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Differential accumulation of maysin and rhamnosylisoorientin in leaves of high-altitude landraces of maize after UV-B exposure
PAULA CASATI 1 & VIRGINIA WALBOT 1
  1 Department of Biological Sciences, 385 Serra Mall, Stanford University, Stanford, CA 94305–5020, USA
Correspondence to  Paula Casati. Fax: + 1 650 725 8221; email: pcasati@stanford.edu
Copyright 2005 Blackwell Publishing Ltd
KEYWORDS
Zea mays • flavone • maysin • rhamnosylisoorientin • ultraviolet-B (UV-B)

ABSTRACT

AbstractINTRODUCTIONMATERIALS AND METHODSRESULTSDISCUSSIONACKNOWLEDGMENTSREFERENCES

Flavonoid induction by UV-B was investigated in five maize landraces from high altitudes and a W23 inbred line lacking the B1 and Pl1 transcription factors required for anthocyanin synthesis. In their natural habitats these landraces receive much higher UV-B fluence than plants at lower altitudes at similar latitudes and would be predicted to have UV-B tolerance by recurrent selection against UV-B stress. We identified two flavones that are induced by UV-B in leaves of high-altitude lines: maysin and its biosynthetic precursor rhamnosylisoorientin. Accumulation is controlled by a p-homologous transcription factor expressed in leaves, and this factor is regulated by UV-B. The levels of either maysin or rhamnosylisoorientin are higher in seedling leaves than in subsequent leaves; the highest flavone concentration was detected in silks. Some landraces have only rhamnosylisoorientin; this likely reflects a mutation in salmon silk1 (sm1) or in a duplicate locus, as genetic crosses with W23 restore the production of maysin in heterozygous F1 plants. In conclusion, it is demonstrated that maize plants from high altitudes respond to UV-B radiation by accumulating UV-absorbing flavones in leaves; in contrast, these compounds are present at only very low levels in inbred lines such as W23 and are not regulated by UV-B.


Received 22 November 2004; received in revised form 6 January 2005; accepted for publication 13 January 2005

DIGITAL OBJECT IDENTIFIER (DOI)
10.1111/j.1365-3040.2005.01329.x About DOI

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