Natural mass-dependent variations in the isotopic composition of molybdenum

• Published in: Earth and planetary science letters 2001-12, Vol.193 (3), p.447-457
• Main Authors: Barling, J, Arnold, G.L, Anbar, A.D
• Format: Article
• Language: English
• Subjects: anaerobic environment; isotope fractionation; Marine; molybdenum; paleoenvironment; stable isotopes
• ISSN: 0012-821X; 1385-013X
• DOI: 10.1016/S0012-821X(01)00514-3

We present the first observations of natural mass-dependent fractionation of the isotopic composition of molybdenum (Mo), using multi-collector inductively coupled plasma mass spectrometry. Variations in the isotopic composition of Mo are reported as δ 97/95Mo (=(( 97Mo/ 95Mo) sample/( 97Mo/ 95Mo) standard−1)×1000‰). External analytical precision of δ 97/95Mo is 1‰ between sediments deposited under anoxic conditions (δ 97/95Mo=+1.02 to +1.52‰ relative to our in-house standard) and ferromanganese nodules (δ 97/95Mo=−0.63 to −0.42‰). δ 97/95Mo of Pacific Ocean seawater (δ 97/95Mo=+1.48‰) lies within the range of values for anoxic sediments, closest to modern Black Sea anoxic sediments. Molybdenites from continental ore deposits have intermediate δ 97/95Mo ranging from −0.26 to +0.09‰. Variations in the abundances of 92Mo, 95Mo, 96Mo, 97Mo and 98Mo are consistent with mass-dependent fractionation. A sporadic unidentified interference occurs at mass 94 and 100Mo is not measured. We hypothesize that the δ 97/95Mo offset between anoxic sediments and ferromanganese nodules results from Mo isotope fractionation during inefficient scavenging of Mo from seawater by Mn oxides under oxic conditions. The similarity in δ 97/95Mo of anoxic sediments and seawater is consistent with the very efficient removal of Mo from seawater under anoxic conditions in the presence of H 2S. The data can be interpreted in terms of a steady-state mass balance between the Mo flux into the oceans from the continents and the Mo flux out of the oceans into oxic and anoxic sediments. Such an interpretation is quantitatively consistent with existing estimates of the removal fluxes of Mo to anoxic and oxic sediments. These findings suggest that δ 97/95Mo in seawater may co-vary with changes in the relative proportions of anoxic and oxic sedimentation in the oceans, and that this variation may be recorded in δ 97/95Mo of anoxic sediments. Hence, the Mo isotope system may be useful in paleoredox investigations.