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  • 1995-1999  (3)
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  • 1
    Publication Date: 2020-06-22
    Description: The development and decline of a phytoplankton spring bloom dominated by the prymnesiophyte Phaeocystis pouchetii were studied in Balsfjord, northern Norway between 30 March and 27 May 1992. At a fixed station, the concentration and composition of suspended particulate matter was monitored and compared to the particulate matter collected in sediment traps at six different depths. Direct sedimentation of phytoplankton contributed a minor fraction to particle flux and was confined to a few diatom genera. No evidence was found for pronounced aggregation of Phaeocystis colonies during bloom decline or direct sedimentation of either Phaeocystis colonies or single cells, Particle flux was dominated by faecal-pellet sedimentation during most of the study period, suggesting zooplankton grazing to be a main loss factor. Despite an abrupt decrease in faecal-pellet sedimentation after the decline of the bloom, particulate-carbon sedimentation rates remained high. High post-bloom sedimentation rates were characterized by elevated C/N and C/Chl a ratios of largely amorphous sedimented material. Post-bloom sedimentation coincided with a decrease in transparent exopolymeric particles (TEP) in the surface layer, suggesting that this change resulted from aggregation and sedimentation of carbon-rich exopolymeric material accumulated in the surface layer in the course of the bloom. While organic-carbon accumulation indicates the significance of disintegration of Phaeocystis colonies, post-bloom mucilage sedimentation could be a secondary pathway for the vertical flux of Phaeocystis-derived organic matter.
    Type: Article , PeerReviewed
    Format: text
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  • 2
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 3
    Publication Date: 2019-07-17
    Description: The frequent formation of large blooms makes the cosmopolitan colony forming Haptophycea Phaeocystis an important primary producer in the world oceans. Despite frequent and massive occurrences of such blooms, the fate of the biomass built by Phaeocystis is largely unknown, partly because of its lack of mineral compounds, which hamperes microscopic recognition of detrital, Phaeocystis-derived material. In order to identify Phaeocystis-derived detrital matter, it is necessary to use algal-specific chemical tracers which remain longer intact than the structural integrity of Phaeocystis cells.As part of a joint project on the fate of phytoplankton in the Balsfjord in Northern Norway, the sedimentation of Phaeocystis pouchetii was investigated in spring 1996 during a massive bloom of this alga. Sediment traps were deployed at 40, 60, 100 and 170 m depth. Samples from the sediment traps and from the water column were taken in short intervals (1 day - 2 weeks). A multimarker approach (using pigments, fatty acids and sterols) was chosen to characterize suspended organic matter and sediment trap material. Biomarker patterns typical for Phaeocystis were detected at the Chlorophyll a maximum and in the sediment traps. The results give evidence for massive sedimentation of Phaeocystis derived organic matter below the euphotic zone in the Balsfjord.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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