Aridity creates global thresholds in soil nitrogen retention and availability

Author:

Elrys Ahmed S.123ORCID,Abo El‐Maati Mohamed F.4ORCID,Dan Xiaoqian1ORCID,Wen YuHong1,Mou Jinxia1,Abdelghany Ahmed Elsayed56,Uwiragiye Yves78ORCID,Shuirong Tang1ORCID,Yanzheng Wu1ORCID,Meng Lei1ORCID,Zhang JinBo138ORCID,Müller Christoph3910ORCID

Affiliation:

1. College of Tropical Crops Hainan University Haikou China

2. Soil Science Department, Faculty of Agriculture Zagazig University Zagazig Egypt

3. Liebig Centre for Agroecology and Climate Impact Research Justus Liebig University Giessen Germany

4. Agriculture Biochemistry Department, Faculty of Agriculture Zagazig University Zagazig Egypt

5. Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid, Areas of Ministry of Education Northwest A&F University Yangling China

6. Water Relation and Field Irrigation Department Agriculture and Biological Institute, National Research Centre Cairo Egypt

7. Department of Agriculture, Faculty of Agriculture, Environmental Management and Renewable Energy University of Technology and Arts of Byumba Byumba Rwanda

8. School of Geography Nanjing Normal University Nanjing China

9. Institute of Plant Ecology Justus Liebig University Giessen Giessen Germany

10. School of Biology and Environmental Science and Earth Institute University College Dublin Dublin Ireland

Abstract

AbstractIdentifying tipping points in the relationship between aridity and gross nitrogen (N) cycling rates could show critical vulnerabilities of terrestrial ecosystems to climate change. Yet, the global pattern of gross N cycling response to aridity across terrestrial ecosystems remains unknown. Here, we collected 14,144 observations from 451 15N‐labeled studies and used segmented regression to identify the global threshold responses of soil gross N cycling rates and soil process‐related variables to aridity index (AI), which decreases as aridity increases. We found on a global scale that increasing aridity reduced soil gross nitrate consumption but increased soil nitrification capacity, mainly due to reduced soil microbial biomass carbon (MBC) and N (MBN) and increased soil pH. Threshold response of gross N production and retention to aridity was observed across terrestrial ecosystems. In croplands, gross nitrification and extractable nitrate were inhibited with increasing aridity below the threshold AI ~0.8–0.9 due to inhibited ammonia‐oxidizing archaea and bacteria, while the opposite was favored above this threshold. In grasslands, gross N mineralization and immobilization decreased with increasing aridity below the threshold AI ~0.5 due to decreased MBN, but the opposite was true above this threshold. In forests, increased aridity stimulated nitrate immobilization below the threshold AI ~1.0 due to increased soil C/N ratio, but inhibited ammonium immobilization above the threshold AI ~1.3 due to decreased soil total N and increased MBC/MBN ratio. Soil dissimilatory nitrate reduction to ammonium decreased with increasing aridity globally and in forests when the threshold AI ~1.4 was passed. Overall, we suggest that any projected increase in aridity in response to climate change is likely to reduce plant N availability in arid regions while enhancing it in humid regions, affecting the provision of ecosystem services and functions.

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

General Environmental Science,Ecology,Environmental Chemistry,Global and Planetary Change

Reference533 articles.

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3. Global ecosystem thresholds driven by aridity

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