scholarly journals Effect heat stress on subcellular localization of Ca2+ in tomato fruits

2014 ◽  
Vol 67 (3-4) ◽  
pp. 235-241 ◽  
Author(s):  
Grażyna Garbaczewska ◽  
Danuta Chołuj ◽  
Zofia Starck

The aim of this paper was to compare the fruit cell ultrastructure and subcellular localization of Ca<sup>2+</sup> after heat stress with the use of the potassium antimonate method (Slocum and Roux 1982, Tretyn et al. 1992). The tomato plants Robin cv., relatively tolerant to heat stress, were grown under uncontrolled greenhouse conditions to the stage of fruiting. The plants were placed for 20h in two temperature regimes: 23<sup>o</sup>C (optimal temperature) or 40<sup>o</sup>C (heat stress) in darkness, under water vapour saturated atmosphere. Immediately after heat stress the fruits were harvested to estimate water soluble and insoluble calcium contents and subcellular localization of Ca<sup>2+</sup>. After heating the concentration of calcium in tomato fruits increased about twice. In both temperature treatments the water soluble fractions were lower than insoluble ones at smaller differences between insoluble and soluble fractions after heat stress. The shapes and localization of Ca<sup>2+</sup> detected with the use of potassium antimonate method show that in fruits of control plants the precipitates were numerous, small and of oval shape. They were dispersed in cytosol or adjoined to endoplasmic reticulum or to external membrane of chloroplast. In the fruit of heated plants the precipitates were irregular in shape, amorphous and singly dispersed in the cytosol. We observed also some cytological changes in the structure of membranes and organelles of the plants of both experimental treatments. The heat induced increase of calcium content and the changes in subcellular localization of Ca<sup>2+</sup> under heat stress suggest that calcium ions may be involved in avoiding heat injury. The problem requires more detailed further investigations.

2004 ◽  
Vol 5 (4) ◽  
pp. 309 ◽  
Author(s):  
Hyun Woo Kim ◽  
Young Bae Kwon ◽  
Tae Won Ham ◽  
Dae Hyun Roh ◽  
Seo Yeon Yoon ◽  
...  

2003 ◽  
Vol 3 (4) ◽  
pp. 3659-3679 ◽  
Author(s):  
M. Seifert ◽  
J. Ström ◽  
R. Krejci ◽  
A. Minikin ◽  
A. Petzold ◽  
...  

Abstract. A thermal volatility technique is used to provide indirect information about the chemical composition of the aerosol involved in cirrus cloud formation. The fraction of particles that disappears after being heated to 125°C is termed volatile and the fraction that disappears between 125 and 250°C is termed semi-volatile. Particles that still remain after being heated to 250°C make up the non-volatile fraction. The thermal composition of residual particles remaining from evaporated cirrus crystals is presented and compared to interstitial aerosol particles (non-activated particles in between the cirrus crystals) for two temperature regimes (cold: T<235 K, warm: 235<T<250 K), based on in-situ observations. The observations were conducted in cirrus clouds in the Southern Hemisphere (SH) and Northern Hemisphere (NH) midlatitudes during the INCA project. In the cold temperature regime, the non-volatile fraction of the residual particles was typically in the range 10 to 30% in the NH and 30 to 40% in the SH. In the warm temperature regime, the non-volatile residual fraction was typically 10 to 30% (NH) and 20 to 40% (SH). At high crystal number densities the non-volatile fraction in both temperature regimes was even higher: in the range of 30 to 40% (NH) and 40 to 50% (SH). The semi-volatile fraction was typically less than 10% in both hemispheres, causing the volatile fraction to essentially be a complement to the non-volatile fraction. In terms of the fractioning into the three types of particles, the SH cold case is clearly different compared to the other three cases (the two warm cases and the cold NH case), which share many features. In the NH data the distribution of different particle types does not seem to be temperature dependent. In all the cases, the non-volatile fraction is enriched in the residual particles compared to the fractions observed for the interstitial particles. This enrichment corresponds to about 15 (NH) and 30 (SH) percent units in the two cold cases and to 15–25 (NH) and 25–35 (SH) percent units in the two warm cases. In the NH cold case, there is a clear relation between the fractions observed in the interstitial particles and what is observed in the residual particles. The observed large fractions of non-volatile particles show that particles forming ice crystals are not entirely made up of water-soluble sulfate particles.


2018 ◽  
Vol 24 (11) ◽  
pp. 5454-5470 ◽  
Author(s):  
Thomas A. Day ◽  
Michael S. Bliss ◽  
Alexander R. Tomes ◽  
Christopher T. Ruhland ◽  
René Guénon

2022 ◽  
Vol 177 ◽  
pp. 114540
Author(s):  
Caio Silvestre Lima Sanson ◽  
Cristiane Vieira Helm ◽  
Washington Luiz Esteves Magalhães ◽  
Graciela Inés Bolzon de Muniz ◽  
André Luiz Missio ◽  
...  

2019 ◽  
Vol 53 (7) ◽  
pp. 3782-3790 ◽  
Author(s):  
Huimin Ma ◽  
Jun Li ◽  
Cong Wan ◽  
Yaohui Liang ◽  
Xiangyun Zhang ◽  
...  

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