(Table 1) Heat flow data in the western Black Sea

Results of heat flow measurements are presented. On the basis of new data on structure of the sedimentary sequence, corrections are introduced that take account of effect of sedimentation. Diagrammatic maps of distribution of observed and deep-seated heat flow have been constructed. A hypothesis is offered that the regional zone of anomalously high heat-flow values on the northern continental slope has been controlled by processes of subsidence of an oceanic plate beneath its continental counterpart.

Bottom invertebrates and madreporarian corals in the Canary upwelling area

Composition and distribution of bottom fauna, especially scleractinian and gorgonarian corals, collected in the area of the Canary upwelling are discussed. Five species of scleractinian corals and one gorgonarian coral were found. Dasmosmillia lymani, Flabellum angulare, Leptopsammia chevalieri, and Bebryce mollis are new in the investigated area. It is shown that bottom fauna of the Canary upwelling area could be regarded as intermediate between the ordinary shallow-water community and extremely oligomixed fauna of intensive upwellings.