Nitrate and Ammonium Assimilation by Roots of Maize (Zea maysL.) Seedlings as Investigated byIn Vivo15N-NMR

1992 ◽  
Vol 43 (5) ◽  
pp. 633-639 ◽  
Author(s):  
SARA AMANCIO ◽  
HELENA SANTOS
2013 ◽  
Vol 64 (11) ◽  
pp. 3373-3383 ◽  
Author(s):  
Emanuel Sanz-Luque ◽  
Francisco Ocaña-Calahorro ◽  
Angel Llamas ◽  
Aurora Galvan ◽  
Emilio Fernandez

2018 ◽  
Vol 9 (1) ◽  
Author(s):  
Johanna Bergkvist ◽  
Isabell Klawonn ◽  
Martin J. Whitehouse ◽  
Gaute Lavik ◽  
Volker Brüchert ◽  
...  

Abstract Chain-forming diatoms are key CO2-fixing organisms in the ocean. Under turbulent conditions they form fast-sinking aggregates that are exported from the upper sunlit ocean to the ocean interior. A decade-old paradigm states that primary production in chain-forming diatoms is stimulated by turbulence. Yet, direct measurements of cell-specific primary production in individual field populations of chain-forming diatoms are poorly documented. Here we measured cell-specific carbon, nitrate and ammonium assimilation in two field populations of chain-forming diatoms (Skeletonema and Chaetoceros) at low-nutrient concentrations under still conditions and turbulent shear using secondary ion mass spectrometry combined with stable isotopic tracers and compared our data with those predicted by mass transfer theory. Turbulent shear significantly increases cell-specific C assimilation compared to still conditions in the cells/chains that also form fast-sinking, aggregates rich in carbon and ammonium. Thus, turbulence simultaneously stimulates small-scale biological CO2 assimilation and large-scale biogeochemical C and N cycles in the ocean.


Planta ◽  
2005 ◽  
Vol 222 (4) ◽  
pp. 667-677 ◽  
Author(s):  
Magali Feraud ◽  
Céline Masclaux-Daubresse ◽  
Sylvie Ferrario-Méry ◽  
Karine Pageau ◽  
Maud Lelandais ◽  
...  

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