{"title":"Are There Wheat Cultivars Allowing Enhanced Carbon Allocation to Soils?","authors":"V. Chaplot, I. Mathew, A. Clulow, H. Shimelis","doi":"10.3390/applbiosci2010010","DOIUrl":null,"url":null,"abstract":"The transfer of atmospheric carbon (C) in soils is a possible strategy for climate change mitigation and for restoring land productivity. While some studies have compared the ability of existing crops to allocate C into the soil, the genetic variations between crop genotypes have received less attention. The objective of this study was to compare the allocation to the soil of atmospheric C by genetically diverse wheat genotypes under different scenarios of soil water availability. The experiments were set up under open-field and greenhouse conditions with 100 wheat genotypes sourced from the International Maize and Wheat Improvement Centre and grown at 25% (drought stressed) and 75% (non-stressed) field capacity, using an alpha lattice design with 10 incomplete blocks and 10 genotypes per block. The genotypes were analyzed for grain yield (GY), plant shoot and root biomass (SB and RB, respectively) and C content, and stocks in plant parts. Additionally, 13C pulse labeling was performed during the crop growth period of 10 selected genotypes for assessing soil C inputs. The average GY varied from 75 to 4696 g m−2 and total plant biomass (PB) from 1967 to 13,528 g m−2. The plant C stocks ranged from 592 to 1109 g C m−2 (i.e., an 87% difference) under drought condition and between 1324 and 2881 g C m−2 (i.e., 117%) under well-watered conditions. Atmospheric C transfer to the soil only occurred under well-drained conditions and increased with the increase in the root to shoot ratio for C stocks (r = 0.71). Interestingly, the highest transfer to the soil was found for LM-26 and LM-47 (13C/12C of 7.6 and 6.5 per mille, respectively) as compared to LM-70 and BW-162 (0.75; 0.85). More is to be done to estimate the differences in C fluxes to the soil over entire growing seasons and to assess the long-term stabilization of the newly allocated C. Future research studies also need to identify genomic regions associated with GY and soil C transfer to enable the breeding of “carbon-superior” cultivars.","PeriodicalId":14998,"journal":{"name":"Journal of Applied Biosciences","volume":"92 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2023-03-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Applied Biosciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3390/applbiosci2010010","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
The transfer of atmospheric carbon (C) in soils is a possible strategy for climate change mitigation and for restoring land productivity. While some studies have compared the ability of existing crops to allocate C into the soil, the genetic variations between crop genotypes have received less attention. The objective of this study was to compare the allocation to the soil of atmospheric C by genetically diverse wheat genotypes under different scenarios of soil water availability. The experiments were set up under open-field and greenhouse conditions with 100 wheat genotypes sourced from the International Maize and Wheat Improvement Centre and grown at 25% (drought stressed) and 75% (non-stressed) field capacity, using an alpha lattice design with 10 incomplete blocks and 10 genotypes per block. The genotypes were analyzed for grain yield (GY), plant shoot and root biomass (SB and RB, respectively) and C content, and stocks in plant parts. Additionally, 13C pulse labeling was performed during the crop growth period of 10 selected genotypes for assessing soil C inputs. The average GY varied from 75 to 4696 g m−2 and total plant biomass (PB) from 1967 to 13,528 g m−2. The plant C stocks ranged from 592 to 1109 g C m−2 (i.e., an 87% difference) under drought condition and between 1324 and 2881 g C m−2 (i.e., 117%) under well-watered conditions. Atmospheric C transfer to the soil only occurred under well-drained conditions and increased with the increase in the root to shoot ratio for C stocks (r = 0.71). Interestingly, the highest transfer to the soil was found for LM-26 and LM-47 (13C/12C of 7.6 and 6.5 per mille, respectively) as compared to LM-70 and BW-162 (0.75; 0.85). More is to be done to estimate the differences in C fluxes to the soil over entire growing seasons and to assess the long-term stabilization of the newly allocated C. Future research studies also need to identify genomic regions associated with GY and soil C transfer to enable the breeding of “carbon-superior” cultivars.
土壤中大气碳(C)的转移是减缓气候变化和恢复土地生产力的一种可能战略。虽然一些研究比较了现有作物将碳分配到土壤中的能力,但作物基因型之间的遗传差异受到的关注较少。本研究的目的是比较不同小麦基因型在不同土壤水分有效性条件下对土壤大气碳的分配。试验在露天和温室条件下进行,选用国际玉米和小麦改良中心提供的100种小麦基因型,在25%(干旱胁迫)和75%(非干旱胁迫)的田间容量下种植,采用α晶格设计,10个不完整块,每个块10个基因型。对籽粒产量(GY)、茎部生物量(SB)和根系生物量(RB)、C含量和植株各部位储量进行了基因型分析。此外,在作物生育期对10个选定的基因型进行13C脉冲标记,以评估土壤C输入。平均生物量为75 ~ 4696 g m−2,总生物量(PB)为1967 ~ 13528 g m−2。干旱条件下植物C储量为592 ~ 1109 g C m−2(差异87%),丰水条件下为1324 ~ 2881 g C m−2(差异117%)。大气碳向土壤的转移只发生在排水良好的条件下,并且随着碳砧木根冠比的增加而增加(r = 0.71)。有趣的是,与LM-70和BW-162相比,LM-26和LM-47的土壤转移量最高(13C/12C分别为7.6和6.5 /英里)。0.85)。要估计整个生长季节土壤碳通量的差异,并评估新分配的碳的长期稳定性,还需要做更多的工作。未来的研究还需要确定与GY和土壤碳转移相关的基因组区域,以便培育“碳优势”品种。