gradient of endogenous calcium forms in mucilage of graviresponding roots of Zea mays

Agar blocks that contacted the upper sides of tips of horizontally-oriented roots of Zea mays contain significantly less calcium (Ca) than blocks that contacted the lower sides of such roots. This gravity-induced gradient of Ca forms prior to the onset of gravicurvature, and does not form across tip...

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Bibliographic Details
Published inAnnals of botany Vol. 61; no. 1; pp. 113 - 116
Main Authors Moore, R, Fondren, W.M
Format Journal Article
LanguageEnglish
Published Headquarters Oxford University Press 1988
Academic Press
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Summary:Agar blocks that contacted the upper sides of tips of horizontally-oriented roots of Zea mays contain significantly less calcium (Ca) than blocks that contacted the lower sides of such roots. This gravity-induced gradient of Ca forms prior to the onset of gravicurvature, and does not form across tips of vertically-oriented roots or roots of agravitropic mutants. These results indicate that (1) Ca can be collected from mucilage of graviresponding roots, (2) gravity induces a downward movement of endogenous Ca in mucilage overlying the root tip, (3) this gravity-induced gradient of Ca does not form across tips of agravitropic roots, and (4) formation of a Ca gradient is not a consequence of gravicurvature. These results are consistent with gravity-induced movement of Ca being a trigger for subsequent redistribution of growth effectors (e.g. auxin) that induce differential growth and gravicurvature.
Bibliography:ark:/67375/HXZ-HX4T3JQW-G
ArticleID:61.1.113
istex:7C80D6283A6F6B3D6DC9521B24D934DF16482C42
HQ
Headquarters
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0305-7364
1095-8290
DOI:10.1093/oxfordjournals.aob.a087523