Atmospheric methane variability through the Last Glacial Maximum and deglaciation mainly controlled by tropical sources
Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
Originalsprog | Engelsk |
---|---|
Tidsskrift | Nature Geoscience |
Vol/bind | 16 |
Udgave nummer | 12 |
Sider (fra-til) | 1174-1180 |
Antal sider | 7 |
ISSN | 1752-0894 |
DOI | |
Status | Udgivet - 27 nov. 2023 |
Bibliografisk note
Funding Information:
This work was supported by the US National Science Foundation (NSF) awards 1702920 (C.B., K.M.), 2102944 (C.B., K.M.) and 0806414 (E.B., C.B., J.R., J.E). The University of Bern gratefully acknowledges financial support by the Swiss National Science Foundation (no. 200020_172506: M.M., J.S., H.F. and 200020B_200328: M.M., J.S., H.F.). We thank the NSF Ice Core Facility (NICF) and the University of Copenhagen for their curation and preparation of the WD/GISP2 and NEEM ice-core samples used in this study, respectively. We also thank M. L. Kalk for his assistance in methane data measurement at Oregon State University.
Funding Information:
This work was supported by the US National Science Foundation (NSF) awards 1702920 (C.B., K.M.), 2102944 (C.B., K.M.) and 0806414 (E.B., C.B., J.R., J.E). The University of Bern gratefully acknowledges financial support by the Swiss National Science Foundation (no. 200020_172506: M.M., J.S., H.F. and 200020B_200328: M.M., J.S., H.F.). We thank the NSF Ice Core Facility (NICF) and the University of Copenhagen for their curation and preparation of the WD/GISP2 and NEEM ice-core samples used in this study, respectively. We also thank M. L. Kalk for his assistance in methane data measurement at Oregon State University.
Publisher Copyright:
© 2023, The Author(s), under exclusive licence to Springer Nature Limited.
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