The abundance, distribution, and isotopic composition of Hydrogen in the Moon as revealed by basaltic lunar samples: Implications for the volatile inventory of the Moon

In this study we have measured the OH contents and D/H ratios in apatite grains in lunar basalts. These new data considerably expand the limited dataset published so far. The data presented in this study also show that there is a major difference between high-and low-Ti mare basalts in terms of their OH and D/H systematics. Apatites in high-Ti basaltic samples display a relatively restricted range in OH contents (similar to 1500-3000 ppm) with large delta D variations (similar to 600-1000 parts per thousand) whereas apatites in low-Ti Apollo basalts and lunar meteorites display a comparatively larger range in OH contents (similar to 500-15000 ppm), each sample displaying relatively restricted variations in their D/H ratios. Analyses of apatites in basaltic meteorites Miller Range 05035 and LaPaz Icefield 04841 substantially expand the lower bound for delta D values measured in apatites from Apollo mare basalts, down to delta D values of similar to 100 parts per thousand. In these meteorites, high resolution mapping of the distribution of secondary ions of H and C was used to avoid cracks and hotspots. Together with mixing calculations for terrestrial contamination, this analytical protocol ensured that most of the values reported for MIL 05035 and LAP 04841 correspond to their actual lunar signatures. We interpret the large variations of apatite delta D values in mare basalts between similar to 200 parts per thousand and 1000 parts per thousand as a result of different amounts of degassing of H-bearing species initially dissolved in the basaltic parental melts. Indeed, the average dD values measured in different low-Ti basalts are consistent with similar to 85-99% degassing of H as H-2, starting from a delta D value of 100 parts per thousand. Degassing of H-bearing species essentially as H-2 was favoured by the reduced nature of lunar magmas. In low-Ti mare basalts, apatite crystallisation occurred after degassing of the H-bearing species and the OH variations reflect different degrees of fractional crystallisation. In high-Ti mare basalts, large delta D variations with relatively restricted range in OH contents imply that apatite crystallisation and degassing of H-bearing species were mostly coeval. Geochemical modelling integrating corrections for degassing and fractional crystallisation suggests that the mantle source regions of the different low-Ti mare basalts could have contained similar to 5-50 ppm H (equivalent to similar to 45-450 ppm H2O), which are similar to the estimated range of similar to 60-350 ppm water for the Earth's upper mantle. Finally, the H isotopic composition of pre-degassed lunar hydrogen in mare basalts is consistent with a CI-chondrite-type value of similar to 100 parts per thousand, which is consistent with the increasing evidence suggesting that the Earth, Mars and the Moon might have accreted similar water of chondritic origin. (C) 2013 Elsevier Ltd. All rights reserved.