INVESTIGADORES
RUBIO Gerardo
artículos
Título:
Mechanisms for the increase in phosphorus uptake of waterlogged plants: soil phosphorus availability, root morphology and uptake kinetics.
Autor/es:
RUBIO G., M. OESTERHELD, C.R. ALVAREZ, R.S. LAVADO
Revista:
OECOLOGIA
Editorial:
SPRINGER
Referencias:
Año: 1997 vol. 112 p. 150 - 155
ISSN:
0029-8549
Resumen:
<!-- /* Font Definitions */ @font-face {font-family:"Lucida Sans Typewriter"; panose-1:2 11 5 9 3 5 4 3 2 4; mso-font-charset:0; mso-generic-font-family:modern; mso-font-pitch:fixed; mso-font-signature:3 0 0 0 1 0;} /* Style Definitions */ p.MsoNormal, li.MsoNormal, div.MsoNormal {mso-style-parent:""; margin:0cm; margin-bottom:.0001pt; mso-pagination:none; mso-layout-grid-align:none; text-autospace:none; font-size:12.0pt; font-family:"Lucida Sans Typewriter"; mso-fareast-font-family:"Times New Roman"; mso-bidi-font-family:"Times New Roman"; mso-ansi-language:EN-US; mso-fareast-language:EN-US;} @page Section1 {size:612.0pt 792.0pt; margin:70.85pt 3.0cm 70.85pt 3.0cm; mso-header-margin:36.0pt; mso-footer-margin:36.0pt; mso-paper-source:0;} div.Section1 {page:Section1;} --> Waterlogging frequently reduces plant biomass allocation to roots. This response may result in a variety of alterations in mineral nutrition, which range from a proportional lowering of whole plant nutrient concentration as a result of unchanged uptake per unit root, to a maintenance of nutrient concentration by means of an increase in uptake per unit root. The first objective of this paper was to test these two alternative hypothetical responses. In a pot experiment, we evaluated how plant P concentration of Paspalum dilatatum, (a waterlogging- tolerant grass from the Flooding Pampa, Argentina) was affected by waterlogging and P supply and how this related to changes in root-shoot ratio. Under both soil P levels waterlogging reduced root-shoot ratios, but did not reduce P concentration. Thus, uptake of P per unit of root biomass increased under waterlogging. Our second objective was to test three non-exclusive hypotheses about potential mechanisms for this increase in P uptake. We hypothesized that the greater P uptake per unit of root biomass was a consequence of 1) an increase in soil P availability induced by waterlogging; 2) a change in root morphology, and/or 3) an increase in the intrinsic uptake capacity of each unit of root biomass. To test these hypotheses we evaluated a) changes in P availability induced by waterlogging; b) specific root length of waterlogged and control plants, and c) P uptake kinetics in excised roots from waterlogged and control plants. The results supported the three hypotheses. Soil P availability was higher during waterlogging periods, roots of waterlogged plants showed a morphology more favorable to nutrient uptake (finer roots) and these roots showed a higher physiological capacity to absorb P. The results suggest that both soil and plant mechanisms contributed to compensate, in terms of P nutrition, for the reduction in allocation to root growth. The rapid transformation of the P uptake system is likely an advantage for plants inhabiting frequently flooded environments with low P fertility, like the Flooding Pampa. This advantage would be one of the reasons for the increased relative abundance of P. dilatatum in the community after waterlogging periods