Abstract:When assayed near respective in situ temperatures, ribulose blsphosphate carboxylase (RuBPC) exhibits a greater response to increasing temperature in arctic than in tropical phytoplankton. This was also true when the Arrhen~us activation energy (E,) was compared for a range of intermediate temperatures. This difference in temperature response and E, for RuBPC is consistent with the temperature response of photosynthetic capacity, but is contrary to the general observation that coldenvironment ectotherms (organ… Show more
“…The high activity of RuBPC compared to PePC and PePCk clearly shows that C3-carboxylation dominated over p-carboxylations. This corresponds to data of Smith & Platt (1985), who showed for Arctic phytoplankton that RuBPC was the only enzyme tightly linked to photosynthetic capacity. For marine phytoplankton, Appleby et al (1980) and Descolas-Gros & Fontugne (1985) observed that RuBPC dominated over the PePC and PePCk.…”
Section: Enzyme Activitiessupporting
confidence: 90%
“…After 3 additional minutes of prelncubation, the samples were inoculated with NaHI4CO3 (100 pl, 5 yCi) and incubated at 20°C for 40 min. This temperature is adequate for enzyme activities according to the results of Li et al (1984) for 3 carboxylatlng enzymes in Arctic phytoplankton, and Descoslas-Gros & De Billy (1987) and Smith & Platt (1985) for RuBPC in respectively cultures of Antarctic diatoms and Arctic phytoplankton. The reaction was stopped by the addition of 0.5 m1 6 N HC1.…”
(chlorophyll a, carotenoids), photosynthetic parameters (Pmax, Ik, a, p) and carboxylating enzymes The complete transition from shade to light adaptation took place over 1 generation time while susceptibility to photoinhibition decreased more rapidly. Activities of carboxylating enzymes were never the ratelimiting step of photosynthesis. At low irradiances, increased pigments in the cells and modifications of the photosynthetic parameters suggest that photosynthesis did depend on the trapping of light energy and on the rate of electron transport. With increased irradiances, light energy harvested by the cells exceeded their energetic requirements, so that photosynthesis was only related to the rate of electron transport. These results emphasize the ability of sea-ice mlcroalgae to photoadapt to the seasonally increasing under-ice irradiance, showing that they are not an obligate shade flora in southeastern Hudson Bay.
“…The high activity of RuBPC compared to PePC and PePCk clearly shows that C3-carboxylation dominated over p-carboxylations. This corresponds to data of Smith & Platt (1985), who showed for Arctic phytoplankton that RuBPC was the only enzyme tightly linked to photosynthetic capacity. For marine phytoplankton, Appleby et al (1980) and Descolas-Gros & Fontugne (1985) observed that RuBPC dominated over the PePC and PePCk.…”
Section: Enzyme Activitiessupporting
confidence: 90%
“…After 3 additional minutes of prelncubation, the samples were inoculated with NaHI4CO3 (100 pl, 5 yCi) and incubated at 20°C for 40 min. This temperature is adequate for enzyme activities according to the results of Li et al (1984) for 3 carboxylatlng enzymes in Arctic phytoplankton, and Descoslas-Gros & De Billy (1987) and Smith & Platt (1985) for RuBPC in respectively cultures of Antarctic diatoms and Arctic phytoplankton. The reaction was stopped by the addition of 0.5 m1 6 N HC1.…”
(chlorophyll a, carotenoids), photosynthetic parameters (Pmax, Ik, a, p) and carboxylating enzymes The complete transition from shade to light adaptation took place over 1 generation time while susceptibility to photoinhibition decreased more rapidly. Activities of carboxylating enzymes were never the ratelimiting step of photosynthesis. At low irradiances, increased pigments in the cells and modifications of the photosynthetic parameters suggest that photosynthesis did depend on the trapping of light energy and on the rate of electron transport. With increased irradiances, light energy harvested by the cells exceeded their energetic requirements, so that photosynthesis was only related to the rate of electron transport. These results emphasize the ability of sea-ice mlcroalgae to photoadapt to the seasonally increasing under-ice irradiance, showing that they are not an obligate shade flora in southeastern Hudson Bay.
“…7A,B). The observation that NR activity in Skeletonema costatum is maximal around 10-15ЊC (Packard et al 1971;Kristiansen 1983;Dohler 1991) and inactivated above 20ЊC (Gao et al 1993(Gao et al , 1997 and the observation that RUBISCO activity is maximal at Ͼ30ЊC (Li et al 1984;Smith and Platt 1985;Descolas-Gros and de Billy 1987) are not yet available and therefore are not included. The linear regression is significant at the P Ͻ 0.001 level.…”
Marine diatoms generally form large blooms during periods of cool temperature (Ͻ20ЊC), high NO fluxes (Ͼ25 Ϫ 3 M-N), and turbulent mixing, but the adaptations that allow diatoms to bloom under these conditions are not well understood. We have conducted both NO uptake kinetics and direct short-term temperature manipulation studies Ϫ 3 on field diatom-dominated populations from Chesapeake and Delaware Bays during both spring and fall blooms. Absolute rates of NO uptake by a Rhizoselenia-dominated population did not appear to saturate even at concen- of experimental temperature (ambient Ϯ 9ЊC). Over the temperature range of 7-25ЊC, absolute uptake rates of NO ( NO3Ϫ ) decreased an average of 46% with increasing temperature from 7 to 25ЊC (nine individual experiments),while NH4ϩ and UREA increased with increasing temperature by an average of 179 and 86% (eight individual experiments), respectively. Based on these observations and the nature of the physical environment, we hypothesize that these diatom-dominated populations were taking up NO in excess of nutritional requirements, the reductionof which may serve as a sink for electrons during transient periods of imbalance between light energy harvesting and utilization. We suggest that the increase in non-nutritional NO uptake increases proportionately with themagnitude of the imbalance between light energy harvesting and imbalance. This hypothesis reconciles previous observations of low C : N uptake ratios, high release rates of dissolved organic nitrogen or NO by diatom-dominatedassemblages, other observations of nonsaturating NO kinetics in field populations, and the apparent ''preference''for NO by the netplankton size fraction. The two phenomena described here, nonsaturable kinetics and a negative mixing. Also, models of new production may need to incorporate terms for temperature dependence of NO uptake.
“…However, Arctic phytoplankton do not appear to acclimate to cold by increasing Rubisco content per unit pigment biomass 0. C. Smith and Platt 1985).…”
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