Methane dynamics in the coastal – Continental shelf transition zone of the Gulf of Cadiz

The concentration of CH in water was measured along five transects in the Gulf of Cadiz (Trafalgar, Sancti Petri, Guadalquivir, Tinto - Odiel and Guadiana) during four cruises throughout the months of March, June, September and December 2016. For two of the cruises water overlying three mud volcanoes situated in the Gulf of Cadiz were also sampled (San Petersburgo, 860 m; Pipoca, 460 m; and Anastasya, 500 m. In addition, the stable carbon isotopic compositions of dissolved CH (δC) were measured in the study area in June and December 2016. The mean CH value for the whole water column was 10.5 ± 4.3 nmol L, with large spatial and temporal variations. The highest values were found in June 2016 and the lowest in March 2016. In surface waters, the mean dissolved methane concentration was of 9.6 ± 2.6 nmol L. In most of the sampling area, high concentrations of CH were found in subsurface waters at depths close to the thermocline and at the coastal stations. The highest concentrations were obtained from the bottom waters above the Anastasya mud volcano (125 nmol L). The stable carbon isotope compositions ranged between - 29.2 and - 58.4‰, and the least negative values were associated with the highest CH concentrations in samples from above the mud volcanoes, related to thermogenic values. The sea-air fluxes of CH ranged from 12.4 to 37.7 μmol m d, showing that the study area acts as a source of CH to the atmosphere.A. Sierra was financed by the Spanish Ministry of Education with a FPU fellowship (FPU2014-04048) and M.D. Jiménez-López was financed by the University of Cádiz with a FPI fellowship (FPI-UCA). We thank the crews of the R/V's Angeles Alvariño and Ramon Margalef for their assistance during field work. This study was supported by the Spanish CICYT (Spanish Program for Science and Technology) under contract CTM2014-59244-C3-1-R