The Marine Carbonate System at Maluku and Sulawesi Seas

Abstract

Maluku and Sulawesi Sea s are parts of Indonesian Large Marine Ecosystem in the east area which has an important role for Indonesian fisheries activities. Those areas are facing the climate change phenomena that could change their marine ecosystem quality. Marine carbonate system is very important for controlling the circulation of CO 2 between the atmosphere and the ocean as well as regulating the pH value of waters. We conducted in situ measurement of marine carbonate system parameters (pH, Total Alkalinity, Total CO 2 (TCO 2 ) and pCO 2 ) during IJEP cruise on September 2016 to analyses spatial variations of the marine carbonate system in the Northwest Monsoon period. The results of marine carbonate system showed that in general Maluku and Sulawesi Sea s are under super saturation of CO 2 or acts as source of CO 2 which have range value of sea surface partial of CO 2 (pCO 2 ) between 280 – 500 µatm. Spatial distribution of sea surface pH values measured with optical sensor at study sites showed varied between 8,03 – 8,15. Measurement results of Total alkalinity (TA) by using titration method varied between 2300 – 2400 µmol/Kg meanwhile range value of TCO 2 was 2300 – 2500 µmol/Kg at surface waterand it’s increased through the deep water with the range value of TCO 2 was 2500 – 2800 µmol/Kg at deeper layer of water.Characteristic of marine carbonate system between Maluku and Sulawesi Sea s was different in the Southeast monsoon period indicates complex marine biogeochemistry processes influences those system .