C-14-assimilate partitioning within white clover plant-soil system: effects of photoperiod temperature treatments and defoliation

Citation
C. Todorovic et al., C-14-assimilate partitioning within white clover plant-soil system: effects of photoperiod temperature treatments and defoliation, EUR J AGRON, 11(1), 1999, pp. 13-21
Citations number
38
Categorie Soggetti
Agriculture/Agronomy
Journal title
EUROPEAN JOURNAL OF AGRONOMY
ISSN journal
11610301 → ACNP
Volume
11
Issue
1
Year of publication
1999
Pages
13 - 21
Database
ISI
SICI code
1161-0301(199906)11:1<13:CPWWCP>2.0.ZU;2-T
Abstract
Shoots of white clover plants were pulse-labelled with (CO2)-C-14 in order to establish the partitioning of recently assimilated carbon among the diff erent parts of the plant-soil system with special interest in below-ground compartments. The C-14-partitioning did not change significantly after 24 h chase period. Leaves and stolons contained more than half of the total rad ioactivity recovered (%TRR). Soil residues (microbial biomass and non-metab olised rhizodeposits) accounted for 7%TRR and rhizosphere CO2 was 25%TRR. I n order to investigate seasonal effects on assimilate partitioning below gr ound, we compared low photoperiod and day/night temperature conditions (10 h-20 degrees C/18 degrees C, PTL treatment) with high photoperiod and day/n ight temperature conditions (16 h-25 degrees C/20 degrees C, PTH treatment) . Plants of PTH conditions favoured C-14-assimilate partitioning to leaves at the expense of storage organs such as stolons and roots. This was suppor ted by distribution of the relative specific activity (RSA) which indicated a significant higher activity of leaves compared to roots. The reduction o f C-14 allocated to roots (from 11%TRR in PTL treatment to 7%TRR in PTH con ditions) was accompanied by a reduction of C-14 found in rhizosphere CO2 (f rom 25%TRR to 12%TRR) and in soil residues (from 7%TRR to 3%TRR). This indi cated that rhizodeposition of recently fixed carbon is correlated to C allo cation to roots. A moderate defoliation (27% of leaf biomass removed) did n ot modify C-14-partitioning within the plant-soil system. A severe defoliat ion (51% of leaf biomass removed) increased C-14 allocated to remaining lea ves from 28%TRR to 37%TRR at the expense of stolons. Partitioning of labell ed assimilates to below ground remained unchanged. It is suggested that the age of a plant strongly influences its response to leaf removal. (C) 1999 Elsevier Science B.V. All rights reserved.