The annual cycle of phytoplankton primary production and hydrography in the Disko Bugt area, West Greenland

The distribution and size of phytoplankton production and biomass in relation to physical and chemical parameters in the upper 50 m at Godhavn and in Kangikerdlak in the inner part of Disko Fjord was investigated through 2½ years (1973-75). Some data from other parts of Disko Bugt are presented. In...

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Bibliographic Details
Main Author: Andersen, Ole G. Norden
Format: Article in Journal/Newspaper
Language:English
Published: Danish Polar Center/Museum Tusculanum Press 1981
Subjects:
Online Access:https://tidsskrift.dk/meddrgroenland_biosci/article/view/142187
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Summary:The distribution and size of phytoplankton production and biomass in relation to physical and chemical parameters in the upper 50 m at Godhavn and in Kangikerdlak in the inner part of Disko Fjord was investigated through 2½ years (1973-75). Some data from other parts of Disko Bugt are presented. In both locations the hydrography alternates between an unstable winter situation with isothermal (-1.75°C) and isohaline (33.5-34.0‰) conditions throughout, and a highly stable summer situation when dilution and heating, especially of the upper 20- 30 m, raise the temperature at the surface to 9.9°C and at 50 m to 3.8°C at Godhavn, and to 12°C and 3.5°C respectively in Kangikerdlak. Salinities drop correspondingly to 30.6‰ in Kangikerdlak. The 1% depth for green light is greatly reduced beneath ice and snow. During the ice free period at Godhavn it varies from 12 m during the spring phytoplankton bloom to more than 60 m from Oct. through the winter. In Kangikerdlak the 1% depth reaches only 40 m in winter, and outflowing turbid fresh water creates I% depths of as little as 4-5 m in June-Aug. At Godhavn NO3-N reaches highs of 10.05 μgat /liter and 10.15 μgat /liter at 0 and 50 m respectively in winter, whereas during the summer, depletion to less than 0.01 μgat /liter occurs in the upper 40 m and to 1.0 μgat / liter at 50 m. PO4-P is similarly reduced from 0.8 μgat/liter and 1.1 μgat/liter to less than 0.01 μgat / liter in the upper 20 m and to 0.21 μgat /liter at 50 m. The N:P ratio drops from 13 to less than 0.01 in the upper 30 m and to 1.0 at 50 m. In Kangikerdlak depletion of NO3-N is similar to conditions at Godhavn, whereas PO4-P reaches a low of 0.1 μgat/liter only, while in mid summer it reaches 1.88 μgat /liter at the surface, giving an N:P ratio which is below 0.1 in the upper 5 m only. At Godhavn primary production is about 90 gC • m-2 • yr-1 (75-104 g) with a maximum of about 5 .5 gC • m-3 • yr-1 at 5- 10 m, whereas in Kangikerdlak production was concentrated near the surface with about 6.0 gC • m-3 • ...