DSpace

Digital.CSIC > Recursos Naturales > Instituto de Ciencias del Mar (ICM) > (ICM) Artículos >

Share

EndNote

Impact

Links

Restricted Access item, embargoed access until 01/01/2016 Phytoplankton growth and microzooplankton grazing along a sub-Arctic fjord (Godthåbsfjord, west Greenland)

Authors:Calbet, Albert
Riisgaard, Karen
Saiz, Enric
Zamora, Sara
Stedmon, Colin
Gissel Nielsen, Torkel
Keywords:West Greenland coast, Sub-Arctic fjord, Plankton Community Structure, Microzooplankton, Grazing
Issue Date:Dec-2011
Publisher:Inter Research
Citation:Marine Ecology Progress Series 442: 11-22 (2011)
Abstract:We evaluated the role of microzooplankton (sensu latto, grazers <500 µm) in determining the fate of phytoplankton production (PP) along a glacier-to-open sea transect in the Greenland subarctic fjord, Godthåbfjord. Based on the distribution of size fractionated chlorophyll a (chl a) concentrations we established 4 zones: (1) Fyllas Bank, characterized by deep chl a maxima (ca. 30 to 40 m) consisting of large cells, (2) the mouth and main branch of the fjord, where phytoplankton was relatively homogeneously distributed in the upper 30 m layer, (3) inner waters influenced by glacial melt water and upwelling, with high chl a concentrations (up to 12 µg l−1) in the >10 µm fraction within a narrow (2 m) subsurface layer, and (4) the Kapisigdlit branch of the fjord, ice-free, and characterized with a thick and deep chl a maximum layer. Overall, microzooplankton grazing impact on primary production was variable and seldom significant in the Fyllas Bank and mouth of the fjord, quite intensive (up to >100% potential PP consumed daily) in the middle part of the main and Kapisigdlit branches of the fjord, and rather low and unable to control the fast growing phytoplankton population inhabiting the nutrient rich waters in the upwelling area in the vicinity of the glacier. Most of the grazing impact was on the <10 µm phytoplankton fraction, and the major grazers of the system seem to be >20 µm microzooplankton, as deducted from additional dilution experiments removing this size fraction. Overall, little or no export of phytoplankton out of the fjord to the Fyllas Bank can be determined from our data.
Description:12 pages, 7 figures, 4 tables.
Publisher version (URL):http://dx.doi.org/10.3354/meps09343
URI:http://hdl.handle.net/10261/45189
ISSN:0171-8630
E-ISSNmetadata.dc.identifier.doi = DOI:1616-1599
???metadata.dc.identifier.doi???:10.3354/meps09343
Appears in Collections:(ICM) Artículos

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.