CARBONIC ANHYDRASE AND CARBON FIXATION IN COCCOLITHOPHORIDS

1982 ◽  
Vol 18 (3) ◽  
pp. 423-426 ◽  
Author(s):  
C. Steven Sikes ◽  
A. P. Wheeler
1982 ◽  
Vol 18 (3) ◽  
pp. 423-426 ◽  
Author(s):  
C. Steven Sikes ◽  
A. P. Wheeler

2009 ◽  
Vol 36 (2) ◽  
pp. 137 ◽  
Author(s):  
Hongyan Wu ◽  
Kunshan Gao

Previous studies have shown that reduced levels of solar UV radiation (280–400 nm) can enhance photosynthetic carbon fixation of marine phytoplankton, but the mechanisms are not known. The supply of CO2 for photosynthesis is facilitated by extracellular (periplasmic) carbonic anhydrase (CAe) in most marine phytoplankton species. The present study showed that the CAe activity of Skeletonema costatum (Greville) Cleve was stimulated when treated with UV-A (320–395 nm) or UV-A + UV-B (295–320 nm) in addition to visible radiation. The presence of UV-A and UV-B enhanced the activity by 28% and 24%, respectively, at a low irradiance (PAR 161, UV-A 28, UV-B 0.9 W m−2) and by 21% and 19%, respectively, at a high irradiance (PAR 328, UV-A 58, UV-B 1.9 W m−2) level after exposure for 1 h. Ultraviolet radiation stimulated CAe activity contributed up to 6% of the photosynthetic carbon fixation as a result of the enhanced supply of CO2, as revealed using the CAe inhibitor (acetazolamide). As a result, there was less inhibition of photosynthetic carbon fixation compared with the apparent quantum yield of PSII. The UV radiation stimulated CAe activity coincided with the enhanced redox activity at the plasma membrane in the presence of UV-A and/or UV-B. The present study showed that UV radiation can enhance CAe activity, which plays an important role in counteracting UV inhibition of photosynthesis.


eLife ◽  
2016 ◽  
Vol 5 ◽  
Author(s):  
Jason D Perlmutter ◽  
Farzaneh Mohajerani ◽  
Michael F Hagan

We computationally study how an icosahedral shell assembles around hundreds of molecules. Such a process occurs during the formation of the carboxysome, a bacterial microcompartment that assembles around many copies of the enzymes ribulose 1,5-bisphosphate carboxylase/ oxygenase and carbonic anhydrase to facilitate carbon fixation in cyanobacteria. Our simulations identify two classes of assembly pathways leading to encapsulation of many-molecule cargoes. In one, shell assembly proceeds concomitantly with cargo condensation. In the other, the cargo first forms a dense globule; then, shell proteins assemble around and bud from the condensed cargo complex. Although the model is simplified, the simulations predict intermediates and closure mechanisms not accessible in experiments, and show how assembly can be tuned between these two pathways by modulating protein interactions. In addition to elucidating assembly pathways and critical control parameters for microcompartment assembly, our results may guide the reengineering of viruses as nanoreactors that self-assemble around their reactants.


2005 ◽  
Vol 83 (7) ◽  
pp. 929-940 ◽  
Author(s):  
Emma Huertas ◽  
Gabriel Navarro ◽  
Susana Rodríguez-Gálvez ◽  
Laura Prieto

The spatial variability in carbon dioxide in surface waters of a coastal area of the Gulf of Cádiz (southwestern Spain) was examined in situ under spring bloom conditions. The influence of phytoplankton biomass and physicochemical variables on the CO2 concentration was studied. According to the relationship observed between chlorophyll a and pCO2, phytoplankton biomass was the main factor responsible for variations in carbon dioxide. The distribution of organic matter in the form of dissolved organic carbon and transparent exopolymer particles also reflected changes in phytoplankton abundance, since high levels of both variables were associated with high chlorophyll concentrations and low levels of free CO2. The involvement of the enzyme carbonic anhydrase in the process of inorganic carbon uptake by the phytoplankton community was also investigated through the effect of the inhibitors dextran-bound sulfonamide and ethoxyzolamide on primary production rates. Ethoxyzolamide substantially inhibited carbon fixation, causing decreases of 40%–60% in the maximum photosynthetic rates; whereas the membrane impermeable inhibitor dextran-bound sulfonamide affected primary production, depending on the diversity of the phytoplankton species composition. Calculations of CO2 fluxes indicated that the sampled coastal sector of the Gulf of Cádiz behaved as a net sink for atmospheric CO2 at the time of analysis, with an average CO2 absorption of –0.41 mmol·m–2·d–1.Key words: air–sea exchange of CO2, carbonic anhydrase, flow cytometry, Gulf of Cádiz, phytoplankton, transparent exopolymer particles.


2010 ◽  
Vol 76 (11) ◽  
pp. 3561-3567 ◽  
Author(s):  
Kimberly P. Dobrinski ◽  
Amanda J. Boller ◽  
Kathleen M. Scott

ABSTRACT The hydrothermal vent chemolithoautotroph Thiomicrospira crunogena grows rapidly in the presence of low concentrations of dissolved inorganic carbon (DIC) (= CO2 + HCO3 − + CO3 −2). Its genome encodes α-carbonic anhydrase (α-CA), β-CA, carboxysomal β-like CA (CsoSCA), and a protein distantly related to γ-CA. The purposes of this work were to characterize the gene products, determine whether they were differentially expressed, and identify those that are necessary for DIC uptake and fixation. When expressed in Escherichia coli, CA activity was detectable for α-CA, β-CA, and CsoSCA but not for the γ-CA-like protein. α-CA and CsoSCA but not β-CA were inhibited by sulfonamide inhibitors. CsoSCA was also inhibited by dithiothreitol. When grown under DIC limitation in chemostats, T. crunogena transcribed csoSCA more frequently than when ammonia limited, while genes encoding α-CA and β-CA were not differentially transcribed under these conditions. Cell extracts from T. crunogena grown under both DIC- and ammonia-limited conditions had CA activity that was strongly inhibited by sulfonamides, though extracts from nitrogen-limited cells had some CA activity that was resistant, perhaps due to a higher level of β-CA activity. Based on predictions from the SignalP software program, subcellular location when expressed in E. coli, and carbonic anhydrase assays conducted on intact T. crunogena cells, α-CA is located in the periplasm. However, inhibition of α-CA by acetazolamide had only a minor impact on rates of DIC uptake or fixation. Conversely, inhibition of CsoSCA with ethoxyzolamide inhibited carbon fixation but not DIC uptake, consistent with this enzyme functioning to facilitate DIC interconversion and fixation within carboxysomes.


2004 ◽  
Vol 186 (3) ◽  
pp. 623-630 ◽  
Author(s):  
Anthony K.-C. So ◽  
George S. Espie ◽  
Eric B. Williams ◽  
Jessup M. Shively ◽  
Sabine Heinhorst ◽  
...  

ABSTRACT A significant portion of the total carbon fixed in the biosphere is attributed to the autotrophic metabolism of prokaryotes. In cyanobacteria and many chemolithoautotrophic bacteria, CO2 fixation is catalyzed by ribulose-1,5-bisphosphate carboxylase/oxygenase (RuBisCO), most if not all of which is packaged in protein microcompartments called carboxysomes. These structures play an integral role in a cellular CO2-concentrating mechanism and are essential components for autotrophic growth. Here we report that the carboxysomal shell protein, CsoS3, from Halothiobacillus neapolitanus is a novel carbonic anhydrase (ε-class CA) that has an evolutionary lineage distinct from those previously recognized in animals, plants, and other prokaryotes. Functional CAs encoded by csoS3 homologues were also identified in the cyanobacteria Prochlorococcus sp. and Synechococcus sp., which dominate the oligotrophic oceans and are major contributors to primary productivity. The location of the carboxysomal CA in the shell suggests that it could supply the active sites of RuBisCO in the carboxysome with the high concentrations of CO2 necessary for optimal RuBisCO activity and efficient carbon fixation in these prokaryotes, which are important contributors to the global carbon cycle.


1991 ◽  
Vol 69 (5) ◽  
pp. 1123-1132 ◽  
Author(s):  
Andrew M. Johnston

Marine macroalgae inhabit three different environments: the eulittoral zone, rock pools, and the sublittoral zone. Many macroalgae exhibit C4 gas exchange characteristics, i.e., low CO2 compensation point, high pH compensation point, photosynthesis insensitive to changes in oxygen changes below 21 kPa, and a high affinity for inorganic carbon. It is concluded that in general eulittoral and rock-pool species are more C4-like than the subtidal species though there are interesting exceptions. Experimental evidence points to the following mechanisms being involved in inorganic carbon acquisition by macroalgae. The role of β-carboxylation as the primary step in carbon fixation is only convincing in Udotea flabellum, while PGA is the first product of 14C fixation in most species. Direct evidence of inorganic carbon accumulation is only available for Ulva fasciata, whereas Chondrus crispus does not have this ability. Studies show that carbonic anhydrase is prominent in the mechanism of carbon acquisition by Ascophyllum nodosum, and when inhibited the alga is dependent on CO2, whereas U. fasciata retains some ability to use bicarbonate ions. It is concluded that macroalgae display a range of inorganic carbon assimilation mechanisms that are active to varying degrees. The relationships between these mechanisms, the different macroalgal habitats, and carbonic anhydrase is discussed. Key words: inorganic carbon concentrating mechanisms, macroalgae, carbonic anhydrase.


1988 ◽  
Vol 15 (6) ◽  
pp. 727 ◽  
Author(s):  
JTM Elzenga ◽  
HBA Prins

The different abilities of three submerged aquatic macrophytes, Elodea canadensis, E. nutallii and Potamogeton lucens, cultured under high and low CO2 concentrations, to utilise bicarbonate was found to correlate with the ability to exhibit a polar leaf pH reaction (i. e. acidification of the medium on one side of the leaf). The utilisation of bicarbonate did not depend on the induction of extracellular carbonic anhydrase activity as found with unicellular algae. Although the bicarbonate utilisation was inhibited by acetazolamide, an inhibitor of carbonic anhydrase activity, there was no difference in the concentration of extracellular carbonic anhydrase between leaves with high and with low bicarbonate utilisation. In experiments using the isotopic disequilibrium method we found only a small contribution of bicarbonate to the carbon fixation of protoplast. The percentage of bicarbonate contribution to the fixation did not differ between protoplasts isolated from Potamogeton leaves with high bicarbonate utilisation (from a low CO2 culture) and from leaves with low bicarbonate utilisation (from a high CO2 culture). We conclude that bicarbonate utilisation depends on the polar leaf pH reaction and that CO2 is the carbon species that is taken up by the leaf.


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