Plant rhizodeposition : a key factor for soil organic matter formation in stable fractions
- Autores
- Villarino, Sebastián Horacio; Pinto, Priscila; Jackson, Robert B.; Piñeiro, Gervasio
- Año de publicación
- 2021
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Fil: Villarino, Sebastián Horacio. CONICET. Buenos Aires, Argentina.
Fil: Villarino, Sebastián Horacio. Universidad Nacional de Mar del Plata (UNMdP). Facultad de Ciencias Agrarias (FCA). Mar del Plata, Buenos Aires, Argentina.
Fil: Pinto, Priscila. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina.
Fil: Pinto, Priscila. CONICET – Universidad de Buenos Aires. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina.
Fil: Jackson, Robert B. Earth System Science Department. Woods Institute for the Environment. USA.
Fil: Jackson, Robert B. Stanford University. Precourt Institute for Energy. Stanford, USA.
Fil: Piñeiro, Gervasio. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina.
Fil: Piñeiro, Gervasio. CONICET – Universidad de Buenos Aires. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina.
Fil: Piñeiro, Gervasio. Universidad de la República. Facultad de Agronomía. Departamento de Sistemas Ambientales. Montevideo, Uruguay.
Soil organic carbon formation remains poorly understood despite its importance for human livelihoods. Uncertainties remain for the relative contributions of aboveground, root, and rhizodeposition inputs to particulate (POC) and mineral-associated (MAOC) organic carbon fractions. Combining a novel framework with isotope tracer studies, we quantified POC and MAOC formation efficiencies (% of C-inputs incorporated into each fraction). We found that rhizodeposition inputs have the highest MAOC formation efficiency (46%) as compared to roots (9%) or aboveground inputs (7%). In addition, rhizodeposition unexpectedly reduced POC formation, likely because it increased decomposition rates of new POC. Conversely, root biomass inputs have the highest POC formation efficiency (19%). Therefore, rhizodeposition and roots appear to play opposite but complementary roles for building MAOC and POC fractions.
grafs., tbls. - Fuente
- Science Advances
Vol.7, no.16
art.eabd3176
https://www.science.org/ - Materia
-
RHIZODEPOSITION
SOIL ORGANIC CARBON
INCUBATION EXPERIMENTS - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- acceso abierto
- Repositorio
- Institución
- Universidad de Buenos Aires. Facultad de Agronomía
- OAI Identificador
- snrd:2021villarino
Ver los metadatos del registro completo
id |
FAUBA_e3ffb9667814505c639d8412d21881a4 |
---|---|
oai_identifier_str |
snrd:2021villarino |
network_acronym_str |
FAUBA |
repository_id_str |
2729 |
network_name_str |
FAUBA Digital (UBA-FAUBA) |
spelling |
Plant rhizodeposition : a key factor for soil organic matter formation in stable fractionsVillarino, Sebastián HoracioPinto, PriscilaJackson, Robert B.Piñeiro, GervasioRHIZODEPOSITIONSOIL ORGANIC CARBONINCUBATION EXPERIMENTSFil: Villarino, Sebastián Horacio. CONICET. Buenos Aires, Argentina.Fil: Villarino, Sebastián Horacio. Universidad Nacional de Mar del Plata (UNMdP). Facultad de Ciencias Agrarias (FCA). Mar del Plata, Buenos Aires, Argentina.Fil: Pinto, Priscila. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina.Fil: Pinto, Priscila. CONICET – Universidad de Buenos Aires. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina.Fil: Jackson, Robert B. Earth System Science Department. Woods Institute for the Environment. USA.Fil: Jackson, Robert B. Stanford University. Precourt Institute for Energy. Stanford, USA.Fil: Piñeiro, Gervasio. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina.Fil: Piñeiro, Gervasio. CONICET – Universidad de Buenos Aires. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina.Fil: Piñeiro, Gervasio. Universidad de la República. Facultad de Agronomía. Departamento de Sistemas Ambientales. Montevideo, Uruguay.Soil organic carbon formation remains poorly understood despite its importance for human livelihoods. Uncertainties remain for the relative contributions of aboveground, root, and rhizodeposition inputs to particulate (POC) and mineral-associated (MAOC) organic carbon fractions. Combining a novel framework with isotope tracer studies, we quantified POC and MAOC formation efficiencies (% of C-inputs incorporated into each fraction). We found that rhizodeposition inputs have the highest MAOC formation efficiency (46%) as compared to roots (9%) or aboveground inputs (7%). In addition, rhizodeposition unexpectedly reduced POC formation, likely because it increased decomposition rates of new POC. Conversely, root biomass inputs have the highest POC formation efficiency (19%). Therefore, rhizodeposition and roots appear to play opposite but complementary roles for building MAOC and POC fractions.grafs., tbls.2021articleinfo:eu-repo/semantics/articlepublishedVersioninfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfdoi:10.1126/sciadv.abd3176issn:2375-2548http://ri.agro.uba.ar/greenstone3/library/collection/arti/document/2021villarinoScience AdvancesVol.7, no.16art.eabd3176https://www.science.org/reponame:FAUBA Digital (UBA-FAUBA)instname:Universidad de Buenos Aires. Facultad de Agronomíaenginfo:eu-repo/semantics/openAccessopenAccesshttp://ri.agro.uba.ar/greenstone3/library/page/biblioteca#section42025-09-29T13:41:57Zsnrd:2021villarinoinstacron:UBA-FAUBAInstitucionalhttp://ri.agro.uba.ar/Universidad públicaNo correspondehttp://ri.agro.uba.ar/greenstone3/oaiserver?verb=ListSetsmartino@agro.uba.ar;berasa@agro.uba.ar ArgentinaNo correspondeNo correspondeNo correspondeopendoar:27292025-09-29 13:41:58.42FAUBA Digital (UBA-FAUBA) - Universidad de Buenos Aires. Facultad de Agronomíafalse |
dc.title.none.fl_str_mv |
Plant rhizodeposition : a key factor for soil organic matter formation in stable fractions |
title |
Plant rhizodeposition : a key factor for soil organic matter formation in stable fractions |
spellingShingle |
Plant rhizodeposition : a key factor for soil organic matter formation in stable fractions Villarino, Sebastián Horacio RHIZODEPOSITION SOIL ORGANIC CARBON INCUBATION EXPERIMENTS |
title_short |
Plant rhizodeposition : a key factor for soil organic matter formation in stable fractions |
title_full |
Plant rhizodeposition : a key factor for soil organic matter formation in stable fractions |
title_fullStr |
Plant rhizodeposition : a key factor for soil organic matter formation in stable fractions |
title_full_unstemmed |
Plant rhizodeposition : a key factor for soil organic matter formation in stable fractions |
title_sort |
Plant rhizodeposition : a key factor for soil organic matter formation in stable fractions |
dc.creator.none.fl_str_mv |
Villarino, Sebastián Horacio Pinto, Priscila Jackson, Robert B. Piñeiro, Gervasio |
author |
Villarino, Sebastián Horacio |
author_facet |
Villarino, Sebastián Horacio Pinto, Priscila Jackson, Robert B. Piñeiro, Gervasio |
author_role |
author |
author2 |
Pinto, Priscila Jackson, Robert B. Piñeiro, Gervasio |
author2_role |
author author author |
dc.subject.none.fl_str_mv |
RHIZODEPOSITION SOIL ORGANIC CARBON INCUBATION EXPERIMENTS |
topic |
RHIZODEPOSITION SOIL ORGANIC CARBON INCUBATION EXPERIMENTS |
dc.description.none.fl_txt_mv |
Fil: Villarino, Sebastián Horacio. CONICET. Buenos Aires, Argentina. Fil: Villarino, Sebastián Horacio. Universidad Nacional de Mar del Plata (UNMdP). Facultad de Ciencias Agrarias (FCA). Mar del Plata, Buenos Aires, Argentina. Fil: Pinto, Priscila. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina. Fil: Pinto, Priscila. CONICET – Universidad de Buenos Aires. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina. Fil: Jackson, Robert B. Earth System Science Department. Woods Institute for the Environment. USA. Fil: Jackson, Robert B. Stanford University. Precourt Institute for Energy. Stanford, USA. Fil: Piñeiro, Gervasio. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina. Fil: Piñeiro, Gervasio. CONICET – Universidad de Buenos Aires. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura (IFEVA). Buenos Aires, Argentina. Fil: Piñeiro, Gervasio. Universidad de la República. Facultad de Agronomía. Departamento de Sistemas Ambientales. Montevideo, Uruguay. Soil organic carbon formation remains poorly understood despite its importance for human livelihoods. Uncertainties remain for the relative contributions of aboveground, root, and rhizodeposition inputs to particulate (POC) and mineral-associated (MAOC) organic carbon fractions. Combining a novel framework with isotope tracer studies, we quantified POC and MAOC formation efficiencies (% of C-inputs incorporated into each fraction). We found that rhizodeposition inputs have the highest MAOC formation efficiency (46%) as compared to roots (9%) or aboveground inputs (7%). In addition, rhizodeposition unexpectedly reduced POC formation, likely because it increased decomposition rates of new POC. Conversely, root biomass inputs have the highest POC formation efficiency (19%). Therefore, rhizodeposition and roots appear to play opposite but complementary roles for building MAOC and POC fractions. grafs., tbls. |
description |
Fil: Villarino, Sebastián Horacio. CONICET. Buenos Aires, Argentina. |
publishDate |
2021 |
dc.date.none.fl_str_mv |
2021 |
dc.type.none.fl_str_mv |
article info:eu-repo/semantics/article publishedVersion 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 |
doi:10.1126/sciadv.abd3176 issn:2375-2548 http://ri.agro.uba.ar/greenstone3/library/collection/arti/document/2021villarino |
identifier_str_mv |
doi:10.1126/sciadv.abd3176 issn:2375-2548 |
url |
http://ri.agro.uba.ar/greenstone3/library/collection/arti/document/2021villarino |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess openAccess http://ri.agro.uba.ar/greenstone3/library/page/biblioteca#section4 |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
openAccess http://ri.agro.uba.ar/greenstone3/library/page/biblioteca#section4 |
dc.format.none.fl_str_mv |
application/pdf |
dc.source.none.fl_str_mv |
Science Advances Vol.7, no.16 art.eabd3176 https://www.science.org/ reponame:FAUBA Digital (UBA-FAUBA) instname:Universidad de Buenos Aires. Facultad de Agronomía |
reponame_str |
FAUBA Digital (UBA-FAUBA) |
collection |
FAUBA Digital (UBA-FAUBA) |
instname_str |
Universidad de Buenos Aires. Facultad de Agronomía |
repository.name.fl_str_mv |
FAUBA Digital (UBA-FAUBA) - Universidad de Buenos Aires. Facultad de Agronomía |
repository.mail.fl_str_mv |
martino@agro.uba.ar;berasa@agro.uba.ar |
_version_ |
1844618863635857408 |
score |
13.070432 |