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>.
Authors
- Yunpeng Luo (ORCID: https://orcid.org/0000-0001-6383-8300)
- Tarek S. El‐Madany (ORCID: https://orcid.org/0000-0002-0726-7141)
- Arnaud Carrara (ORCID: https://orcid.org/0000-0002-9095-8807)
- Silvia Caldararu (ORCID: https://orcid.org/0000-0001-5839-6480)
- Gerardo Moreno
- Javier Pacheco‐Labrador (ORCID: https://orcid.org/0000-0003-3401-7081)
- Kendalynn A. Morris (ORCID: https://orcid.org/0000-0002-0388-6965)
- Markus Reichstein (ORCID: https://orcid.org/0000-0001-5736-1112)
- Richard Nair (ORCID: https://orcid.org/0000-0002-6293-3610)
- Mirco Migliavacca (ORCID: https://orcid.org/0000-0003-3546-8407)
- Marion Schrumpf (ORCID: https://orcid.org/0000-0003-4219-4125)
- Víctor Rolo (ORCID: https://orcid.org/0000-0001-5854-9512)
Institutions
- 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)
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