Nitrogen availability and summer drought, but not N:P imbalance, drive carbon use efficiency of a Mediterranean tree‐grass ecosystem

All ecosystems contain both sources and sinks for atmospheric carbon (C). A change in their balance of net and gross ecosystem carbon uptake, ecosystem-scale carbon use efficiency (CUE<sub>ECO</sub>), is a change in their ability to buffer climate change. However, anthropogenic nitrogen (N) deposition is increasing N availability, potentially shifting terrestrial ecosystem stoichiometry towards phosphorus (P) limitation. Depending on how gross primary production (GPP, plants alone) and ecosystem respiration (R<sub>ECO</sub>, plants and heterotrophs) are limited by N, P or associated changes in other biogeochemical cycles, CUE<sub>ECO</sub> may change. Seasonally, CUE<sub>ECO</sub> also varies as the multiple processes that control GPP and respiration and their limitations shift in time. We worked in a Mediterranean tree-grass ecosystem (locally called 'dehesa') characterized by mild, wet winters and summer droughts. We examined CUE<sub>ECO</sub> from eddy covariance fluxes over 6 years under control, +N and + NP fertilized treatments on three timescales: annual, seasonal (determined by vegetation phenological phases) and 14-day aggregations. Finer aggregation allowed consideration of responses to specific patterns in vegetation activity and meteorological conditions. We predicted that CUE<sub>ECO</sub> should be increased by wetter conditions, and successively by N and NP fertilization. Milder and wetter years with proportionally longer growing seasons increased CUE<sub>ECO</sub>, as did N fertilization, regardless of whether P was added. Using a generalized additive model, whole ecosystem phenological status and water deficit indicators, which both varied with treatment, were the main determinants of 14-day differences in CUE<sub>ECO</sub>. The direction of water effects depended on the timescale considered and occurred alongside treatment-dependent water depletion. Overall, future regional trends of longer dry summers may push these systems towards lower CUE<sub>ECO</sub>.

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Publication Details

Journal
Global Change Biology
Published
2024-08-31
DOI
https://doi.org/10.1111/gcb.17486
Citations
6
Primary Topic
Plant Water Relations and Carbon Dynamics
Type
article
Field-Weighted Citation Impact
1.70
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article

Nitrogen availability and summer drought, but not N:P imbalance, drive carbon use efficiency of a Mediterranean tree‐grass ecosystem

Yunpeng Luo, Tarek S. El‐Madany, Arnaud Carrara, Silvia Caldararu et al.
6 citations
Global Change Biology
Plant Water Relations and Carbon Dynamics
1.70
article

Nitrogen availability and summer drought, but not N:P imbalance, drive carbon use efficiency of a Mediterranean tree‐grass ecosystem

Yunpeng Luo, Tarek S. El‐Madany, Arnaud Carrara, Silvia Caldararu, Gerardo Moreno, Javier Pacheco‐Labrador, Kendalynn A. Morris, Markus Reichstein, Richard Nair, Mirco Migliavacca, Marion Schrumpf, Víctor Rolo
article en
6 citations

Abstract

All ecosystems contain both sources and sinks for atmospheric carbon (C). A change in their balance of net and gross ecosystem carbon uptake, ecosystem-scale carbon use efficiency (CUE<sub>ECO</sub>), is a change in their ability to buffer climate change. However, anthropogenic nitrogen (N) deposition is increasing N availability, potentially shifting terrestrial ecosystem stoichiometry towards phosphorus (P) limitation. Depending on how gross primary production (GPP, plants alone) and ecosystem respiration (R<sub>ECO</sub>, plants and heterotrophs) are limited by N, P or associated changes in other biogeochemical cycles, CUE<sub>ECO</sub> may change. Seasonally, CUE<sub>ECO</sub> also varies as the multiple processes that control GPP and respiration and their limitations shift in time. We worked in a Mediterranean tree-grass ecosystem (locally called 'dehesa') characterized by mild, wet winters and summer droughts. We examined CUE<sub>ECO</sub> from eddy covariance fluxes over 6 years under control, +N and + NP fertilized treatments on three timescales: annual, seasonal (determined by vegetation phenological phases) and 14-day aggregations. Finer aggregation allowed consideration of responses to specific patterns in vegetation activity and meteorological conditions. We predicted that CUE<sub>ECO</sub> should be increased by wetter conditions, and successively by N and NP fertilization. Milder and wetter years with proportionally longer growing seasons increased CUE<sub>ECO</sub>, as did N fertilization, regardless of whether P was added. Using a generalized additive model, whole ecosystem phenological status and water deficit indicators, which both varied with treatment, were the main determinants of 14-day differences in CUE<sub>ECO</sub>. The direction of water effects depended on the timescale considered and occurred alongside treatment-dependent water depletion. Overall, future regional trends of longer dry summers may push these systems towards lower CUE<sub>ECO</sub>.

Global Change BiologyVol. 30(9)
Joint Global Change Research Institute (US), Consejo Superior de Investigaciones Científicas (ES), Pacific Northwest National Laboratory (US), Trinity College Dublin (IE), Swiss Federal Institute for Forest, Snow and Landscape Research (CH), Mediterranean Center for Environmental Studies (ES), Joint Research Centre (IT), Max Planck Institute for Biogeochemistry (DE), Universidad de Extremadura (ES)
Clean water and sanitation
Openalex Percentile: Top 16%
Plant Water Relations and Carbon Dynamics
1.70
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