Decoupling of soil nutrients cycles as a function of aridity in global drylands
- Autores
- Delgado Baquerizo, Manuel; Maestre, Fernando T.; Gallardo, Antonio; Bowker, Matthew A.; Wallenstein, Matthew D.; Bran, Donaldo Eduardo; Gatica, Mario Gabriel; Hepper, Estela Noemí; Prina, Anibal Oscar; Pucheta, Eduardo Raúl; Huber Sannwald, Elisabeth; Jankju, Mohammad; Liu, Jushan; Mau, Rebecca L.; Miriti, Maria; Monerris, Jorge; Naseri, Kamal; Noumi, Zouhaier; Polo, Vicente; Ramírez Collantes, David A.; Romão, Roberto; Tighe, Matthew; Torres, Duilio; Torres Díaz, Cristian; Ungar, Eugene D.; Val, James; Wamiti, Wanyoike; Wang, Deli; Zaady, Eli
- Año de publicación
- 2013
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The biogeochemical cycles of carbon (C), nitrogen (N) and phosphorus (P) are interlinked by primary production, respiration and decomposition in terrestrial ecosystems. It has been suggested that the C, N and P cycles could become uncoupled under rapid climate change because of the different degrees of control exerted on the supply of these elements by biological and geochemical processes. Climatic controls on biogeochemical cycles are particularly relevant in arid, semi-arid and dry sub-humid ecosystems (drylands) because their biological activity is mainly driven by water availability. The increase in aridity predicted for the twenty-first century in many drylands worldwide may therefore threaten the balance between these cycles, differentially affecting the availability of essential nutrients. Here we evaluate how aridity affects the balance between C, N and P in soils collected from 224 dryland sites from all continents except Antarctica. Wefind a negative effect of aridity on the concentration of soil organic C and total N, but a positive effect on the concentration of inorganic P. Aridity is negatively related to plant cover, which may favour the dominance of physical processes such as rock weathering, a major source of P to ecosystems, over biological processes that provide more C and N, such as litter decomposition1. Our findings suggest that any predicted increase in aridity with climate change will probably reduce the concentrations of N and C in global drylands, but increase that of P. These changes would uncouple the C, N and P cycles in drylands and could negatively affect the provision of key services provided by these ecosystems.
Fil: Delgado Baquerizo, Manuel. Universidad Pablo de Olavide; España. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; España
Fil: Maestre, Fernando T.. Universidad Pablo de Olavide; España. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; España
Fil: Gallardo, Antonio. Universidad Pablo de Olavide; España
Fil: Bowker, Matthew A.. No especifíca;
Fil: Wallenstein, Matthew D.. Northern Arizona University; Estados Unidos
Fil: Bran, Donaldo Eduardo. Instituto Nacional de Tecnología Agropecuaria. Centro Regional Patagonia Norte. Estación Experimental Agropecuaria San Carlos de Bariloche; Argentina. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; España
Fil: Gatica, Mario Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales; Argentina
Fil: Hepper, Estela Noemí. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Pampa. Facultad de Agronomía; Argentina
Fil: Prina, Anibal Oscar. Universidad Nacional de La Pampa. Facultad de Agronomía; Argentina
Fil: Pucheta, Eduardo Raúl. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales; Argentina
Fil: Huber Sannwald, Elisabeth. Instituto Potosino de Investigación Científica y Tecnológica; México
Fil: Jankju, Mohammad. Ferdowsi University of Mashhad; Irán
Fil: Liu, Jushan. Northeast Normal University. Institute of Grassland Science,; China
Fil: Mau, Rebecca L.. Northern Arizona University; Estados Unidos
Fil: Miriti, Maria. Ohio State University; Estados Unidos
Fil: Monerris, Jorge. Université du Québec a Montreal; Canadá
Fil: Naseri, Kamal. Ferdowsi University of Mashhad; Irán
Fil: Noumi, Zouhaier. Université de Sfax; Túnez
Fil: Polo, Vicente. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; España
Fil: Ramírez Collantes, David A.. International Potato Center; Perú
Fil: Romão, Roberto. Universidade Estadual de Feira de Santana. Departamento de Ciencias Biológica, Herbario; Brasil
Fil: Tighe, Matthew. University of New England; Australia
Fil: Torres, Duilio. Universidad Centroccidental ‘‘Lisandro Alvarado’’; Venezuela
Fil: Torres Díaz, Cristian. Universidad del Bio Bio. Facultad de Ciencias. Departamento de Ciencias Básicas. Laboratorio de Genómica y Biodiversidad; Chile
Fil: Ungar, Eugene D.. The Volcani Center. Agricultural Research Organization. Institute of Plant Sciences; Israel
Fil: Val, James. Office of Environment and Heritage; Australia
Fil: Wamiti, Wanyoike. National Museums of Kenya. Zoology Department; Kenia
Fil: Wang, Deli. Northeast Normal University. Institute of Grassland Science; China
Fil: Zaady, Eli. Gilat Research Center; Israel - Materia
-
Drylands
Earth Sciences
Biogeochemistry
Carbon, Nitrogen And Phosphorus - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/29204
Ver los metadatos del registro completo
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Decoupling of soil nutrients cycles as a function of aridity in global drylandsDelgado Baquerizo, ManuelMaestre, Fernando T.Gallardo, AntonioBowker, Matthew A.Wallenstein, Matthew D.Bran, Donaldo EduardoGatica, Mario GabrielHepper, Estela NoemíPrina, Anibal OscarPucheta, Eduardo RaúlHuber Sannwald, ElisabethJankju, MohammadLiu, JushanMau, Rebecca L.Miriti, MariaMonerris, JorgeNaseri, KamalNoumi, ZouhaierPolo, VicenteRamírez Collantes, David A.Romão, RobertoTighe, MatthewTorres, DuilioTorres Díaz, CristianUngar, Eugene D.Val, JamesWamiti, WanyoikeWang, DeliZaady, EliDrylandsEarth SciencesBiogeochemistryCarbon, Nitrogen And Phosphorushttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The biogeochemical cycles of carbon (C), nitrogen (N) and phosphorus (P) are interlinked by primary production, respiration and decomposition in terrestrial ecosystems. It has been suggested that the C, N and P cycles could become uncoupled under rapid climate change because of the different degrees of control exerted on the supply of these elements by biological and geochemical processes. Climatic controls on biogeochemical cycles are particularly relevant in arid, semi-arid and dry sub-humid ecosystems (drylands) because their biological activity is mainly driven by water availability. The increase in aridity predicted for the twenty-first century in many drylands worldwide may therefore threaten the balance between these cycles, differentially affecting the availability of essential nutrients. Here we evaluate how aridity affects the balance between C, N and P in soils collected from 224 dryland sites from all continents except Antarctica. Wefind a negative effect of aridity on the concentration of soil organic C and total N, but a positive effect on the concentration of inorganic P. Aridity is negatively related to plant cover, which may favour the dominance of physical processes such as rock weathering, a major source of P to ecosystems, over biological processes that provide more C and N, such as litter decomposition1. Our findings suggest that any predicted increase in aridity with climate change will probably reduce the concentrations of N and C in global drylands, but increase that of P. These changes would uncouple the C, N and P cycles in drylands and could negatively affect the provision of key services provided by these ecosystems.Fil: Delgado Baquerizo, Manuel. Universidad Pablo de Olavide; España. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; EspañaFil: Maestre, Fernando T.. Universidad Pablo de Olavide; España. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; EspañaFil: Gallardo, Antonio. Universidad Pablo de Olavide; EspañaFil: Bowker, Matthew A.. No especifíca;Fil: Wallenstein, Matthew D.. Northern Arizona University; Estados UnidosFil: Bran, Donaldo Eduardo. Instituto Nacional de Tecnología Agropecuaria. Centro Regional Patagonia Norte. Estación Experimental Agropecuaria San Carlos de Bariloche; Argentina. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; EspañaFil: Gatica, Mario Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales; ArgentinaFil: Hepper, Estela Noemí. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Pampa. Facultad de Agronomía; ArgentinaFil: Prina, Anibal Oscar. Universidad Nacional de La Pampa. Facultad de Agronomía; ArgentinaFil: Pucheta, Eduardo Raúl. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales; ArgentinaFil: Huber Sannwald, Elisabeth. Instituto Potosino de Investigación Científica y Tecnológica; MéxicoFil: Jankju, Mohammad. Ferdowsi University of Mashhad; IránFil: Liu, Jushan. Northeast Normal University. Institute of Grassland Science,; ChinaFil: Mau, Rebecca L.. Northern Arizona University; Estados UnidosFil: Miriti, Maria. Ohio State University; Estados UnidosFil: Monerris, Jorge. Université du Québec a Montreal; CanadáFil: Naseri, Kamal. Ferdowsi University of Mashhad; IránFil: Noumi, Zouhaier. Université de Sfax; TúnezFil: Polo, Vicente. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; EspañaFil: Ramírez Collantes, David A.. International Potato Center; PerúFil: Romão, Roberto. Universidade Estadual de Feira de Santana. Departamento de Ciencias Biológica, Herbario; BrasilFil: Tighe, Matthew. University of New England; AustraliaFil: Torres, Duilio. Universidad Centroccidental ‘‘Lisandro Alvarado’’; VenezuelaFil: Torres Díaz, Cristian. Universidad del Bio Bio. Facultad de Ciencias. Departamento de Ciencias Básicas. Laboratorio de Genómica y Biodiversidad; ChileFil: Ungar, Eugene D.. The Volcani Center. Agricultural Research Organization. Institute of Plant Sciences; IsraelFil: Val, James. Office of Environment and Heritage; AustraliaFil: Wamiti, Wanyoike. National Museums of Kenya. Zoology Department; KeniaFil: Wang, Deli. Northeast Normal University. Institute of Grassland Science; ChinaFil: Zaady, Eli. Gilat Research Center; IsraelNature Publishing Group2013-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/29204Delgado Baquerizo, Manuel; Maestre, Fernando T.; Gallardo, Antonio; Bowker, Matthew A.; Wallenstein, Matthew D.; et al.; Decoupling of soil nutrients cycles as a function of aridity in global drylands; Nature Publishing Group; Nature; 502; 7473; 10-2013; 672-6760028-0836CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://www.nature.com/nature/journal/v502/n7473/full/nature12670.htmlinfo:eu-repo/semantics/altIdentifier/doi/10.1038/nature12670info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:40:59Zoai:ri.conicet.gov.ar:11336/29204instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:40:59.493CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Decoupling of soil nutrients cycles as a function of aridity in global drylands |
title |
Decoupling of soil nutrients cycles as a function of aridity in global drylands |
spellingShingle |
Decoupling of soil nutrients cycles as a function of aridity in global drylands Delgado Baquerizo, Manuel Drylands Earth Sciences Biogeochemistry Carbon, Nitrogen And Phosphorus |
title_short |
Decoupling of soil nutrients cycles as a function of aridity in global drylands |
title_full |
Decoupling of soil nutrients cycles as a function of aridity in global drylands |
title_fullStr |
Decoupling of soil nutrients cycles as a function of aridity in global drylands |
title_full_unstemmed |
Decoupling of soil nutrients cycles as a function of aridity in global drylands |
title_sort |
Decoupling of soil nutrients cycles as a function of aridity in global drylands |
dc.creator.none.fl_str_mv |
Delgado Baquerizo, Manuel Maestre, Fernando T. Gallardo, Antonio Bowker, Matthew A. Wallenstein, Matthew D. Bran, Donaldo Eduardo Gatica, Mario Gabriel Hepper, Estela Noemí Prina, Anibal Oscar Pucheta, Eduardo Raúl Huber Sannwald, Elisabeth Jankju, Mohammad Liu, Jushan Mau, Rebecca L. Miriti, Maria Monerris, Jorge Naseri, Kamal Noumi, Zouhaier Polo, Vicente Ramírez Collantes, David A. Romão, Roberto Tighe, Matthew Torres, Duilio Torres Díaz, Cristian Ungar, Eugene D. Val, James Wamiti, Wanyoike Wang, Deli Zaady, Eli |
author |
Delgado Baquerizo, Manuel |
author_facet |
Delgado Baquerizo, Manuel Maestre, Fernando T. Gallardo, Antonio Bowker, Matthew A. Wallenstein, Matthew D. Bran, Donaldo Eduardo Gatica, Mario Gabriel Hepper, Estela Noemí Prina, Anibal Oscar Pucheta, Eduardo Raúl Huber Sannwald, Elisabeth Jankju, Mohammad Liu, Jushan Mau, Rebecca L. Miriti, Maria Monerris, Jorge Naseri, Kamal Noumi, Zouhaier Polo, Vicente Ramírez Collantes, David A. Romão, Roberto Tighe, Matthew Torres, Duilio Torres Díaz, Cristian Ungar, Eugene D. Val, James Wamiti, Wanyoike Wang, Deli Zaady, Eli |
author_role |
author |
author2 |
Maestre, Fernando T. Gallardo, Antonio Bowker, Matthew A. Wallenstein, Matthew D. Bran, Donaldo Eduardo Gatica, Mario Gabriel Hepper, Estela Noemí Prina, Anibal Oscar Pucheta, Eduardo Raúl Huber Sannwald, Elisabeth Jankju, Mohammad Liu, Jushan Mau, Rebecca L. Miriti, Maria Monerris, Jorge Naseri, Kamal Noumi, Zouhaier Polo, Vicente Ramírez Collantes, David A. Romão, Roberto Tighe, Matthew Torres, Duilio Torres Díaz, Cristian Ungar, Eugene D. Val, James Wamiti, Wanyoike Wang, Deli Zaady, Eli |
author2_role |
author author author author author author author author author author author author author author author author author author author author author author author author author author author author |
dc.subject.none.fl_str_mv |
Drylands Earth Sciences Biogeochemistry Carbon, Nitrogen And Phosphorus |
topic |
Drylands Earth Sciences Biogeochemistry Carbon, Nitrogen And Phosphorus |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The biogeochemical cycles of carbon (C), nitrogen (N) and phosphorus (P) are interlinked by primary production, respiration and decomposition in terrestrial ecosystems. It has been suggested that the C, N and P cycles could become uncoupled under rapid climate change because of the different degrees of control exerted on the supply of these elements by biological and geochemical processes. Climatic controls on biogeochemical cycles are particularly relevant in arid, semi-arid and dry sub-humid ecosystems (drylands) because their biological activity is mainly driven by water availability. The increase in aridity predicted for the twenty-first century in many drylands worldwide may therefore threaten the balance between these cycles, differentially affecting the availability of essential nutrients. Here we evaluate how aridity affects the balance between C, N and P in soils collected from 224 dryland sites from all continents except Antarctica. Wefind a negative effect of aridity on the concentration of soil organic C and total N, but a positive effect on the concentration of inorganic P. Aridity is negatively related to plant cover, which may favour the dominance of physical processes such as rock weathering, a major source of P to ecosystems, over biological processes that provide more C and N, such as litter decomposition1. Our findings suggest that any predicted increase in aridity with climate change will probably reduce the concentrations of N and C in global drylands, but increase that of P. These changes would uncouple the C, N and P cycles in drylands and could negatively affect the provision of key services provided by these ecosystems. Fil: Delgado Baquerizo, Manuel. Universidad Pablo de Olavide; España. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; España Fil: Maestre, Fernando T.. Universidad Pablo de Olavide; España. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; España Fil: Gallardo, Antonio. Universidad Pablo de Olavide; España Fil: Bowker, Matthew A.. No especifíca; Fil: Wallenstein, Matthew D.. Northern Arizona University; Estados Unidos Fil: Bran, Donaldo Eduardo. Instituto Nacional de Tecnología Agropecuaria. Centro Regional Patagonia Norte. Estación Experimental Agropecuaria San Carlos de Bariloche; Argentina. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; España Fil: Gatica, Mario Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales; Argentina Fil: Hepper, Estela Noemí. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Pampa. Facultad de Agronomía; Argentina Fil: Prina, Anibal Oscar. Universidad Nacional de La Pampa. Facultad de Agronomía; Argentina Fil: Pucheta, Eduardo Raúl. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales; Argentina Fil: Huber Sannwald, Elisabeth. Instituto Potosino de Investigación Científica y Tecnológica; México Fil: Jankju, Mohammad. Ferdowsi University of Mashhad; Irán Fil: Liu, Jushan. Northeast Normal University. Institute of Grassland Science,; China Fil: Mau, Rebecca L.. Northern Arizona University; Estados Unidos Fil: Miriti, Maria. Ohio State University; Estados Unidos Fil: Monerris, Jorge. Université du Québec a Montreal; Canadá Fil: Naseri, Kamal. Ferdowsi University of Mashhad; Irán Fil: Noumi, Zouhaier. Université de Sfax; Túnez Fil: Polo, Vicente. Universidad Rey Juan Carlos. Departamento de Biología y Geología. Área de Biodiversidad y Conservación; España Fil: Ramírez Collantes, David A.. International Potato Center; Perú Fil: Romão, Roberto. Universidade Estadual de Feira de Santana. Departamento de Ciencias Biológica, Herbario; Brasil Fil: Tighe, Matthew. University of New England; Australia Fil: Torres, Duilio. Universidad Centroccidental ‘‘Lisandro Alvarado’’; Venezuela Fil: Torres Díaz, Cristian. Universidad del Bio Bio. Facultad de Ciencias. Departamento de Ciencias Básicas. Laboratorio de Genómica y Biodiversidad; Chile Fil: Ungar, Eugene D.. The Volcani Center. Agricultural Research Organization. Institute of Plant Sciences; Israel Fil: Val, James. Office of Environment and Heritage; Australia Fil: Wamiti, Wanyoike. National Museums of Kenya. Zoology Department; Kenia Fil: Wang, Deli. Northeast Normal University. Institute of Grassland Science; China Fil: Zaady, Eli. Gilat Research Center; Israel |
description |
The biogeochemical cycles of carbon (C), nitrogen (N) and phosphorus (P) are interlinked by primary production, respiration and decomposition in terrestrial ecosystems. It has been suggested that the C, N and P cycles could become uncoupled under rapid climate change because of the different degrees of control exerted on the supply of these elements by biological and geochemical processes. Climatic controls on biogeochemical cycles are particularly relevant in arid, semi-arid and dry sub-humid ecosystems (drylands) because their biological activity is mainly driven by water availability. The increase in aridity predicted for the twenty-first century in many drylands worldwide may therefore threaten the balance between these cycles, differentially affecting the availability of essential nutrients. Here we evaluate how aridity affects the balance between C, N and P in soils collected from 224 dryland sites from all continents except Antarctica. Wefind a negative effect of aridity on the concentration of soil organic C and total N, but a positive effect on the concentration of inorganic P. Aridity is negatively related to plant cover, which may favour the dominance of physical processes such as rock weathering, a major source of P to ecosystems, over biological processes that provide more C and N, such as litter decomposition1. Our findings suggest that any predicted increase in aridity with climate change will probably reduce the concentrations of N and C in global drylands, but increase that of P. These changes would uncouple the C, N and P cycles in drylands and could negatively affect the provision of key services provided by these ecosystems. |
publishDate |
2013 |
dc.date.none.fl_str_mv |
2013-10 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/29204 Delgado Baquerizo, Manuel; Maestre, Fernando T.; Gallardo, Antonio; Bowker, Matthew A.; Wallenstein, Matthew D.; et al.; Decoupling of soil nutrients cycles as a function of aridity in global drylands; Nature Publishing Group; Nature; 502; 7473; 10-2013; 672-676 0028-0836 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/29204 |
identifier_str_mv |
Delgado Baquerizo, Manuel; Maestre, Fernando T.; Gallardo, Antonio; Bowker, Matthew A.; Wallenstein, Matthew D.; et al.; Decoupling of soil nutrients cycles as a function of aridity in global drylands; Nature Publishing Group; Nature; 502; 7473; 10-2013; 672-676 0028-0836 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://www.nature.com/nature/journal/v502/n7473/full/nature12670.html info:eu-repo/semantics/altIdentifier/doi/10.1038/nature12670 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Nature Publishing Group |
publisher.none.fl_str_mv |
Nature Publishing Group |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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13.070432 |