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
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/29204

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network_name_str CONICET Digital (CONICET)
spelling 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
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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/
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application/pdf
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dc.publisher.none.fl_str_mv Nature Publishing Group
publisher.none.fl_str_mv Nature Publishing Group
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