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vol.23 número1LA MALACOFAUNA DE LA ZONA COSTERA DE SANTA MARTA Y PARQUE NACIONAL NATURAL TAYRONA, CARIBE COLOMBIANOCLAVE GRÁFICA PARA LA IDENTIFICACIÓN DE FAMILIAS Y GÉNEROS DE anfípodos DEL SUBORDEN GAMMARIDEA DEL ATLÁNTICO OCCIDENTAL TROPICAL índice de autoresíndice de assuntospesquisa de artigos
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Boletín de Investigaciones Marinas y Costeras - INVEMAR

versão impressa ISSN 0122-9761

Resumo

GOCKE, Klaus  e  HERNANDEZ J., Carlos A.. DETERMINACIÓN COMPARATIVA DE LA PRODUCCIÓN PRIMARIA CON LAS TÉCNICAS DE 14C Y O2 EN AGUAS SALOBRES CON DIFERENTES GRADOS DE EUTROFICACIÓN. Bol. Invest. Mar. Cost. [online]. 1994, vol.23, n.1, pp.45-58. ISSN 0122-9761.

The primary productivity of phytoplankton was determined in the mesotrophic Kiel Bight (KB), the eutrophic Kiel Fjord (KF) and the hypertrophic Schlei Fjord using the 14C-technique and the O2-method. Results of these measurements were compared. These brackish areas of the western-most part of the Baltic Sea differ markedly in primary productivity (PP). If the depth of maximum productivity alone is considered, the PP, on a volumetric basis, of the Schlei was 9 times higher than in the Kiel Fjord and more than 40 times that of the Kiel Bight. On an area basis the differences were much smaller since the compensation depth in the Schlei was found at no more than 0.8 m, whereas in the Kiel Bight it was 5.5 m and 5.2 m in the Kiel Fjord. In agreement with theoretical considerations, the PP determined with the 14C-technique (14C-PP) was larger than the net productivity (NP) and smaller than the gross productivity (GP), both determined with the O2-method using a photosynthetic quotient of 1.2. On average, in the Kiel Fjord the NP was 9 % smaller and the GP 36 % larger than the 14C-PP. in the Kiel Bight the NP was 40 % smaller and the GP 72 % larger. However, the relation NP<14CPP<GP was found only in the Kiel Bight and -Fjord, whereas in the polyproductive Schlei the 14C-PP was larger than both the NP and GP (32 % larger than the NP and 7 % larger than the GP). This deviation from theoretical values may be due, in part, to a senescent phytoplankton, which may have had a PQ smaller than 1.2.

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