Plant Physiol. email content delivery
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Plant Physiology 76:36-39 (1984)
© 1984 American Society of Plant Biologists

This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via CrossRef
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Cline, G. R.
Right arrow Articles by Szaniszlo, P. J.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Cline, G. R.
Right arrow Articles by Szaniszlo, P. J.
Agricola
Right arrow Articles by Cline, G. R.
Right arrow Articles by Szaniszlo, P. J.
Articles

Effects of a Hydroxamate Siderophore on Iron Absorption by Sunflower and Sorghum 1

Gary R. Cline2, C. P. Patrick Reid, Paul E. Powell and Paul J. Szaniszlo

Department of Forest and Wood Sciences, Colorado State University, Fort Collins, Colorado 80523, Department of Microbiology, University of Texas, Austin, Texas 78712

When Fe was supplied at 100 micromolar in nutrient solution of pH 7.5, 10 and 1 micromolar levels of the siderophore desferrioxamine B (DFOB), a microbial iron transport compound, significantly ({alpha} = 0.05) enhanced growth and reduced chlorosis of an Fe-inefficient variety of sorghum (Sorghum bicolor L.). Although significantly adverse effects resulted when both Fe and desferrioxamine B (DFOB) were added at 100 micromolar as FeDFOB, the plants were relatively healthy when grown with 100 micromolar DFOB plus 200 micromolar Fe. It was concluded that sorghum absorbed Fe from the pool of nonchelated, solubilized Fe, and utilized DFOB as a shuttle agent, in equilibrium with this pool, to transport Fe from finely suspended solid phase Fe particles to the membrane of absorbing root cells.

In contrast to sorghum, absorption of Fe by the Fe-efficient species sunflower (Helianthus annuus L.) was related to the level of FeDFOB and independent of the level of solubilized, nonchelated Fe. The latter was decreased whenever the concentration of DFOB was equal to or greater than the concentration of total Fe. For an Fe concentration of 10 micromolar, significantly larger and greener plants were obtained when DFOB was present at 1, 10, or 100 micromolar than in the absence of DFOB. When grown with 100 micromolar FeDFOB, sunflower plants appeared larger and less chlorotic than those supplied with 100 micromolar Fe and no DFOB. Sunflower apparently was able to utilize FeDFOB more directly than was sorghum. It is suggested that sunflower acquires Fe after binding FeDFOB at membrane sites and/or by producing sufficient reductants in the rhizosphere to reduce biologically significant levels of Fe(III)DFOB to the less stable Fe(II)DFOB.


2 Present address: Caesar Kleberg Wildlife Research Institute, College of Agriculture, Texas A & I University, Kingsville, TX 78363.

1 Supported by National Science Foundation grant DEB-79-11276. From a dissertation by the senior author submitted to the Academic Faculty of Colorado State University in partial fulfillment of the requirements for the Ph.D. degree.




This article has been cited by other articles:


Home page
Soil Sci.Home page
H. Siebner-Freibach, Y. Hadar, and Y. Chen
Interaction of Iron Chelating Agents with Clay Minerals
Soil Sci. Soc. Am. J., March 1, 2004; 68(2): 470 - 480.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
ASPB Publications PLANT PHYSIOLOGY THE PLANT CELL
Copyright © 1984 by the American Society of Plant Biologists