A Spatial Analysis of Fish Farming in the Context of ICZM in the Bay of Izmir-Turkey

Cage fish farming is one of the fastest growing food industries, both worldwide and in Turkey. There are growing concerns about the manner of resolving the competing claims for the use of limited coastline and water body space. Matters connected with the siting of fish farming increase the need for the integrated coastal zone planning of aquaculture. This should be undertaken in collusion with other coastal stakeholders and with the cooperation of the government ministries that promote and regulate aquaculture development. In this study the integration and coexistence of fish farms is evaluated in the context of other activities in Izmir Bay. This study shows how different terrestrial and marine activities interact with each other, and that certain areas are subject to layers of multiple usages. One of the major sea users of the Bay, for example, is the fishery sector, which utilizes 850.4 km² of a total surface area of Izmir's Bay of 960.4 km². This overlaps with the 113.4 km² that are used by marine transportation. Military zones encompass 63.1 km² and fish farming utilizes only 1.23 km². This study uses Geographic Information Systems (GIS) to build a spatial database that analyzes conflicting claims for integrating fish farming with other claimants. Clearly planned and properly managed fish farming development should be undertaken within a broader framework of integrated coastal zone management.     

Circulation, hydrographic and nutrient characteristics of the Cilician Basin, Northeastern Mediterranean Sea

The water mass, circulation and chemical properties of the Cilician Basin, the northeastern Levantine Sea, are described on the basis of three hydrographic cruises performed during May 1997 (spring), July 1998 (summer) and October 2003 (autumn). The hydrographic data reveal the presence of Levantine Surface Water (LSW) and Modified Atlantic Water (MAW) within the upper 90 m layer, Levantine Intermediate Water (LIW) between 90 and 250 m, and Transitional Mediterranean Water (TMW) further below. The temporal variability of the circulation system is manifested by a change in shape, size and intensity of eddies as well as the pathways of the Lattakia Basin coastal current system. The nutrient concentrations varied between nitrate + nitrite = 0.16–0.31 μM, phosphate = 0.02–0.03 μM and silicate = 0.95–1.2 μM for the surface layer during sampling periods. Dissolved nutrient concentrations in the Transitional Mediterranean Water were: 2.1–5.3 μM for NO₃ + NO₂, 0.10–0.21 μM for PO₄ and 5.7–10 μM for Si. The molar ratios of nitrate to phosphate in the water column range between 5 and 20 in the surface layer and reach up to a value of 45 at the top of the nutricline at the depths of 29.05 kg/m³ isopycnal surface for most of the year. Below the nutricline the N / P ratios retain the values around 24–28.