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pro vyhledávání: '"J. G. M. Crumpton-Banks"'
Publikováno v:
Biogeosciences, Vol 19, Pp 5633-5644 (2022)
Recent advances in geochemical techniques mean that several robust proxies now exist to determine the past carbonate chemistry of the oceans. Foraminiferal δ11B and alkenone carbon isotopes allow us to reconstruct sea-surface pH and pCO2, respective
Externí odkaz:
https://doaj.org/article/36420020220246cdafdd22d199aa3e36
