Nitrogen addition delays the emergence of an aridity-induced threshold for plant biomass

Crossing certain aridity thresholds in global drylands can lead to abrupt decays of ecosystem attributes such as plant productivity, potentially causing land degradation and desertification. It is largely unknown, however, whether these thresholds can be altered by other key global change drivers kn...

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Detalles Bibliográficos
Autores: Li, Hailing, Terrer, César|||0000-0002-5479-3486, Berdugo, Miguel|||0000-0003-1053-8907, Maestre, Fernando T.|||0000-0002-7434-4856, Zhu, Zaichun|||0000-0001-5235-5194, Peñuelas, Josep|||0000-0002-7215-0150, Yu, Kailiang|||0000-0003-4223-5169, Luo, Lin, Gong, Jie-Yu, Ye, Jiansheng|||0000-0001-5335-7896
Tipo de recurso: artículo
Fecha de publicación:2023
País:España
Institución:Universitat Autònoma de Barcelona
Repositorio:Dipòsit Digital de Documents de la UAB
Idioma:inglés
OAI Identifier:oai:ddd.uab.cat:285096
Acceso en línea:https://ddd.uab.cat/record/285096
https://dx.doi.org/urn:doi:10.1093/nsr/nwad242
Access Level:acceso abierto
Palabra clave:Aboveground biomass
Root:shoot ratios
Elevated CO2
Nitrogen fertilization
Ecosystem threshold
Descripción
Sumario:Crossing certain aridity thresholds in global drylands can lead to abrupt decays of ecosystem attributes such as plant productivity, potentially causing land degradation and desertification. It is largely unknown, however, whether these thresholds can be altered by other key global change drivers known to affect the water-use efficiency and productivity of vegetation, such as elevated CO2 and nitrogen (N). Using 5000 empirical measurements of plant biomass, we showed that crossing an aridity (1-precipitation/potential evapotranspiration) threshold of ∼0.50, which marks the transition from dry sub-humid to semi-arid climates, led to abrupt declines in aboveground biomass (AGB) and progressive increases in root:shoot ratios, thus importantly affecting carbon stocks and their distribution. N addition significantly increased AGB and delayed the emergence of its aridity threshold from 0.49 to 0.55 (P 0.05). By coupling remote sensing estimates of leaf area index with simulations from multiple models, we found that CO2 enrichment did not alter the observed aridity threshold. By 2100, and under the RCP 8.5 scenario, we forecast a 0.3% net increase in the global land area exceeding the aridity threshold detected under a scenario that includes N deposition, in comparison to a 2.9% net increase if the N effect is not considered. Our study thus indicates that N addition could mitigate to a great extent the negative impact of increasing aridity on plant biomass in drylands. These findings are critical for improving forecasts of abrupt vegetation changes in response to ongoing global environmental change.