dc.creatorDi Mauro, Guido
dc.creatorParra, Gonzalo
dc.creatorSantos, Diego Jose
dc.creatorEnrico, Juan Martin
dc.creatorZuil, Sebastian
dc.creatorMurgio, Marcos
dc.creatorZbinden, Facundo
dc.creatorCostanzi, Jerónimo
dc.creatorArias, Norma Monica
dc.creatorCarrio, Alejandro Javier
dc.creatorVissani, Cristian Angel
dc.creatorFuentes, Francisco Horacio
dc.creatorSalvagiotti, Fernando
dc.date.accessioned2022-09-12T12:22:14Z
dc.date.accessioned2023-03-15T14:17:32Z
dc.date.available2022-09-12T12:22:14Z
dc.date.available2023-03-15T14:17:32Z
dc.date.created2022-09-12T12:22:14Z
dc.date.issued2022-10
dc.identifier0378-4290
dc.identifierhttps://doi.org/10.1016/j.fcr.2022.108676
dc.identifierhttp://hdl.handle.net/20.500.12123/12851
dc.identifierhttps://www.sciencedirect.com/science/article/abs/pii/S0378429022002477
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/6215796
dc.description.abstractSoybean genotypes are grouped in maturity groups (MG) based on the response to photoperiod, and a genotype belonging to a particular MG is recommended according to latitude and planting date. From an agronomic viewpoint, an “optimum maturity group” (MGopt) can be defined as the one that maximizes soybean yield in a particular environment, and not necessarily corresponds with the recommended MG based on thermo-photoperiod response. Our objectives were to (i) delineate spatial pattern of MGopt across contrasting environmental conditions for full-season soybean using geostatistics, and (ii) test whether the weather scenario change the spatial distribution of the MGopt. We hypothesized that, for the same region, the MGopt in dry years (i.e. La Niña phase) is larger than in humid years (i.e. El Niño phase). We analyzed multi-environment trials of full-season soybean (1675 site-years) using recent soybean genotypes and management practices across the Southern Cone of America. The MGopt ranged between 3.8 and 7.8 across regions and ENSO phases. The geostatistics approach indicated a spatial MGopt auto-correlation. The map for each ENSO phase indicates zones with contrasting MGopt and independently of ENSO phase, MGopt increased as latitude decreased. Also, for a particular latitude range, MGopt also varied according to longitude, suggesting that its variation can be associated with rainfall pattern and soil types in the region. Our approach delineated the distribution of MGopt for the American Southern Cone and highlighted that the inclusion of ENSO phase is important for guiding farmers MG options at regional scale.
dc.languageeng
dc.publisherElsevier
dc.relationinfo:eu-repograntAgreement/INTA/2019-RIST-E6-I226-001/2019-RIST-E6-I226-001/AR./Red de evaluación de cultivares
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.sourceField Crops Research 287 : 108676 (October 2022)
dc.subjectSoja
dc.subjectTiempo Meteorológico
dc.subjectMadurez
dc.subjectManejo del Cultivo
dc.subjectAmérica del Sur
dc.subjectSoybeans
dc.subjectWeather
dc.subjectMaturity
dc.subjectCrop Management
dc.subjectSouth America
dc.titleDefining soybean maturity group options for contrasting weather scenarios in the American Southern Cone
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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