Genetic diversity of Rhizobium from nodulating beans grown in a variety of Mediterranean climate soils of Chile
Author
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Baginsky Guerrero, Cecilia
Author
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Brito, Belén
Author
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Scherson Vicencio, Rosa
Author
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Pertuze Concha, Ricardo
Author
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Seguel Seguel, Oscar
Author
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Cañete, Alejandro
Author
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Araneda Tolosa, Cristian
Author
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Johnson, Warren E.
Admission date
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2015-07-08T20:13:11Z
Available date
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2015-07-08T20:13:11Z
Publication date
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2015
Cita de ítem
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Arch Microbiol (2015) 197:419–429
en_US
Identifier
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DOI 10.1007/s00203-014-1067-y
Identifier
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https://repositorio.uchile.cl/handle/2250/131865
General note
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Artículo de publicación ISI
en_US
Abstract
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In spite of potentially being an important source
of rhizobial diversity and a key determinant of common
bean productivity, there is a paucity of data on Rhizobium
genetic variation and species composition in the important
bean producing area of Chile and only one species has been
documented (Rhizobium leguminosarum). In this study, 240
Rhizobium isolates from Torcaza bean (Phaseolus vulgaris L.)
nodules established in the highest bean producing area in Chile
(33°34′S–70°38′W and 37°36′S–71°47′W) were characterized
by PCR-RFLP markers for nodC gene, revealing eight banding
patterns with the polymorphic enzyme Hinf I. The locality
of San Agustín de Aurora in Central Chile (35°32′S–71°29′W)
had the highest level of diversity. Isolates were classified by species using PCR-RFLP markers for 16S rDNA gene and
were confirmed by sequencing an internal fragment of the 16S
rDNA gene. The results confirmed the presence of R. leguminosarum
and three other species of rhizobia nodulating beans
in South Central Chile (R. etli, R. tropici and R. leucaenae).
R. tropici and R. leucaenae showed the least genetic variation
and were most commonly identified in acid soils, while R. etli
was the most common species in slightly acidic to moderately
alkaline soils, with higher levels of organic matter content. R.
leguminosarum was identified in almost all soils, was the most
genetically diverse, and was the most common, being documented
in soils with pH that ranged between 5.3 and 8.2, and
with organic matter content between 2.1 and 4 %.