INORGANIC CARBON REPLETION DISRUPTS PHOTOSYNTHETIC ACCLIMATION TO LOW TEMPERATURE IN THE CYANOBACTERIUM SYNECHOCOCCUS ELONGATUS1

2005 ◽  
Vol 41 (2) ◽  
pp. 322-334 ◽  
Author(s):  
Robert A. Burns ◽  
C. Danielle MacDonald ◽  
Patrick J. McGinn ◽  
Douglas. A. Campbell
Plants ◽  
2017 ◽  
Vol 6 (4) ◽  
pp. 32 ◽  
Author(s):  
Nityananda Khanal ◽  
Geoffrey Bray ◽  
Anna Grisnich ◽  
Barbara Moffatt ◽  
Gordon Gray

2016 ◽  
Vol 43 (10) ◽  
pp. 931 ◽  
Author(s):  
Barbara Jurczyk ◽  
Ewa Pociecha ◽  
Janusz Košcielniak ◽  
Marcin Rapacz

Increased precipitation and snowmelt during warmer winters may lead to low-temperature waterlogging of plants. Perennial ryegrass (Lolium perenne L.) is one of the most important cool-season grasses in agriculture. It is well adapted to cold climates, and may be considered as a model system for studying the mechanisms involved in cold acclimation. The aim of this study was to evaluate the effects of waterlogging on photosynthetic acclimation to cold in perennial ryegrass. Two L. perenne genotypes that differ in their responses to waterlogging in terms of freezing tolerance were compared. We evaluated the effects of waterlogging during cold acclimation on the water-soluble carbohydrate concentration, ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco) activity, photochemical efficiency of PSII, and transcript levels of the Rubisco activase (RcaA) and sucrose-sucrose fructosyltransferase (1-SST) genes. The genotype that did not accumulate water-soluble carbohydrates in the leaf under waterlogging showed a lower degree of feedback inhibition of photosynthesis under low temperature, and activated a photochemical mechanism of photosynthetic acclimation to cold. The other genotype accumulated water-soluble carbohydrates in the leaf during waterlogging, and activated a non-photochemical mechanism under cold conditions. Different photosynthetic acclimation systems to cold under waterlogging may be activated in these two contrasting L. perenne genotypes.


Author(s):  
P.P.K. Smith

Grains of pigeonite, a calcium-poor silicate mineral of the pyroxene group, from the Whin Sill dolerite have been ion-thinned and examined by TEM. The pigeonite is strongly zoned chemically from the composition Wo8En64FS28 in the core to Wo13En34FS53 at the rim. Two phase transformations have occurred during the cooling of this pigeonite:- exsolution of augite, a more calcic pyroxene, and inversion of the pigeonite from the high- temperature C face-centred form to the low-temperature primitive form, with the formation of antiphase boundaries (APB's). Different sequences of these exsolution and inversion reactions, together with different nucleation mechanisms of the augite, have created three distinct microstructures depending on the position in the grain.In the core of the grains small platelets of augite about 0.02μm thick have farmed parallel to the (001) plane (Fig. 1). These are thought to have exsolved by homogeneous nucleation. Subsequently the inversion of the pigeonite has led to the creation of APB's.


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