Aluminum resistance and cell-wall characteristics of pineapple root apices

2013 ◽  
Vol 176 (5) ◽  
pp. 795-800
Author(s):  
Yong-Hong Lin ◽  
Jen-Hshuan Chen
2002 ◽  
Vol 130 (1) ◽  
pp. 415-421 ◽  
Author(s):  
Qin Yu ◽  
Andrej Hlavacka ◽  
Toru Matoh ◽  
Dieter Volkmann ◽  
Diedrik Menzel ◽  
...  

1968 ◽  
Vol 46 (4) ◽  
pp. 391-395 ◽  
Author(s):  
R. M. Endo ◽  
W. W. Thomson ◽  
Emmylou M. Krausman

To study the effects of growth-inhibitory concentrations of D-galactose on the morphology and function of organelles, thin sections of galactose-treated, KMnO4-fixed bentgrass (Agrostis palustris L.) root apices were examined in the electron microscope. Inhibitory effects were noted on root cap mucilage formation, cell plate formation, cell wall accretion, and the organelles associated with these processes such as the dictyosomes and the endoplasmic reticulum. These studies suggest that D-galactose inhibits root elongation by not only suppressing the synthesis of cell wall precursors—as evidenced by apparent reduction in the activity of the dictyosomes and root cap mucilage formation—but also the cellular processes involved in cell wall accretion and the formation of the cell plate.


2005 ◽  
Vol 27 (3) ◽  
pp. 297-302 ◽  
Author(s):  
Teresa M. M. dos Santos ◽  
Jan J. laski ◽  
Miguel ă. A. Pinheiro de Carvalho ◽  
Gregory J. Taylor ◽  
Maria R. Clemente Vieira

2010 ◽  
Vol 138 (2) ◽  
pp. 176-190 ◽  
Author(s):  
Andrés Felipe Rangel ◽  
Idupulapati Madhusudana Rao ◽  
Hans-Peter Braun ◽  
Walter Johannes Horst

2001 ◽  
Vol 125 (3) ◽  
pp. 1473-1484 ◽  
Author(s):  
Peter Wenzl ◽  
Gloria M. Patiño ◽  
Alba L. Chaves ◽  
Jorge E. Mayer ◽  
Idupulapati M. Rao

1997 ◽  
Vol 161 ◽  
pp. 491-504 ◽  
Author(s):  
Frances Westall

AbstractThe oldest cell-like structures on Earth are preserved in silicified lagoonal, shallow sea or hydrothermal sediments, such as some Archean formations in Western Australia and South Africa. Previous studies concentrated on the search for organic fossils in Archean rocks. Observations of silicified bacteria (as silica minerals) are scarce for both the Precambrian and the Phanerozoic, but reports of mineral bacteria finds, in general, are increasing. The problems associated with the identification of authentic fossil bacteria and, if possible, closer identification of bacteria type can, in part, be overcome by experimental fossilisation studies. These have shown that not all bacteria fossilise in the same way and, indeed, some seem to be very resistent to fossilisation. This paper deals with a transmission electron microscope investigation of the silicification of four species of bacteria commonly found in the environment. The Gram positiveBacillus laterosporusand its spore produced a robust, durable crust upon silicification, whereas the Gram negativePseudomonas fluorescens, Ps. vesicularis, andPs. acidovoranspresented delicately preserved walls. The greater amount of peptidoglycan, containing abundant metal cation binding sites, in the cell wall of the Gram positive bacterium, probably accounts for the difference in the mode of fossilisation. The Gram positive bacteria are, therefore, probably most likely to be preserved in the terrestrial and extraterrestrial rock record.


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