Hydrologic regulation of plant rooting depth
- Autores
- Fan, Ying; Miguez Macho, Gonzalo; Jobbagy Gampel, Esteban Gabriel; Jackson, Robert B.; Otero Casal, Carlos
- Año de publicación
- 2017
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Plant rooting depth affects ecosystem resilience to environmental stress such as drought. Deep roots connect deep soil/groundwater to the atmosphere, thus influencing the hydrologic cycle and climate. Deep roots enhance bedrock weathering, thus regulating the long-term carbon cycle. However, we know little about how deep roots go and why. Here, we present a global synthesis of 2,200 root observations of >1,000 species along biotic (life form, genus) and abiotic (precipitation, soil, drainage) gradients. Results reveal strong sensitivities of rooting depth to local soil water profiles determined by precipitation infiltration depth from the top (reflecting climate and soil), and groundwater table depth from below (reflecting topography-driven land drainage). In well-drained uplands, rooting depth follows infiltration depth; in waterlogged lowlands, roots stay shallow, avoiding oxygen stress below the water table; in between, high productivity and drought can send roots many meters down to the groundwater capillary fringe. This framework explains the contrasting rooting depths observed under the same climate for the same species but at distinct topographic positions. We assess the global significance of these hydrologic mechanisms by estimating root water-uptake depths using an inverse model, based on observed productivity and atmosphere, at 30″ (∼1-km) global grids to capture the topography critical to soil hydrology. The resulting patterns of plant rooting depth bear a strong topographic and hydrologic signature at landscape to global scales. They underscore a fundamental plant–water feedback pathway that may be critical to understanding plant-mediated global change.
Fil: Fan, Ying. Rutgers University; Estados Unidos
Fil: Miguez Macho, Gonzalo. Universidad de Santiago de Compostela; España
Fil: Jobbagy Gampel, Esteban Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Luis. Instituto de Matemática Aplicada de San Luis ; Argentina
Fil: Jackson, Robert B.. University of Stanford; Estados Unidos
Fil: Otero Casal, Carlos. Universidad de Santiago de Compostela; España - Materia
-
Global Change Biology
Infiltration Depth
Plant Rooting Depth
Soil Hydrology
Water Table Depth - 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:11336/65973
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Hydrologic regulation of plant rooting depthFan, YingMiguez Macho, GonzaloJobbagy Gampel, Esteban GabrielJackson, Robert B.Otero Casal, CarlosGlobal Change BiologyInfiltration DepthPlant Rooting DepthSoil HydrologyWater Table Depthhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1https://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Plant rooting depth affects ecosystem resilience to environmental stress such as drought. Deep roots connect deep soil/groundwater to the atmosphere, thus influencing the hydrologic cycle and climate. Deep roots enhance bedrock weathering, thus regulating the long-term carbon cycle. However, we know little about how deep roots go and why. Here, we present a global synthesis of 2,200 root observations of >1,000 species along biotic (life form, genus) and abiotic (precipitation, soil, drainage) gradients. Results reveal strong sensitivities of rooting depth to local soil water profiles determined by precipitation infiltration depth from the top (reflecting climate and soil), and groundwater table depth from below (reflecting topography-driven land drainage). In well-drained uplands, rooting depth follows infiltration depth; in waterlogged lowlands, roots stay shallow, avoiding oxygen stress below the water table; in between, high productivity and drought can send roots many meters down to the groundwater capillary fringe. This framework explains the contrasting rooting depths observed under the same climate for the same species but at distinct topographic positions. We assess the global significance of these hydrologic mechanisms by estimating root water-uptake depths using an inverse model, based on observed productivity and atmosphere, at 30″ (∼1-km) global grids to capture the topography critical to soil hydrology. The resulting patterns of plant rooting depth bear a strong topographic and hydrologic signature at landscape to global scales. They underscore a fundamental plant–water feedback pathway that may be critical to understanding plant-mediated global change.Fil: Fan, Ying. Rutgers University; Estados UnidosFil: Miguez Macho, Gonzalo. Universidad de Santiago de Compostela; EspañaFil: Jobbagy Gampel, Esteban Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Luis. Instituto de Matemática Aplicada de San Luis ; ArgentinaFil: Jackson, Robert B.. University of Stanford; Estados UnidosFil: Otero Casal, Carlos. Universidad de Santiago de Compostela; EspañaNational Academy of Sciences2017-10-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/65973Fan, Ying; Miguez Macho, Gonzalo; Jobbagy Gampel, Esteban Gabriel; Jackson, Robert B.; Otero Casal, Carlos; Hydrologic regulation of plant rooting depth; National Academy of Sciences; Proceedings of the National Academy of Sciences of The United States of America; 114; 40; 3-10-2017; 10572-105770027-8424CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1073/pnas.1712381114info:eu-repo/semantics/altIdentifier/url/http://www.pnas.org/content/114/40/10572info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:39:30Zoai:ri.conicet.gov.ar:11336/65973instacron: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 09:39:30.994CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Hydrologic regulation of plant rooting depth |
title |
Hydrologic regulation of plant rooting depth |
spellingShingle |
Hydrologic regulation of plant rooting depth Fan, Ying Global Change Biology Infiltration Depth Plant Rooting Depth Soil Hydrology Water Table Depth |
title_short |
Hydrologic regulation of plant rooting depth |
title_full |
Hydrologic regulation of plant rooting depth |
title_fullStr |
Hydrologic regulation of plant rooting depth |
title_full_unstemmed |
Hydrologic regulation of plant rooting depth |
title_sort |
Hydrologic regulation of plant rooting depth |
dc.creator.none.fl_str_mv |
Fan, Ying Miguez Macho, Gonzalo Jobbagy Gampel, Esteban Gabriel Jackson, Robert B. Otero Casal, Carlos |
author |
Fan, Ying |
author_facet |
Fan, Ying Miguez Macho, Gonzalo Jobbagy Gampel, Esteban Gabriel Jackson, Robert B. Otero Casal, Carlos |
author_role |
author |
author2 |
Miguez Macho, Gonzalo Jobbagy Gampel, Esteban Gabriel Jackson, Robert B. Otero Casal, Carlos |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
Global Change Biology Infiltration Depth Plant Rooting Depth Soil Hydrology Water Table Depth |
topic |
Global Change Biology Infiltration Depth Plant Rooting Depth Soil Hydrology Water Table Depth |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Plant rooting depth affects ecosystem resilience to environmental stress such as drought. Deep roots connect deep soil/groundwater to the atmosphere, thus influencing the hydrologic cycle and climate. Deep roots enhance bedrock weathering, thus regulating the long-term carbon cycle. However, we know little about how deep roots go and why. Here, we present a global synthesis of 2,200 root observations of >1,000 species along biotic (life form, genus) and abiotic (precipitation, soil, drainage) gradients. Results reveal strong sensitivities of rooting depth to local soil water profiles determined by precipitation infiltration depth from the top (reflecting climate and soil), and groundwater table depth from below (reflecting topography-driven land drainage). In well-drained uplands, rooting depth follows infiltration depth; in waterlogged lowlands, roots stay shallow, avoiding oxygen stress below the water table; in between, high productivity and drought can send roots many meters down to the groundwater capillary fringe. This framework explains the contrasting rooting depths observed under the same climate for the same species but at distinct topographic positions. We assess the global significance of these hydrologic mechanisms by estimating root water-uptake depths using an inverse model, based on observed productivity and atmosphere, at 30″ (∼1-km) global grids to capture the topography critical to soil hydrology. The resulting patterns of plant rooting depth bear a strong topographic and hydrologic signature at landscape to global scales. They underscore a fundamental plant–water feedback pathway that may be critical to understanding plant-mediated global change. Fil: Fan, Ying. Rutgers University; Estados Unidos Fil: Miguez Macho, Gonzalo. Universidad de Santiago de Compostela; España Fil: Jobbagy Gampel, Esteban Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Luis. Instituto de Matemática Aplicada de San Luis ; Argentina Fil: Jackson, Robert B.. University of Stanford; Estados Unidos Fil: Otero Casal, Carlos. Universidad de Santiago de Compostela; España |
description |
Plant rooting depth affects ecosystem resilience to environmental stress such as drought. Deep roots connect deep soil/groundwater to the atmosphere, thus influencing the hydrologic cycle and climate. Deep roots enhance bedrock weathering, thus regulating the long-term carbon cycle. However, we know little about how deep roots go and why. Here, we present a global synthesis of 2,200 root observations of >1,000 species along biotic (life form, genus) and abiotic (precipitation, soil, drainage) gradients. Results reveal strong sensitivities of rooting depth to local soil water profiles determined by precipitation infiltration depth from the top (reflecting climate and soil), and groundwater table depth from below (reflecting topography-driven land drainage). In well-drained uplands, rooting depth follows infiltration depth; in waterlogged lowlands, roots stay shallow, avoiding oxygen stress below the water table; in between, high productivity and drought can send roots many meters down to the groundwater capillary fringe. This framework explains the contrasting rooting depths observed under the same climate for the same species but at distinct topographic positions. We assess the global significance of these hydrologic mechanisms by estimating root water-uptake depths using an inverse model, based on observed productivity and atmosphere, at 30″ (∼1-km) global grids to capture the topography critical to soil hydrology. The resulting patterns of plant rooting depth bear a strong topographic and hydrologic signature at landscape to global scales. They underscore a fundamental plant–water feedback pathway that may be critical to understanding plant-mediated global change. |
publishDate |
2017 |
dc.date.none.fl_str_mv |
2017-10-03 |
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/11336/65973 Fan, Ying; Miguez Macho, Gonzalo; Jobbagy Gampel, Esteban Gabriel; Jackson, Robert B.; Otero Casal, Carlos; Hydrologic regulation of plant rooting depth; National Academy of Sciences; Proceedings of the National Academy of Sciences of The United States of America; 114; 40; 3-10-2017; 10572-10577 0027-8424 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/65973 |
identifier_str_mv |
Fan, Ying; Miguez Macho, Gonzalo; Jobbagy Gampel, Esteban Gabriel; Jackson, Robert B.; Otero Casal, Carlos; Hydrologic regulation of plant rooting depth; National Academy of Sciences; Proceedings of the National Academy of Sciences of The United States of America; 114; 40; 3-10-2017; 10572-10577 0027-8424 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1073/pnas.1712381114 info:eu-repo/semantics/altIdentifier/url/http://www.pnas.org/content/114/40/10572 |
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 |
dc.publisher.none.fl_str_mv |
National Academy of Sciences |
publisher.none.fl_str_mv |
National Academy of Sciences |
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) |
collection |
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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1844613250073755648 |
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13.070432 |