Potassium: a neglected nutrient in global change
Aim: Potassium (K) is the second most abundant nutrient in plant photosynthetic tissues after nitrogen (N). Thousands of physiological and metabolic studies in recent decades have established the fundamental role of K in plant function, especially in water-use efficiency and economy, and yet macroec...
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Published in | Global ecology and biogeography Vol. 24; no. 3; pp. 261 - 275 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Oxford
Blackwell Publishing Ltd
01.03.2015
John Wiley & Sons Ltd Wiley Subscription Services, Inc |
Subjects | |
Online Access | Get full text |
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Summary: | Aim: Potassium (K) is the second most abundant nutrient in plant photosynthetic tissues after nitrogen (N). Thousands of physiological and metabolic studies in recent decades have established the fundamental role of K in plant function, especially in water-use efficiency and economy, and yet macroecological studies have mostly overlooked this nutrient. Methods: We have reviewed available studies on the content, stoichiometry and roles of in the soil–plant system and in terrestrial ecosystems. We have also reviewed the impacts of global change drivers on K content, stoichiometry and roles. Conclusions: The current literature indicates that K, at a global level, is as limiting as N and phosphorus (P) for plant productivity in terrestrial ecosystems. Some degree of K limitation has been seen in up to 70% of all studied terrestrial ecosystems. However, in some areas atmospheric K deposition from human activities is greater than that from natural sources. We are far from understanding the K fluxes between the atmosphere and land, and the role of anthropogenic activities in these fluxes. The increasing aridity expected in wide areas of the world makes K more critical through its role in water-use efficiency. N deposition exerts a strong impact on the ecosystem K cycle, decreasing K availability and increasing K limitation. Plant invasive success is enhanced by higher soil K availability, especially in environments without strong abiotic stresses. The impacts of other drivers of global change, such as increasing atmospheric CO₂ or changes in land use, remain to be elucidated. Current models of the responses of ecosystems and carbon storage to projected global climatic and atmospheric changes are now starting to consider N and P, but they should also consider K, mostly in arid and semi-arid ecosystems. |
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Bibliography: | Spanish Government - No. CGL2013-48074-P istex:51A20AB6DF363F6DB5AB16CBDA81D722EEC19EAC ark:/67375/WNG-SRLVXN4D-8 ArticleID:GEB12259 European Research Council Synergy - No. ERC-2013-SyG-610028 Appendix S1 Annual atmospheric rates of K deposition (kg ha−1 year−1). Appendix S2 The limiting role of K on plant growth. Appendix S3 Effects of water availability on the ecosystem K cycle. Appendix S4 Impacts of increases of N supply on the ecosystem K cycle. Appendix S5 Plant invasion and soil K availability. Appendix S6 References for the Supporting Information. Catalan Government - No. SGR 2014-274 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
ISSN: | 1466-822X 1466-8238 |
DOI: | 10.1111/geb.12259 |