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

Author:

Nair Richard12ORCID,Luo Yunpeng3,El‐Madany Tarek2ORCID,Rolo Victor4ORCID,Pacheco‐Labrador Javier56,Caldararu Silvia1ORCID,Morris Kendalynn A.5,Schrumpf Marion27,Carrara Arnaud8,Moreno Gerardo4,Reichstein Markus2,Migliavacca Mirco29

Affiliation:

1. Discipline of Botany, School of Natural Sciences Trinity College Dublin Dublin Ireland

2. Department of Biogeochemical Integration Max Planck Institute for Biogeochemistry Jena Germany

3. Swiss Federal Institute for Forest Snow and Landscape Research WSL Birmensdorf Switzerland

4. Forest Research Group, INDEHESA University of Extremadura Plasencia Cáceres Spain

5. Joint Global Change Research Institute Pacific Northwest National Laboratory College Park Maryland USA

6. Environmental Remote Sensing and Spectroscopy Laboratory (SpecLab) Spanish National Research Council Madrid Spain

7. Department of Biogeochemical Processes Max Planck Institute for Biogeochemistry Jena Germany

8. Fundación Centro de Estudios Ambientales del Mediterráneo (CEAM) Valencia Spain

9. European Commission Joint Research Centre Ispra VA Italy

Abstract

AbstractAll 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 (CUEECO), 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 (RECO, plants and heterotrophs) are limited by N, P or associated changes in other biogeochemical cycles, CUEECO may change. Seasonally, CUEECO 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 CUEECO 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 CUEECO should be increased by wetter conditions, and successively by N and NP fertilization. Milder and wetter years with proportionally longer growing seasons increased CUEECO, 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 CUEECO. 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 CUEECO.

Publisher

Wiley

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