Use of δ(18)O(atm) in dating a Tibetan ice core record of Holocene/Late Glacial climate

Ice cores from the northwestern Tibetan Plateau (NWTP) contain long records of regional climate variability, but refrozen meltwater and dust in these cores has hampered development of robust timescales. Here, we introduce an approach to dating the ice via the isotopic composition of atmospheric O(2)...

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Detalles Bibliográficos
Autores principales: Thompson, Lonnie G., Severinghaus, Jeffrey P., Yao, Tandong, Davis, Mary E., Mosley-Thompson, Ellen, Beaudon, Emilie, Sierra-Hernández, M. Roxana, Porter, Stacy E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2022
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9659374/
https://www.ncbi.nlm.nih.gov/pubmed/36322740
http://dx.doi.org/10.1073/pnas.2205545119

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9659374/
https://www.ncbi.nlm.nih.gov/pubmed/36322740
http://dx.doi.org/10.1073/pnas.2205545119

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