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a Centro Internacional de Agricultura Tropical (CIAT), A.A. 6713, Cali, Colombia
b South China Agricultural Univ., Guangzhou, PRC
c Univ. of Nebraska, Lincoln, NE, USA
d Univ. of Florida, Hastings, FL, USA
e Pennsylvania State Univ., University Park, PA, USA
* Corresponding author (m.blair{at}cgiar.org)
| ABSTRACT |
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Abbreviations: AFLP, amplified fragment length polymorphism CIM, composite interval mapping cM, centimorgan DW, dry weight HP, high phosphorus LG, linkage group LOD, base 10 algorithm of the likelihood ratio LP, low phosphorus QTL, quantitative trait locus R2, proportion of variance explained by QTL at test site RL, root length SCAR, sequence characterized amplified region RAPD, randomly amplified polymorphic DNA RFLP, restriction fragment length polymorphism RIL, recombinant inbred line TR2, proportion of variance explained for the QTL and the background markers TSP, triple super phosphate
| INTRODUCTION |
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The ability of a plant to access available P under LP conditions depends on its RL and on several other morphological and physiological properties of the root (Raghothama, 1999), including association with arbuscular-mycorrhizal fungi that increase the soil volume from which P can be acquired (Marschner, 1995, p. 889) and root-induced changes in the rhizosphere such as P mobilization by root exudates (Gaume et al., 2001). Superior P acquisition, often referred to as phosphorus-acquisition efficiency, differs from phosphorus-use efficiency, which is the plant's ability to produce yield per unit of acquired P from soil (Lynch and Beebe, 1995; Rao et al., 1999). Understanding the mechanisms and genetic control of phosphorus acquisition and use efficiency and other aspects of LP tolerance would facilitate genetic improvement (Lynch and Beebe, 1995; Rao, 2001). Root architectural traits that enhance topsoil foraging appear to be particularly important for P acquisition efficiency and genotypic adaptation of common bean to LP soils (Lynch and Brown, 1999, 2001). Phosphorus availability regulates many features of root architecture, including adventitious rooting, aerenchyma formation, basal root elongation, basal root-growth angle, lateral rooting, root hair density, and root hair length (Bates and Lynch, 1996; Bonser et al., 1996; Borch et al., 1999; Fan et al., 2003; Liao et al., 2001; Ma et al., 2001a; Miller et al., 2003). These changes appear to act synergistically to enhance P acquisition, by enhancing the quality and quantity of soil foraging, and by reducing the metabolic costs of soil exploration (Lynch and Ho, 2004; Lynch and Brown, 2001; Ma et al., 2001b). Another trait that varies with P supply is specific RL, defined as length of root per unit root weight (Miller et al., 2003). Specific RL is related to root diameter (Fitter, 1985; Eissenstat 1992) and root tissue density (Fan et al., 2003; Ryser, 1996), and is important in determining the metabolic cost of root elongation, an important aspect of efficient soil exploration (Lynch and Ho, 2004). Specific RL varies among species and cultivars (de Willigen and van Noordwijk, 1987), and such differences have been associated with genetic differences in P efficiency (Sattelmacher et al., 1994).
Common bean is the most important food legume for direct human consumption in the world, and most production occurs in Latin America and Africa by resource-poor farmers on infertile tropical soils that are deficient in nutrients, especially P (CIAT, 1992). Genetic studies of common bean have concentrated on resistance to biotic constraints (Kelly et al., 2003), but several abiotic stress tolerances such as drought and LP tolerance have begun to be analyzed through a QTL approach (Schneider et al., 1997; Liao et al., 2004; Yan et al., 2004). Cultivated common bean was domesticated in the tropics and subtropics in at least two independent events (Gepts, 1988) and consists of two major gene pools, one Mesoamerican and one Andean, that display ample DNA polymorphism (Nodari et al., 1992). Differences have been observed in the ability of bean lines and landraces to produce grain under P limiting conditions (Thung, 1991; Youngdahl, 1990; Yan et al., 1995a; Beebe et al., 1997) and in their P acquisition efficiency (Yan et al., 1995b).
The objectives of this study were to identify QTLs for root architectural traits and evaluate their relationship with QTLs for P acquisition efficiency in common bean by analyzing a segregating population of RILs created from an intergene pool cross of common bean involving DOR 364, a genotype that is P inefficient, and G19833, a P-efficient genotype. This population has been used to analyze other LP adaptation traits such as root hair density, acid exudation, and basal root gravitropism (Liao et al., 2004; Yan et al., 2004).
| MATERIALS AND METHODS |
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Field Trials
Two trials were established in the field in Darién, Colombia (1400 m above sea level; 20°C average yearly temperature, Andosol soil type). The native soil P at this site is normally less than 2 mg kg1 (Bray II). One trial was managed with LP levels (6 kg P ha1 as triple super phosphate [TSP] before planting) and the other with HP levels (20 kg P ha1 as TSP in both the season in which the trial was established and 6 mo previously). In both treatments, fertilizer was broadcast and incorporated. Parental genotypes were planted with six repetitions in each trial and 71 RILs for which seed was available were planted with three repetitions in a randomized complete block design. Ten seed were sown per experimental plot, which consisted of single rows 1 m in length and 0.6 m apart. At 35 d after planting, the plants in the extremes of the row were discarded and whole plants in the remaining 0.8 m of row were extracted manually from the soil with root systems conserved in the laboratory in sodium azide (0.02%) at 4°C and aerial parts separated from roots and both oven dried to determine shoot, root, and total DW.
Root Traits of Field-Grown Plants
Two randomly selected segments of 5 to 6 cm in length with attached lateral roots were cut from each conserved root system, and nodules were removed to avoid biasing estimates of root diameter. Samples were stained with neutral red (0.16 g L1), scanned and analyzed with Delta T-Scan software (Delta-T Devices, Burwell, Cambridge, UK). Data obtained were average root diameter and RL, as well as RL per diameter classes. Fragments were oven-dried and weighed to calculate specific RL as RL in meters per gram of root. Specific RL for the root sample were extrapolated to the whole root system on a weightweight basis based on the harvest of the whole root system from the field. This gave us total RL and total length of fine roots (<0.38 mm). Plant tissue was analyzed for P concentration (Murphy and Riley, 1963) to calculate total P accumulation and P content per unit RL.
Root Traits of Greenhouse Grown Plants
Seed of the two parents and 86 F5.7 RILs (including those in the field trial plus an additional 15) were surface sterilized for 1 min in 10% NaOCl before germination. Seed were germinated on germination paper soaked in 0.5 mM CaSO4 in an incubator in the dark at 25°C. Seven days later, uniform seedlings were transplanted to the greenhouse at Pennsylvania State University with an average temperature of 29/20°C (day/night), a relative humidity of 48/83% (day/night), and an average measure of photosynthetically active radiation between 500 and 1000 µmol m2 s1. Plants were grown at a low level of available P (0.2 µM P) in 100-L hydroponic tanks with nutrient solution containing (in mM) 4.5 KNO3, 1.2 NH4NO3, 3.6 Ca(NO3)2, 3.0 MgSO4, 1.2 K2SO4, 1.2 (NH4)2SO4, and (in µM) 30 Fe-EDTA, 4.5 MnSO4, 4.5 ZnSO4, 1.5 CuSO4, 1.5 H3BO3, and 0.4 NH4Mo7O24. The solution was well aerated and the pH was maintained between 5.8 and 6.0 with daily additions of 1.0 M KOH or HCl. Plants were harvested 14 d after transplanting and divided into leaves, stems, and roots. The roots were conserved in 25% ethanol immediately after harvest and then divided into tap and basal roots, and basal roots were counted. The roots were stained with 0.5 mM neutral red dye (Sigma, USA) before being scanned into images with a desk scanner (ScanJet IIc, Hewlett-Packard, USA). Samples were dried and weighed to determine basal root DW, taproot DW, total root DW, specific RL, shoot DW, and total DW. Knowing average root diameter and length surface area was estimated by geometry. From the images, tap RL, basal RL, and total RL were analyzed by computer as described above with the DT-Scan program (Delta T, Inc., Richfield, WI).
Map Construction
DNA was extracted from parental genotypes by a modified Dellaporta method used by Vallejos et al. (1992). Parental polymorphism surveys were prepared by digesting the parental DNA with six restriction enzymes (BamHI, DraI, HindIII, EcoRI, EcoRV, and XbaI) and transferring the digested DNA to Nylon membranes. Southern hybridization was conducted with 101 restriction fragment length polymorphism (RFLP) probes from two common bean genetic maps (Vallejos et al., 1992; Nodari et al., 1993). Fifty probes were chosen based on polymorphism among the parents and map position in the genome and were evaluated on the 86-RIL progeny. Additionally, a selection of 32 microsatellites from Yu et al. (2000) and Blair et al. (2003) were amplified on the DNA of the RILs. Two amplified fragment length polymorphism (AFLP) primer combinations, used previously to produce a large number of bands in common bean (Tohme et al., 1996), were employed to generate 24 additional markers. In addition, sequence characterized amplified region (SCAR) primer pairs developed by Gu et al. (1995) were used to amplify another six bands and a total of 23 10-mer oligonucleotide primers from Operon (Huntsville, AL) were used to generate 124 randomly amplified polymorphic DNA (RAPD) markers. Markers presenting significant segregation distortion were eliminated. A total of 236 markers were used to create the final map, extending a map that was reported previously (Beebe et al., 1998) using the Map Maker (Kintyre, UK) program (Lander et al., 1987). Linkage analysis was conducted initially for the RFLP and microsatellite markers at likelihood of odds (LOD) 6 to anchor the map to the core map of Freyre et al. (1998). Remaining markers were placed individually at a LOD > 3.5 using the Assign and Place functions and confirmed by the Ripple function in Map Maker.
Statistical Analysis
Analyses of variance were performed using the SAS program (SAS Institute, 1987) for both field and greenhouse traits. Since the parental genotypes were planted with more repetitions than the RILs in the field, they were analyzed separately from the RILs in all the trials. Simple linear correlations were calculated among mean values of variables in both the field and greenhouse trials to reveal physiological relationships. The QTLs were detected with CIM analysis, which was performed using the software program QTL Cartographer v. 1.15 (Basten et al., 2005). Since our interest was primarily P accumulation in P-limited conditions, our analyses focused on the association of root variables with P accumulation in the low-P field trial. The following traits were analyzed singly and jointly with P accumulation in the LP treatment: total RL and specific RL in the low-P field trial; basal RL and DW in the greenhouse trial; and tap RL and DW in the greenhouse trial. In the SRmapQTL subprogram, parameters for forwardbackward stepwise regression analysis were a window size of 10 cM, a walkspeed at every 1 cM, and probability thresholds of 0.05 for the partial F test for both marker inclusion or exclusion. The five most significant markers found with the SRmapQTL subprogram were used as background markers in the single and joint CIM analysis realized with the ZmapQTL and JZmapQTL subprograms, respectively. In the single CIM analysis, determination coefficients were calculated for each interval separately (R2) and for each interval given the background markers (TR2). The subprogram Eqtl was used to summarize the significant QTLs found with the previous CIM subprograms. The LOD thresholds were set at a default of 2.5 for both the individual and joint analysis. The LOD thresholds were also calculated through the generation of 1000 permutations (Churchill and Doerge, 1994), to determine an effective significance level of P = 0.05 across the genome. Results were displayed using QTL Cartographer v. 1.21 and represented graphically with standard drawing software, to designate genomic regions that proved to be significant in the analysis described above.
| RESULTS |
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In the greenhouse study, differences were observed between the two parents for root traits that were comparable with differences observed in the field at LP (Table 2). G19833 had significantly higher total RL, basal RL, and DW than DOR364 in the greenhouse. The two parents were not significantly different for specific RL nor for taproot parameters. Unlike the field trial, G19833 had more DW both in shoots and basal roots, as can occur with large-seeded beans at early stages of development (Yan et al., 1995b).
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Phosphorus accumulation of field-grown progenies was correlated with some root traits in both HP and LP environments, including basal root DW and basal RL; however, total RL was only correlated with P accumulation in the HP environment, not in the LP environment (Table 3). Correlations of P accumulation in the field with root data in the greenhouse were significant, especially with basal RL and DW (r = 0.3510.378, P = 0.001), but also with total RL and root DW (data not shown).
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A total of 29 significant QTLs for the individual traits were identified with CIM and were named according to a three-letter convention that was numbered with the LG and QTL order (Table 4). Two significant QTLs were identified for P accumulation in the LP treatment analyzed as an individual trait on LGs B4 and B10 (Fig. 1 ). The QTLs for RL and for specific RL were found in the same regions as these two loci, respectively. Different QTLs were identified for P accumulation, RL and specific RL in the HP treatment than in the LP treatment. For example, a very significant QTL for P accumulation in the HP environment was found on LG B02 at a site that did not contain QTLs for other traits in the LP environment. Similarly, the QTLs for specific RL in the high-P environment were on separate LGs compared with the QTLs for this trait in the low-P environment. On the other hand, the QTLs for RL on LGs B4 and B7 in the HP environment were in equivalent positions to the QTLs for this same trait on these LGs for the LP environment. A total of three additional RL, three seed weight, two basal RL, three basal root DW, three specific RL, one taproot RL, and three taproot DW QTLs were also identified on six additional LGs, B1, B3, B7, B8, B9, and B11, in the greenhouse environment. One of the QTLs for specific RL in the greenhouse was also linked to a QTL for the same trait in the HP environment on LG B7. Another QTL for specific RL in the greenhouse was in the same position on LG B10 as a QTL for specific RL in the LP environment. Quantitative trait loci for different traits were also located together at similar regions of the genome. For example, regions on LGs B3 and B10 contributed simultaneously to both basal root DW and length, while other associations are described further below. The highest LOD score for any QTL was 7.5, although QTLs for P accumulation tended to be of lower significance. The determination coefficients for the QTLs identified by individual CIM analysis ranged from 8.9 to 25.0% individually (R2), and from 41.8 to 66.0% when evaluated with background markers (TR2) (Table 4). All QTLs had markers within 5 cM of the highest LOD peak (Fig. 1).
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In the joint QTL analysis, CIM was used to identify regions of the genome where interactions between P accumulation under LP conditions and other traits were significant. Results of three of these analyses (with basal RL in the greenhouse; specific RL in the field; and total RL in the field) are presented. The joint analysis of traits identified not only the QTLs on B04 and B10 which directly influenced P accumulation in the LP treatment, but also several others where there was an association between P accumulation in the field and specific root traits. Quantitative trait loci regions for P accumulation were most consistently associated with basal root DW and length in the greenhouse, and with RL in field. For example, a QTL on LG B04, close to the RAPD marker P903G, was associated with increased P accumulation in the LP treatment, while the joint analysis of this trait plus basal RL in the greenhouse or total RL in the LP field resulted in more significant QTLs close to the same marker (peak LOD = 3.7) compared with the individual analysis (peak LOD = 3.1). Similar relationships were inferred from the joint analysis of P accumulation in the LP trial and basal or total RL traits, which showed regions within LGs B03, B07, and B11 that had significant QTLs (these latter two LGs with two separate regions each).
A positive relationship between specific RL and P accumulation in the LP trial was uncovered by the joint QTL analysis, in which we found significant regions on B04 and B11 for this combination of traits. The region on LG B04 was interesting because it was also significant for the combined analysis of basal roots plus P accumulation in the LP treatment, suggesting that basal roots and total RL contributed to finer roots and greater specific RL. At all of these loci, the increased effect of the individual traits was derived from G19833. For three more regions on B08, significance in the joint analysis was not greater than that of specific RL alone, and the positive effect on specific RL was derived from DOR 364. In still another region on B10, the relationship of specific RL and P accumulation was different. Here, the segment that contributed to specific RL was not associated with either basal root development or taproot development, but coincided with Pup10.1, the most important QTL for P accumulation under the LP trial (Fig. 2 ). Greater significance of this QTL was observed in the joint analysis (peak LOD = 3.8) than for P accumulation alone (peak LOD = 3.15); thus, joint analysis strengthened the conclusion suggested by single trait analysis that thicker roots were indeed associated with greater P accumulation efficiency at this QTL.
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| DISCUSSION |
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The two parental genotypes used in this study contrasted for root traits and LP adaptation (P efficiency). Previous studies show that G19833 has superior growth and yield in LP soil field trials than DOR 364 (CIAT, 1991, p. 161169; Liao et al., 2004), and superior growth under LP stress in soil, P-buffered sand, and growth pouches in controlled environments (Liao et al., 2001; Liao et al., 2004; Yan et al., 2004). The distinct evolutionary background of these two materials, with DOR364 derived from the Mesoamerican gene pool and G19833 a landrace of the Andean gene pool, may have contributed to the physiological differences that were observed between them. G19833 has greater expression of several root traits that contribute to efficient P acquisition in LP environments, including greater root hair length and density (Yan et al., 2004), greater root exudation of acid (Yan et al., 2004), more shallow deployment of basal roots (Liao et al., 2004), greater cortical aerenchyma formation (Fan et al., 2003), and greater production of adventitious roots (Miller et al., 2003). These traits confer on G19833 the ability to exploit topsoil P resources more effectively than DOR 364, which is an important aspect of LP adaptation in bean (Lynch and Brown, 2001), and reduce the metabolic cost of soil exploration in G19833, which is another important component of LP adaptation in bean (Lynch and Ho, 2004). Data presented here are consistent with these earlier observations, showing that among RILs descended from G19833 and DOR364, P acquisition in the field is linked with root growth, and specifically with basal root development and specific root length. In this study, while RL in the field had low correlations with P accumulation, perhaps because of variability in plant development under field conditions, or error introduced in the extraction of roots from soil, the traits basal root DW and length in the greenhouse hydroponic trial presented higher correlations with total RL and P accumulation in the low and HP field environments. The correlation of root traits expressed early in plant development, such as basal roots with eventual yield under LP conditions, is consistent with earlier reports that basal root angle of young seedlings is well correlated with field performance under LP conditions (Bonser et al., 1996; Rachier et al., 1998). Basal roots emerge from the primary root within 1 wk of germination, and establish the structural scaffold for the development of the majority of the mature root system under normal circumstances. Basal root development in seedlings may therefore be useful indicators of root development in the field, as shown here. It is noteworthy that as in the report by Bonser et al. (1996), basal root growth as assessed in a controlled environment has meaningful correlation with field performance despite the well-known phenotypic plasticity of root traits.
Quantitative trait locus analysis revealed a relationship of P accumulation with greater RL in the field and with basal root DW or RL in the greenhouse. This latter relationship was consistent across six different chromosomal regions on five LGs. Therefore, QTL analysis was in agreement with phenotypic correlations that associated P accumulation with basal roots and supported the conclusion that basal roots play a very important role in P accumulation by bean. This could be explained by the hypothesis that basal roots tend to explore more superficial soil layers, where soil P availability is greater than in subsoil layers (Lynch and Brown, 2001). Quantitative trait locus analysis also identified genetic linkage between the three QTLs for seed weight and several root trait QTLs. This may explain a relationship between seed size and LP tolerance that was noted previously, and was attributed to greater seed P and carbon reserves of large-seeded beans, which resulted in better growth early in plant development (Yan et al., 1995b). The question of an association between seed size QTLs and root trait QTLs deserves more attention, especially regarding Andean beans that tend to have larger seed.
Specific RL, as a measure of root fineness, is generally expected to be positively correlated with efficient P acquisition, since theoretically finer roots should be more efficient in exploring the soil per unit of metabolic investment in root biomass (Eissenstat, 1992). Although finer roots may incur tradeoffs in terms of increased root mortality and susceptibility to pathogens and herbivores, a recent study of root longevity and turnover in bean under LP stress found low rates of root mortality (Fisher et al., 2002), suggesting that such tradeoffs are not of central importance in common beans. In addition to root diameter, specific RL could be influenced by anatomical traits that change the relationship of root volume and root weight. Cortical aerenchyma formation is particularly interesting in this regard, since LP stress stimulates aerenchyma formation in bean, thereby reducing the metabolic costs of soil exploration, and since G19833 has more cortical aerenchyma under P stress than DOR364 (Fan et al., 2003). Another factor influencing bulk root system specific RL is root architecture and branching. The root system is composed of several distinct types of roots, including the taproot, basal roots, adventitious roots, and their laterals, which have substantially different diameters, tissue densities, and therefore specific RL (Lynch and van Beem, 1993; Miller et al., 2003) which could also have contributed to bulk differences in specific RL.
In the QTL analysis we found contrasting effects of specific RL between genotypes from the two gene pools of common beans. For at least two QTLs, greater specific RL contributed to P accumulation as expected, but at other QTLs its effect was null, or even negative, as in the case of the QTL Srl10.1 on B10. The relationship of specific RL and P accumulation at this locus was suggestive of a pleiotropic QTL or cluster of linked QTLs that would control both traits and that the alleles for thicker roots were associated with the alleles for increased P acquisition. This implies a different mechanism for P accumulation in DOR364 than in G19833, whereby DOR364 tends to express greater P accumulation per unit RL than G19833. This effect was not significant between the parents, but the progenies did show different amounts of P accumulation per unit RL, suggesting that this trait had a genetic and physiological basis. The efficiency of fine roots vs. course roots per unit of P accumulation and the mechanism of P accumulation in DOR364 require additional study to determine the most appropriate root structure at a given P level. The effect of longer rooting systems appears to be important for P accumulation as suggested by the association of the Pup4.1 QTL with RL QTLs identified on LG B4 for both high and LP environments. The positive allele for all of these QTLs was derived from G19833 the more LP tolerant parent suggesting that this region of the genome can be used for improvement of LP tolerance. The relationship of RL QTLs to specific RL QTLs that were found in the same regions of the genome also would be of interest to analyze in greater detail to determine if longer root systems are associated with finer rooting.
Apart from the relationship of these root traits to P accumulation, a more general observation concerns the complexity of root systems and their genetic control. The present study offers a comparison of QTL mapping positions for several root traits in bean that have not been reported previously, and identifies a total of 26 individual QTLs in 15 different regions of the genome spread across nine LGs which affect root traits. Some QTLs were associated with both basal and taproots, and others only with one or the other, while some QTLs for these traits were associated with specific RL and others were not. Quantitative trait loci for P accumulation in the LP environment on LGs B4 and B10 were associated with QTLs for some of these root parameters, especially with QTLs for total and specific RL, while another QTL for P accumulation in the HP environment on LG B2 was not associated with any of the root trait QTLs. Additional QTLs for P accumulation may be explained by basal root gravitropism, resulting in a shallower root system that may enhance root exploration of the surface soil horizons where P is concentrated (Bonser et al., 1996; Liao et al., 1999, 2004) or root hair and root exudate traits that also play an important role in P accumulation (Hinsinger 2001; Holford 1997; Yan et al., 2004). Apart from an understanding of physiological mechanisms of LP tolerance, the molecular markers identified in this study could be useful potential tools for marker assisted selection in breeding programs to select indirectly for these root traits that are difficult to evaluate in large populations. In this regard, this study will allow the pyramiding of root trait QTLs and especially the two P accumulation QTLs into a single genetic background through introgression breeding.
| ACKNOWLEDGMENTS |
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Received for publication March 15, 2005.
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