Cited by 273Selenium in Biological SystemsOrganoselenium and organotellurium chemistryNitrogen and Sulfur Effects on Brassica

Rate-Limiting Steps in Selenium Assimilation and Volatilization by Indian Mustard1

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de Souza, Mark P., Pilon-Smits, Elizabeth A.H., Lytle, C. Mel, Hwang, Seongbin, Tai, Jenny, Honma, Todd S.U., Yeh, Lucretia, Terry, Norman·1998·Plant Physiology

Abstract

Se can be accumulated by plants and volatilized to dimethylselenide, providing an attractive technology for Se phytoremediation. To determine the rate-limiting steps in Se volatilization from selenate and selenite, time- and concentration-dependent kinetics of Se accumulation and volatilization were studied in Indian mustard (Brassica juncea). Time-dependent kinetic studies showed that selenate was taken up 2-fold faster than selenite. Selenate was rapidly translocated to the shoot, away from the root, the site of volatilization, whereas only approximately 10% of the selenite was translocated. For both selenate- and selenite-supplied plants, Se accumulation and volatilization increased linearly with external Se concentration up to 20 μm; volatilization rates were also linearly correlated with root Se concentrations. Se-volatilization rates were 2- to 3-fold higher from plants supplied with selenite compared with selenate. Se speciation by x-ray absorption spectroscopy revealed that selenite-supplied plants accumulated organic Se, most likely selenomethionine, whereas selenate-supplied plants accumulated selenate. Our data suggest that Se volatilization from selenate is limited by the rate of selenate reduction, as well as by the availability of Se in roots, as influenced by uptake and translocation. Se volatilization from selenite may be limited by selenite uptake and by the conversion of selenomethionine to dimethylselenide.

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Crossref · 10.1104/pp.117.4.1487

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  • The main form of Se accumulated by hyperaccumulator species is organic methyl-SeCys, while in related non-hyperaccumulators a large fraction of Se remains in the inorganic form of selenite.

    “the main form of Se accumulated by hyperaccumulator species is organic methyl-SeCys [224], while in related non-hyperaccumulators a large fraction of the Se remains in the inorganic form of selenite [225,226].”

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Authors
de Souza, M. P., Pilon-Smits, E. A. H., Lytle, C. M., Hwang, S., Tai, J., Honma, T. S. U., Yeh, L., & Terry, N.
Affiliations
University of California, Berkeley (US)
Venue
Plant Physiology
Published
1998-08-01
Volume
117
Issue
4
Pages
1487-1494
ISSN
  • 0032-0889 (ISSN-L)
  • 1532-2548
OpenAlex
W2152999824
Cited by
273
References
0
Citations by year
2026: 1 · 2025: 1 · 2024: 4 · 2023: 8 · 2022: 6 · 2021: 4 · 2020: 9 · 2019: 14 · 2018: 15 · 2017: 18 · 2016: 8 · 2015: 19 · 2014: 11 · 2013: 12 · 2012: 18
FWCI
6.47
Type
journal article
Language
en
Open access
Locations
  • PLANT PHYSIOLOGY (publishedVersion)
  • PubMed Central (publishedVersion)
  • PubMed (publishedVersion)
Funders
  • U.S. Department of Energy
  • Electric Power Research Institute
Topics
  • Health Sciences › Nursing › Nutrition and Dietetics › Selenium in Biological Systems
  • Life Sciences › Pharmacology, Toxicology and Pharmaceutics › Toxicology › Organoselenium and organotellurium chemistry
  • Life Sciences › Biochemistry, Genetics and Molecular Biology › Molecular Biology › Nitrogen and Sulfur Effects on Brassica
Keywords
selenium volatilization, dimethylselenide, Brassica juncea, selenite uptake, selenate reduction, selenium translocation, selenomethionine, organic selenium, selenium speciation, rate-determining step

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