scholarly journals Iron and zinc isotope fractionation during uptake and translocation in rice (Oryza sativa) grown in oxic and anoxic soils

2015 ◽  
Vol 347 (7-8) ◽  
pp. 397-404 ◽  
Author(s):  
Tim Arnold ◽  
Tamara Markovic ◽  
Guy J.D. Kirk ◽  
Maria Schönbächler ◽  
Mark Rehkämper ◽  
...  
2018 ◽  
Vol 9 ◽  
Author(s):  
Pablo Díaz-Benito ◽  
Raviraj Banakar ◽  
Sara Rodríguez-Menéndez ◽  
Teresa Capell ◽  
Rosario Pereiro ◽  
...  

Author(s):  
P. Savitha ◽  
R. Usha Kumari

Rice (Oryza sativa L.) which belongs to the family poaceae, is the life and the prince among cereals as this unique grain helps to sustain two thirds of the world's population. India have traditionally been used or rice cultivation due to availability of water and conductive soil (Nadesa panic). Rice was grown in 155.30 million hectares and around 600 million tonnes of rice harvested each year globally. About 114 countries produce rice with China and India supporting 50 per cent of total production. India stands first in area under cultivation (41.85 mha) and ranks second in production, where as China ranks first in production with just half of the area. India's production is 89.13 million tonnes with a productivity of 2130 kg/ha. Among the rice producing states of India, Tamil Nadu ranks sixth in production (6.53 million tonnes) and second in productivity of 3918 kg/ha with an area of 20.16 lakh ha (Season and Crop Report, 2012). Local farmers in such farming systems retain the traditional varieties based on their knowledge of the quality of the rice varieties and their adaptation to varying agro-ecological situations created by diverse seasons and land situations (Tapasi das & Ashesh Kumar Das, 2014). Among the major micronutrient deficiencies common in rice consuming countries, iron and zinc deficiencies (“hidden hunger”), affect over three billion people worldwide, mostly in developing countries (Welch & Graham, 2004).


2019 ◽  
Vol 70 (10) ◽  
pp. 2773-2786 ◽  
Author(s):  
Rita Giuliani ◽  
Shanta Karki ◽  
Sarah Covshoff ◽  
Hsiang-Chun Lin ◽  
Robert A Coe ◽  
...  

2018 ◽  
Vol 219 (1) ◽  
pp. 195-205 ◽  
Author(s):  
Matthias Wiggenhauser ◽  
Moritz Bigalke ◽  
Martin Imseng ◽  
Armin Keller ◽  
Corey Archer ◽  
...  

2019 ◽  
Vol 244 ◽  
pp. 99-112 ◽  
Author(s):  
Vasileios Mavromatis ◽  
Aridane G. González ◽  
Martin Dietzel ◽  
Jacques Schott

2014 ◽  
Vol 48 (20) ◽  
pp. 11926-11933 ◽  
Author(s):  
Teng-Hao-Bo Deng ◽  
Christophe Cloquet ◽  
Ye-Tao Tang ◽  
Thibault Sterckeman ◽  
Guillaume Echevarria ◽  
...  

2017 ◽  
Vol 63 (2) ◽  
pp. 660-671 ◽  
Author(s):  
Moneesha Samanta ◽  
Michael J. Ellwood ◽  
Robert F. Strzepek

2020 ◽  
Vol 71 (3) ◽  
pp. 355 ◽  
Author(s):  
Michael J. Ellwood ◽  
Robert Strzepek ◽  
Xiaoyu Chen ◽  
Thomas W. Trull ◽  
Philip W. Boyd

In this study we investigated the distribution of dissolved and particulate zinc (dZn and pZn respectively) and its isotopes in the Subantarctic Zone as part of a Geotraces Process voyage. dZn and pZn depth profiles contrasted each other, with dZn showing depletion within the euphotic zone while pZn profiles showed enrichment. Fitting a power law equation to the pZn profiles produced an attenuation factor of 0.82, which contrasted values for particulate phosphorus, cadmium and copper. The results indicate that zinc has a longer regeneration length scale than phosphorus and cadmium, but shorter than copper. The differential regeneration of pZn relative to that of particulate phosphorus likely explains why dZn appears to have a deeper regeneration profile than that of phosphate. The dZn isotope (δ66Zndissolved) profiles collected across the Subantarctic Zone showed differing profile structures. For one station collected within an isolated cold-core eddy (CCE), δ66Zndissolved showed surface enrichment relative to deep waters. The corresponding pZn isotope profiles within the CCE did not show enrichment; rather, they were subtly depleted in surface waters and then converged to similar values at depth. Zinc isotope fractionation can be explained through a combination of fractionation processes associated with uptake by phytoplankton, zinc complexation by natural organic ligands and zinc regeneration from particulate matter.


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