  The pressure, temperature, and timing (PTt) conditions at which CO2 was
produced during the Himalayan prograde metamorphism have been constrained,
focusing on the most abundant calcsilicate rock type in the Himalaya. A
detailed petrological modeling of a clinopyroxene, scapolite, Kfeldspar,
plagioclase, quartz, calcite calcsilicate rock allowed the identification and
full characterization, for the first time, of different metamorphic reactions
leading to the simultaneous growth of titanite and CO2 production. The results
of thermometric determinations (Zr in Ttn thermometry) and UPb geochronological
analyses suggest that, in the studied lithology, most titanite grains grew
during two nearly consecutive episodes of titanite formation: a nearpeak event
at 730 740 {\deg}C, 10 kbar, 30 26 Ma, and a peak event at 740 765 {\deg}C,
10.5 kbar, 25 20 Ma. Both episodes of titanite growth are correlated with
specific CO2producing reactions and constrain the timing, duration and PT
conditions of the main CO2producing events, as well as the amounts of CO2
produced (1.4 1.8 wt percent of CO2). A firstorder extrapolation of such CO2
amounts to the orogen scale provides metamorphic CO2 fluxes ranging between 1.4
and 19.4 Mt yr; these values are of the same order of magnitude as the
presentday CO2 fluxes degassed from spring waters located along the Main
Central Thrust. We suggest that these metamorphic CO2 fluxes should be
considered in any future attempts of estimating the global budget of non
volcanic carbon fluxes from the lithosphere.
