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Autor:
P. Meister, A. Alexandre, H. Bailey, P. Barker, B. K. Biskaborn, E. Broadman, R. Cartier, B. Chapligin, M. Couapel, J. R. Dean, B. Diekmann, P. Harding, A. C. G. Henderson, A. Hernandez, U. Herzschuh, S. S. Kostrova, J. Lacey, M. J. Leng, A. Lücke, A. W. Mackay, E. K. Magyari, B. Narancic, C. Porchier, G. Rosqvist, A. Shemesh, C. Sonzogni, G. E. A. Swann, F. Sylvestre, H. Meyer
Publikováno v:
Climate of the Past, Vol 20, Pp 363-392 (2024)
Oxygen isotopes in biogenic silica (δ18OBSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy-model comparison in terrestrial environments. The signals of individual records have been attributed to different f
Externí odkaz:
https://doaj.org/article/ca285675242c49c0aaf38f9f97329d6c
