Transport and assimilation of inorganic carbon by Lichina pygmaea under emersed and submersed conditions
Photosynthetic O2evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light-saturated conditions at 5⚬C is saturated by the 2 mol m-3inorganic C found in seawater at pH 8.0. Photosynthesis is not reduced when pH is increased to pH 9.4, and is slightly reduced at pH 10.0, wh...
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| Published in | The New phytologist Vol. 114; no. 3; pp. 407 - 417 |
|---|---|
| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
| Published |
Oxford, UK
Cambridge University Press
01.03.1990
Blackwell Publishing Ltd Blackwell |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Photosynthetic O2evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light-saturated conditions at 5⚬C is saturated by the 2 mol m-3inorganic C found in seawater at pH 8.0. Photosynthesis is not reduced when pH is increased to pH 9.4, and is slightly reduced at pH 10.0, when submersed in seawater with 2 mol m-3inorganic C. The rate of photosynthesis at pH 10 greatly exceeds the rate of uncatalysed conversion of HCO3
-. It is concluded that HCO3
-is used in photosynthesis. Since extracellular carbonic anhydrase is present, it is possible that CO2enters the photobiont (Calothrix) cells even during HCO3
-use. pH drift experiments support the notion of HCO3
-use. Emersed photosynthesis at 5⚬C is more than half-saturated by 35 Pa (normal atmospheric) CO2; the light- and CO2-saturated emersed photosynthetic rate is not significantly different from the light and inorganic C-saturated photosynthetic rate when submersed. Inorganic C diffusion from the thallus surface to the photobiont needs, at least under some conditions, carbonic anhydrase activity which permits HCO3
-fluxes to supplement CO2movement. The CO2compensation partial pressure at 5⚬C is 0.83 Pa, i.e. at the low range of values found for terrestrial cyanobacterial lichens. Dark14C-inorganic C assimilation when submersed is a small fraction of the dark respiratory rate, consistent with the observed absence of diel CAM-like variation in intracellular titratable acidity. The high value (-11.5 per mil) of δ13C, the low CO2compensation partial pressure, and the relatively high affinity for inorganic C, are consistent with the operation of an inorganic C concentrating mechanism such as occurs in free-living cyanobacteria and probably occurs in terrestrial cyanobacterial lichens and in most intertidal algae. |
|---|---|
| AbstractList | Photosynthetic O
evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light-saturated conditions at 5 °C is saturated by the 2 mol m
inorganic C found in seawater at pH 8.0. Photosynthesis is not reduced when pH is increased to pH 9.4, and is slightly reduced at pH 10.0, when submersed in seawater with 2 mol m
inorganic C. The rate of photosynthesis at pH 10 greatly exceeds the rate of uncatalysed conversion of HCO
. It is concluded that HCO
is used in photosynthesis. Since extracellular carbonic anhydrase is present, it is possible that CO
enters the photobiont (Calothrix) cells even during HCO
use. pH drift experiments support the notion of HCO
use. Emersed photosynthesis at 5 °C is more than half-saturated by 35 Pa (normal atmospheric) CO
; the light- and CO
-saturated emersed photosynthetic rate is not significantly different from the light and inorganic C-saturated photosynthetic rate when submersed. Inorganic C diffusion from the thallus surface to the photobiont needs, at least under some conditions, carbonic anhydrase activity which permits HCO
fluxes to supplement CO
movement. The CO
compensation partial pressure at 5 °C is 0.83 Pa, i.e. at the low range of values found for terrestrial cyanobacterial lichens. Dark
C-inorganic C assimilation when submersed is a small fraction of the dark respiratory rate, consistent with the observed absence of diel CAM-like variation in intracellular titratable acidity. The high value (-11.5%) of δ
C, the low CO
compensation partial pressure, and the relatively high affinity for inorganic C., are consistent with the operation of an inorganic C concentrating mechanism such as occurs in free-living cyanobacteria and probably occurs in terrestrial cyanobacterial lichens and in most intertidal algae. SUMMARY Photosynthetic O 2 evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light‐saturated conditions at 5 °C is saturated by the 2 mol m −3 inorganic C found in seawater at pH 8.0. Photosynthesis is not reduced when pH is increased to pH 9.4, and is slightly reduced at pH 10.0, when submersed in seawater with 2 mol m −3 inorganic C. The rate of photosynthesis at pH 10 greatly exceeds the rate of uncatalysed conversion of HCO 3 − . It is concluded that HCO 3 − is used in photosynthesis. Since extracellular carbonic anhydrase is present, it is possible that CO 2 enters the photobiont ( Calothrix ) cells even during HCO 3 use. pH drift experiments support the notion of HCO 3 − use. Emersed photosynthesis at 5 °C is more than half‐saturated by 35 Pa (normal atmospheric) CO 2 ; the light‐ and CO 2 ‐saturated emersed photosynthetic rate is not significantly different from the light and inorganic C‐saturated photosynthetic rate when submersed. Inorganic C diffusion from the thallus surface to the photobiont needs, at least under some conditions, carbonic anhydrase activity which permits HCO 3 − fluxes to supplement CO 2 movement. The CO 2 compensation partial pressure at 5 °C is 0.83 Pa, i.e. at the low range of values found for terrestrial cyanobacterial lichens. Dark 14 C‐inorganic C assimilation when submersed is a small fraction of the dark respiratory rate, consistent with the observed absence of diel CAM‐like variation in intracellular titratable acidity. The high value (−11.5%) of δ 13 C, the low CO 2 compensation partial pressure, and the relatively high affinity for inorganic C., are consistent with the operation of an inorganic C concentrating mechanism such as occurs in free‐living cyanobacteria and probably occurs in terrestrial cyanobacterial lichens and in most intertidal algae. Photosynthetic O2evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light-saturated conditions at 5⚬C is saturated by the 2 mol m-3inorganic C found in seawater at pH 8.0. Photosynthesis is not reduced when pH is increased to pH 9.4, and is slightly reduced at pH 10.0, when submersed in seawater with 2 mol m-3inorganic C. The rate of photosynthesis at pH 10 greatly exceeds the rate of uncatalysed conversion of HCO3 -. It is concluded that HCO3 -is used in photosynthesis. Since extracellular carbonic anhydrase is present, it is possible that CO2enters the photobiont (Calothrix) cells even during HCO3 -use. pH drift experiments support the notion of HCO3 -use. Emersed photosynthesis at 5⚬C is more than half-saturated by 35 Pa (normal atmospheric) CO2; the light- and CO2-saturated emersed photosynthetic rate is not significantly different from the light and inorganic C-saturated photosynthetic rate when submersed. Inorganic C diffusion from the thallus surface to the photobiont needs, at least under some conditions, carbonic anhydrase activity which permits HCO3 -fluxes to supplement CO2movement. The CO2compensation partial pressure at 5⚬C is 0.83 Pa, i.e. at the low range of values found for terrestrial cyanobacterial lichens. Dark14C-inorganic C assimilation when submersed is a small fraction of the dark respiratory rate, consistent with the observed absence of diel CAM-like variation in intracellular titratable acidity. The high value (-11.5 per mil) of δ13C, the low CO2compensation partial pressure, and the relatively high affinity for inorganic C, are consistent with the operation of an inorganic C concentrating mechanism such as occurs in free-living cyanobacteria and probably occurs in terrestrial cyanobacterial lichens and in most intertidal algae. SUMMARY Photosynthetic O2 evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light‐saturated conditions at 5 °C is saturated by the 2 mol m−3 inorganic C found in seawater at pH 8.0. Photosynthesis is not reduced when pH is increased to pH 9.4, and is slightly reduced at pH 10.0, when submersed in seawater with 2 mol m−3 inorganic C. The rate of photosynthesis at pH 10 greatly exceeds the rate of uncatalysed conversion of HCO3−. It is concluded that HCO3− is used in photosynthesis. Since extracellular carbonic anhydrase is present, it is possible that CO2 enters the photobiont (Calothrix) cells even during HCO3 use. pH drift experiments support the notion of HCO3− use. Emersed photosynthesis at 5 °C is more than half‐saturated by 35 Pa (normal atmospheric) CO2; the light‐ and CO2‐saturated emersed photosynthetic rate is not significantly different from the light and inorganic C‐saturated photosynthetic rate when submersed. Inorganic C diffusion from the thallus surface to the photobiont needs, at least under some conditions, carbonic anhydrase activity which permits HCO3− fluxes to supplement CO2 movement. The CO2 compensation partial pressure at 5 °C is 0.83 Pa, i.e. at the low range of values found for terrestrial cyanobacterial lichens. Dark 14C‐inorganic C assimilation when submersed is a small fraction of the dark respiratory rate, consistent with the observed absence of diel CAM‐like variation in intracellular titratable acidity. The high value (−11.5%) of δ13C, the low CO2 compensation partial pressure, and the relatively high affinity for inorganic C., are consistent with the operation of an inorganic C concentrating mechanism such as occurs in free‐living cyanobacteria and probably occurs in terrestrial cyanobacterial lichens and in most intertidal algae. |
| Author | Mcinroy, S.G Johnston, A.M Raven, J.A Handley, L.L |
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| Keywords | Assimilation Littoral zone Scanning electron microscopy Carbon dioxide Ecophysiology Carbon Hydrogencarbonates Carbonic anhydrase Ultrastructure Lichenes Gas exchange Photosynthesis Thallophyta Adaptation CO2 compensation partial pressure photosynthesis carbonic anhydrase pH lichens C-isotope ratios inorganic C-concentrating mechanism |
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| Snippet | Photosynthetic O2evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light-saturated conditions at 5⚬C is saturated by the 2 mol... SUMMARY Photosynthetic O2 evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light‐saturated conditions at 5 °C is saturated by the... Photosynthetic O evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light-saturated conditions at 5 °C is saturated by the 2 mol m... SUMMARY Photosynthetic O 2 evolution by the upper littoral lichen, Lichina pygmaea (Lightf.) C.Ag., under light‐saturated conditions at 5 °C is saturated by... |
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| SubjectTerms | Algae bicarbonates Biological and medical sciences Carbon dioxide carbonate dehydratase carbonic anhydrase CO2 compensation partial pressure compensation point Cyanobacteria C‐isotope ratios dark fixation diurnal variation Fundamental and applied biological sciences. Psychology gas exchange inorganic carbon concentrating mechanism inorganic C‐concentrating mechanism intertidal environment Lichens Metabolism net assimilation rate nutrient uptake oxygen Photosynthesis Photosynthesis, respiration. Anabolism, catabolism Physiology Plant physiology and development Plants Ravens Sea water seawater Thallus titratable acidity |
| Title | Transport and assimilation of inorganic carbon by Lichina pygmaea under emersed and submersed conditions |
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