Fig. 5: Mo isotope records in shales and abundance distributions of banded iron formations and sedimentary Mn deposits through geological time. | Communications Earth & Environment

Fig. 5: Mo isotope records in shales and abundance distributions of banded iron formations and sedimentary Mn deposits through geological time.

From: Molybdenum isotope fractionations between ferromanganese oxides and seawater influenced ancient sedimentary isotopic signatures

Fig. 5: Mo isotope records in shales and abundance distributions of banded iron formations and sedimentary Mn deposits through geological time.The alternative text for this image may have been generated using AI.

a Marine sedimentary records of Mo isotopes throughout geological time. b Temporal changes in distributions of banded iron formations and sedimentary Mn deposits. In a the dashed line in represents the δ98Mo values of modern seawater and average rivers10. Red arrows denote the increased occurrence of positive and negative δ98Mo signatures following the enhanced marine Mn cycle. The δ98Mo data of shales are modified from ref. 14. The distributions of banded iron formations and sedimentary Mn deposits are modified from refs. 45,46.

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