Diurnal Cycles of Gaseous Mercury within the Snowpack at Kuujjuarapik/Whapmagoostui, Québec, Canada

2003 ◽  
Vol 37 (15) ◽  
pp. 3289-3297 ◽  
Author(s):  
Aurélien Dommergue ◽  
Christophe P. Ferrari ◽  
Laurier Poissant ◽  
Pierre-Alexis Gauchard ◽  
Claude F. Boutron
2003 ◽  
Vol 107 ◽  
pp. 389-392
Author(s):  
A. Dommergue ◽  
C. P. Ferrari ◽  
P.-A. Gauchard ◽  
L. Poissant ◽  
C. F. Boutron

2003 ◽  
Vol 107 ◽  
pp. 509-512 ◽  
Author(s):  
E. Garcia ◽  
J. Laroulandie ◽  
M. Amyot ◽  
X. R. Saint-Simon

2021 ◽  
Vol 9 (4) ◽  
pp. 809
Author(s):  
Hiroya Yurimoto ◽  
Kosuke Shiraishi ◽  
Yasuyoshi Sakai

Methanol is abundant in the phyllosphere, the surface of the above-ground parts of plants, and its concentration oscillates diurnally. The phyllosphere is one of the major habitats for a group of microorganisms, the so-called methylotrophs, that utilize one-carbon (C1) compounds, such as methanol and methane, as their sole source of carbon and energy. Among phyllospheric microorganisms, methanol-utilizing methylotrophic bacteria, known as pink-pigmented facultative methylotrophs (PPFMs), are the dominant colonizers of the phyllosphere, and some of them have recently been shown to have the ability to promote plant growth and increase crop yield. In addition to PPFMs, methanol-utilizing yeasts can proliferate and survive in the phyllosphere by using unique molecular and cellular mechanisms to adapt to the stressful phyllosphere environment. This review describes our current understanding of the physiology of methylotrophic bacteria and yeasts living in the phyllosphere where they are exposed to diurnal cycles of environmental conditions.


2000 ◽  
Vol 259 (1-3) ◽  
pp. 183-190 ◽  
Author(s):  
R. Ferrara ◽  
B. Mazzolai ◽  
E. Lanzillotta ◽  
E. Nucaro ◽  
N. Pirrone

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