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pro vyhledávání: '"J, Roadt"'
Publikováno v:
Geobiology. 9:313-320
An anoxic, sulfidic ocean that may have existed during the Proterozoic Eon (0.54–2.4 Ga) would have had limited trace metal abundances because of the low solubility of metal sulfides. The lack of copper, in particular, could have had a significant
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b736076d66e06261b0d32dee6dd2c6be
https://doi.org/10.1111/j.1472-4669.2011.00286.x
https://doi.org/10.1111/j.1472-4669.2011.00286.x
Publikováno v:
Geobiology. 9(4)
An anoxic, sulfidic ocean that may have existed during the Proterozoic Eon (0.54-2.4 Ga) would have had limited trace metal abundances because of the low solubility of metal sulfides. The lack of copper, in particular, could have had a significant im
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::9acd0a0de50f0d2f2738bde26fa2ffb4
https://pubmed.ncbi.nlm.nih.gov/21682839
https://pubmed.ncbi.nlm.nih.gov/21682839
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