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  • 2000-2004  (4)
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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science, Ltd
    Plant, cell & environment 24 (2001), S. 0 
    ISSN: 1365-3040
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: With microsensors, we measured the steady-state microprofiles of O2, pH and Ca2+ on the topside of young segments of Halimeda discoidea, as well as the surface dynamics upon light–dark shifts. The effect of several inhibitors was studied. The steady-state measurements showed that under high light intensity, calcium and protons were taken up, while O2 was produced. In the dark, O2 was consumed, the pH decreased to below seawater level and Ca2+ uptake was reduced to 50%. At low light intensity (12 mmol photons m-2 s-1), Ca2+ efflux was observed. Upon light–dark shifts, a complicated pattern of both the pH and calcium surface dynamics was observed. Illumination caused an initial pH decrease, followed by a gradual pH increase: this indicated that the surface pH of H. discoidea is determined by more than one light-induced process. When photosynthesis was inhibited by dichlorophenyl dimethyl urea (DCMU), a strong acidification was observed upon illumination. The nature and physiological function of this putative pump is not known. The calcium dynamics followed all pH dynamics closely, both in the presence and absence of DCMU. The Ca-channel blockers verapamil and nifedipine had no effect on the Ca2+ dynamics and steady-state profiles. Thus, in H. discoidea, calcification is not regulated by the alga, but is a consequence of pH increase during photosynthesis. Acetazolamide had no effect on photosynthesis, whereas ethoxyzolamide inhibited photosynthesis at higher light intensities. Therefore, all carbonic anhydrase activity is intracellular. Carbonic anhydrase is required to alleviate the CO2 limitation. Calcification cannot supply sufficient protons and CO2 to sustain photosynthesis.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2017-03-06
    Description: This paper presents a new non-invasive technique for measuring sediment O2 uptake that, in its concept, differs fundamentally from other methods used to date. In almost all natural aquatic environments, the vertical transport of O2 through the water column toward the sediment surface is facilitated by turbulent motion. The new technique relies on measuring 2 parameters simultaneously and at the same point in the water above the sediment: the fluctuating vertical velocity using an acoustic Doppler velocimeter and the fluctuating O2 concentration using an O2 microelectrode. From these 2 parameters, which typically are measured 10 to 50 cm above the sediment surface for a period of 10 to 20 min and at a frequency of 15 to 25 Hz, the vertical flux of O2 toward the sediment surface is derived. Based on measurements performed under actual field conditions and comparisons with in situ flux-chamber measurements, we believe that this new technique is the optimal approach for determining O2 uptake by sediments. The technique is superior to conventional methods as measurements are done under true in situ conditions, i.e. without any disturbance of the sediment and under the natural hydrodynamic conditions. Furthermore, this technique can be used for bio-irrigated or highly permeable sediments, such as sands, where traditional methods often fail. While this paper only focuses on O2 uptake by sediments, the technique can also be applied to other solutes that can be measured at a sufficiently high temporal resolution.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 3
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    Unknown
    In:  EPIC3MARBEF Theme 2 Kick-off Workshop, Palma de Mallorca.-18.5.04., 17
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
    Format: application/pdf
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  • 4
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    In:  EPIC31st General Assembly of the European Geosciences Union (EUG) Nice, FranceApril 2004., 25
    Publication Date: 2019-07-17
    Description: In situ measurements of microbial activity were performed on sediments of theHaakon Mosby Mud Vulcano (HVVM) in the Barents Sea. A lander was deployedcontaining a benthic chamber to measure O2 exchange and a profiling unit for microsensors(O2, H2S, pH and temperature). The volcano area consists of a centralarea where mud is expelled, surrounded by large fields of the sulfide oxidizingbacteria Beggiatoa. The outer rim of the HMMV is dominated by the symbioticmethane-oxidizing Pogonophora tubeworms. At a reference site outside the volcanoarea methane oxidation was insignificant. With microsensors the microenvironmentsin the zones of the main metabolic processes, anaerobic methane oxidation (AOM) andsulfide oxidation, were characterized. From the microprofiles local activities and diffusiveinterfacial fluxes were determined. The benthic chambers allowed total (advective+ diffusive) oxygen uptake rate measurements. Profound differences were found betweenthe Beggiatoa and Pogonophora fields. The process rates in Beggiatoa fields arecontrolled by diffusion, in Pogonophora fields by advection driven by benthic fauna.AOM is particularly high under the Beggiatoa fields in a narrow zone at 2 cm depth,characterized by a steep sulfide peak. Effectively, all methane diffusing upwards isoxidized in a zone less than 5 mm thick. No clear pH effects by AOM were observed.At the HMMV, AOM was tightly coupled to aerobic sulfide oxidation by Beggiatoa.Oxygen uptake rates measured on retrieved cores were ca 5 times lower than thosemeasured with the lander, demonstrating the importance of in situ measurements.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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