Vegetation strategies for nitrogen and potassium acquisition along a climate and vegetation gradient: From semi-desert to temperate rainforest
| Primer Autor |
Stock, Svenja C.
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| Co-autores |
Koester, Moritz
Najera, Francisco
Boy, Jens
Matus, Francisco
Merino, Carolina
Abdallah, Khaled
Spielvogel, Sandra
Gorbushina, Anna A.
Dippold, Michaela A.
Kuzyakov, Yakov
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| Título |
Vegetation strategies for nitrogen and potassium acquisition along a climate and vegetation gradient: From semi-desert to temperate rainforest
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| Editorial |
ELSEVIER
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| Revista |
GEODERMA
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| Lenguaje |
en
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| Resumen |
Nutrient acquisition strategies of plants regulate water flow and mass transport within ecosystems, shaping earth surface processes. Understanding plant strategies under current conditions is important to assess and predict responses of natural ecosystems to future climate and environmental changes. Nitrogen (N) and potassium (K) (re-)utilization from topsoil and their acquisition from subsoil and saprolite were evaluated in a continental transect, encompassing three study sites - an arid shrubland, a mediterranean woodland, and a temperate rainforest - on similar granitoid parent material in the Chilean Coastal Cordillera. The short-term (< 1 year) plant N and K acquisition was traced with N-15 and the K analogs rubidium and cesium. To do so, the tracers were either injected into topsoil, subsoil, or saprolite, in the immediate vicinity of eight individual plants per study site and injection depth. The long-term (> decades) K uplift by plants was investigated by the vertical distribution of exchangeable K+ and Na+. Recoveries of N-15 and K analogs by arid shrubland plants were similar from topsoil, subsoil, and saprolite. Mediterranean woodland shrubs recovered the tracers primarily from topsoil (i.e., 89 % of recovered N-15 and 84 % of recovered K analogs). Forest plants recovered the tracers from topsoil (N-15 = 49 %, K analogs = 57 %) and partially from greater depth: 38 % of recovered N-15 and 43 % of recovered K analogs were acquired from subsoil and saprolite, respectively. Low nutrient accessibility in the topsoil (e.g., because of frequent droughts) drives shrubland plants to expand their N and K uptake to deeper and moister soil and saprolite. Woodland and forest plants dominantly recycled nutrients from topsoil. In the forest, this strategy was complemented by short-term uplift of N and K from depth. The vertical distribution of exchangeable K indicated long-term uplift of K by roots in all three sites. This highlighted that long-term K uplift from depth complements the nutrient budget across the continental transect.
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| Tipo de Recurso |
artículo original
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| doi |
10.1016/j.geoderma.2022.116077
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| Formato Recurso |
PDF
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| Palabras Claves |
Subsoil nutrient tracing
N-15 and K analog tracer
Nutrient uplift and recycling
Nutrient cycles
Chilean Coastal Cordillera
(semi)arid to humid-temperate natural ecosystems
PINE ARAUCARIA-ANGUSTIFOLIA
COASTAL CORDILLERA
HYDRAULIC REDISTRIBUTION
NUTRIENT ACQUISITION
GLOBAL PATTERNS
SOIL NUTRIENTS
ROOT ACTIVITY
PLANT
NITRATE
GROWTH
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| Ubicación del archivo | |
| Categoría OCDE |
Ciencia del suelo
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| Materias |
Seguimiento de nutrientes del subsuelo
Trazador analógico N-15 y K
Elevación y reciclaje de nutrientes
Ciclos de nutrientes
Cordillera Costera de Chile
Ecosistemas naturales (semi)áridos a templados húmedos
PINO ARAUCARIA-ANGUSTIFOLIA
CORDILLERA COSTERA
REDISTRIBUCIÓN HIDRÁULICA
ADQUISICIÓN DE NUTRIENTES
GLOBAL PATRONES
NUTRIENTES DEL SUELO
ACTIVIDAD DE LAS RAÍCES
PLANTA
NITRATO
CRECIMIENTO
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| Disciplinas de la OCDE |
Ciencias del suelo
Ecología
Ciencias del Medio Ambiente
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| Título de la cita (Recomendado-único) |
Vegetation strategies for nitrogen and potassium acquisition along a climate and vegetation gradient: From semi-desert to temperate rainforest
|
| Identificador del recurso (Mandatado-único) |
artículo original
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| Versión del recurso (Recomendado-único) |
version publicada
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| Condición de la licencia (Recomendado-repetible) |
0
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| Derechos de acceso |
metadata
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| Access Rights |
metadata
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| Id de Web of Science |
WOS:000862831800003
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