Antioxidative responses to different altitudes in leaves of alpine plant Polygonum viviparum in summer

2009 ◽  
Vol 31 (4) ◽  
pp. 839-848 ◽  
Author(s):  
Yuping Wang ◽  
Wenliang He ◽  
Huiying Huang ◽  
Lizhe An ◽  
Di Wang ◽  
...  
Keyword(s):  
Alpine Plant ◽  
Antioxidative Responses ◽  
Different Altitudes

Antioxidative responses to different altitudes in Plantago major

1999 ◽  
Vol 42 (1) ◽  
pp. 51-59 ◽  
Author(s):  
Hong-Xu Ren ◽  
Zong-Ling Wang ◽  
Xiong Chen ◽  
Yuan-Lin Zhu
Keyword(s):  
Plantago Major ◽  
Antioxidative Responses ◽  
Different Altitudes

Dynamic metabolic analysis of tobacco starch biosynthesis at different altitudes

2013 ◽  
Vol 38 (1) ◽  
pp. 22-26
Author(s):  
Yong-xia YANG ◽  
Bing-jin SHI ◽  
Xiao-long WANG ◽  
Qi FENG ◽  
Song-tao ZHANG ◽  
...  
Keyword(s):  
Starch Biosynthesis ◽  
Metabolic Analysis ◽  
Different Altitudes

Changes of Ionic and Oxygen Isotopic Composition of the Snowpack at the Glacier Austre Okstindbreen, Norway, 1995

1998 ◽  
Vol 29 (1) ◽  
pp. 1-20 ◽  
Author(s):  
Peter Raben ◽  
Wilfred H. Theakstone
Keyword(s):  
Isotopic Composition ◽  
Sea Level ◽  
Oxygen Isotopes ◽  
Oxygen Isotopic Composition ◽  
Isotopic Ratios ◽  
Vertical Variations ◽  
Oxygen Isotopic ◽  
The Difference ◽  
Liquid Precipitation ◽  
Different Altitudes

Marked vertical variations of ions and oxygen isotopes were present in the snowpack at the glacier Austre Okstindbreen during the pre-melting phase in 1995 at sites between 825 m and 1,470 m above sea level. As the first meltwater percolated from the top of the pack, ions were moved to a greater depth, but the isotopic composition remained relatively unchanged. Ions continued to move downwards through the pack during the melting phase, even when there was little surface melting and no addition of liquid precipitation. The at-a-depth correlation between ionic concentrations and isotopic ratios, strong in the pre-melting phase, weakened during melting. In August, concentrations of Na+ and Mg2+ ions in the residual pack were low and vertical variations were slight; 18O enrichment had occurred. The difference of the time at which melting of the snowpack starts at different altitudes influences the input of ions and isotopes to the underlying glacier.

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