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MEPS 238:15-29 (2002)
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Abstract
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Benthic diatoms of a high Arctic fjord (Young Sound, NE Greenland): importance for ecosystem primary production
Ronnie N. Glud1,*, Michael Kühl1, Frank Wenzhöfer1,3, Søren Rysgaard2
1 Marine Biological Laboratory, Copenhagen University, Strandpromenaden 5, 3000 Helsingør, Denmark
2 Department of Marine Ecology, National Environmental Research Institute, Vejlsøvej 25, 8600 Silkeborg, Denmark
3 Max Planck Institute for Marine Microbiology, Celsiusstr. 1, 28359 Bremen, Germany
*E-mail: rnglud@zi.ku.dk

ABSTRACT: Patches of benthic diatoms covered 23 to 73% of the sediment area at water depths down to 30 m of a high Arctic fjord system (Young Sound, NE Greenland). Mapping of the in situ chlorophyll (chl a) fluorescence by a pulse amplitude
modulated (PAM) fluorometer demonstrated the presence of diatom-covered sediment patches with a characteristic size scale of 5 to 8 m. The benthic diatoms were well adapted to the ambient irradiance as demonstrated by in situ measurements of the
relative electron transport rate (ETR) versus irradiance. However, the characteristics of the PE (photosynthesis versus downwelling irradiance) relations changed within minutes after exposure to changed light conditions neutralizing any depth related
light acclimation. This demonstrated that the diatoms efficiently optimized their photosynthetic apparatus to the current light conditions. Steady state O2 microprofiles measured in situ and in the laboratory showed a gradual increase in
the O2 penetration depth and O2 concentration at the sediment surface with increasing irradiance. Net photosynthesis showed a compensation irradiance of 4.5 µmol photons m-2 s-1 and a net photosynthetic
capacity (Pmax) of 85 O2 mmol m-2 d-1. No photoinhibition was observed at the maximum irradiance of 140 µmol photons m-2 s-1. Total exchange rates of O2 and DIC mirrored each
other and confirmed the depth distribution of benthic diatoms and the microsensors measurements. The compensation irradiance for the integrated benthic community (including macrofauna) decreased with water depth to a minimum of 12 µmol photons
m-2 s-1 at 30 m water depth. The mean O2/DIC exchange ratio across the benthic interface was approximately 1.2 and was independent of water depth. Extrapolation of our productivity data to the outer fjord system by
accounting for the in situ light regime showed that the primary production of the benthic diatoms was equivalent to that of benthic macroalgae. Benthic net photosynthesis was almost 7 times higher than the gross photosynthetic rates of the pelagic
community for water depths <30 m. However, integrated for the entire outer Young Sound, benthic net photosynthesis only accounted for ~70% of the pelagic production as measured by the 14C-incubation technique.
KEY WORDS: Benthic microphytes · Microelectrodes · Photosynthesis
Full text in pdf format

Published in MEPS Vol.
238
(2002) on August 8
Print ISSN: 0171-8630; Online ISSN: 1616-1599.
Copyright © Inter-Research, Oldendorf/Luhe, 2002
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