,000 years.

Jouzel J, Masson-Delmotte V, Cattani O, Dreyfus G, Falourd S, Hoffmann G, Minster B, Nouet J, Barnola JM, Chappellaz J, Fischer H, Gallet JC, Johnsen S, Leuenberger M, Loulergue L, Luethi D, Oerter H, Parrenin F, Raisbeck G, Raynaud D, Schilt A, Schwander J, Selmo E, Souchez R, Spahni R, Stauffer B, Steffensen JP, Stenni B, Stocker TF, Tison JL, Werner M, Wolff EW.

Science. 2007 Aug 10;317(5839):793-6. Epub 2007 Jul 5.

4.

Atmospheric methane and nitrous oxide of the Late Pleistocene from Antarctic ice cores.

Spahni R, Chappellaz J, Stocker TF, Loulergue L, Hausammann G, Kawamura K, Fl├╝ckiger J, Schwander J, Raynaud D, Masson-Delmotte V, Jouzel J.

Science. 2005 Nov 25;310(5752):1317-21.

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