Helium, inorganic and organic carbon isotopes of fluids and gases across the Costa Rica convergent margin

In 2017, fluid and gas samples were collected across the Costa Rican Arc. He and Ne isotopes, C isotopes as well as total organic and inorganic carbon concentrations were measured. The samples (n = 24) from 2017 are accompanied by (n = 17) samples collected in 2008, 2010 and 2012. He-isotopes ranged from arc-like (6.8 R-A) to crustal (0.5 R-A). Measured dissolved inorganic carbon (DIC) delta C-13(VPDB) values varied from 3.55 to -21.57%, with dissolved organic carbon (DOC) following the trends of DIC. Gas phase CO2 only occurs within similar to 20 km of the arc; delta C-13(VPDB) values varied from -0.84 to -5.23%. Onsite, pH, conductivity, temperature and dissolved oxygen (DO) were measured; pH ranged from 0.9-10.0, conductivity from 200-91,900 mu S/cm, temperatures from 23-89 degrees C and DO from 2-84%. Data were used to develop a model which suggests that similar to 91 +/- 4.0% of carbon released from the slab/mantle beneath the Costa Rican forearc is sequestered within the crust by calcite deposition with an additional 3.3 +/- 1.3% incorporated into autotrophic biomass.