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Autor:
Sophie Hage, Brian W. Romans, Thomas G. E. Peploe, Miquel Poyatos-Moré, Omid Haeri Ardakani, Daniel Bell, Rebecca G. Englert, Sebastian A. Kaempfe-Droguett, Paul R. Nesbit, Georgia Sherstan, Dane P. Synnott, Stephen M. Hubbard
Publikováno v:
Nature Geoscience (1752-0894) (Nature), 2022-11, Vol. 15, N. 11, P. 919-924
Burial of terrestrial organic carbon in marine sediments can draw down atmospheric CO2 levels on Earth over geologic timescales (≥105 yr). The largest sinks of organic carbon burial in present-day oceans lie in deltas, which are composed of three-d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1fb5996b7066fad317732072b1f969f6
https://archimer.ifremer.fr/doc/00799/91125/
https://archimer.ifremer.fr/doc/00799/91125/
