Late summer metalimnetic oxygen minimum zone in the northern Baltic Sea

• Published in: Journal of marine systems Vol. 80; no. 1; pp. 1 - 7
• Main Authors: Raateoja, M., Kuosa, H., Flinkman, J., Pääkkönen, J.-P., Perttilä, M.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 20.02.2010
• Subjects: Ammonium; Baltic Sea; Biological; Consumption; Decomposition; Gulfs; Hydrography; Marine; Mathematical models; Microorganisms; Oxygen; Respiration; Stations; Thermocline; Thermocline; Oxygen; Ammonium; Decomposition; Baltic Sea; Hydrography
• ISSN: 0924-7963; 1879-1573
• DOI: 10.1016/j.jmarsys.2009.06.005

The frequently observed, but commonly ignored hydrographic characteristic of the Baltic Sea, the oxygen minimum zone (OMiZ) above and within the summertime thermocline, was studied during the 6-yr monitoring programme encompassing the Gulfs of Bothnia and Finland in the northern Baltic Sea. A temperature-anomaly-driven density gradient was found to be a prerequisite for the existence of the OMiZ. We determined the magnitude of the apparently utilized O 2 in the OMiZ by combining graphical analysis and empirical modelling. A sound criterion for distinguishing the cases in which the OMiZ had a biological origin, and not only a hydrodynamic one, was the accompanying ammonium maximum zone (AMaZ). Of a total of 46 stations visited, a density gradient was found at every station, an accompanying OMiZ at 37 stations, and an accompanying AMaZ at 20 stations. This suggests that biological activity is an essential factor in forming the OMiZ. We investigated to what extent the OMiZ was a manifestation of microbial decomposition of autochthonous organic matter, as zooplankton respiration was also a factor. As a study average, ~ 80% of the apparently utilized O 2 was consumed by the microbial decomposition process and ~ 20% of it by mesozooplankton respiration. According to the O 2 quota consumed in the process, the microbial community in the OMiZ of the Gulf of Finland decomposed, on average, 14% of all the organic matter settling from the euphotic zone in the time frame of mid-June to early August. A pronounced allochthonous organic carbon pool in the Gulf of Bothnia hinders a prompt estimation of a corresponding share for that basin.