Divergent trends of ecosystem-scale photosynthetic efficiency between arid and humid lands across the globe

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Aim: Widespread greening and an increasing global terrestrial carbon sink over recent decades have been reported. However, the spatio-temporal relationships between vegetation greenness and productivity and the factors influencing this relationship remain unclear. We define a new metric of ecosystem-scale photosynthetic efficiency (EPE) to analyse its spatio-temporal pattern and investigate how potential drivers regulate the greenness–productivity relationship. Location: Global. Time period: From 2001 to 2016. Major taxa studied: Global terrestrial ecosystems. Methods: This study used global datasets of leaf area index (LAI) and solar-induced fluorescence (SIF) as proxies of vegetation greenness and ecosystem productivity, respectively, to propose a new metric of SIF/LAI, representing ecosystem-scale photosynthetic efficiency (EPE). We identified the spatial pattern and dynamics of EPE and examined factors influencing EPE. Results: The results showed a weaker increase in productivity compared with the global greening rate from 2001 to 2016, suggesting a decline in EPE at the global scale. This decline in EPE indicates a disproportionate increase in terrestrial productivity against the widespread greening. When stratified into areas following an aridity gradient, we found that EPE overall showed upward trends in arid and semi-arid areas, and downward trends in dry sub-humid and humid regions. The EPE was controlled primarily by soil moisture, which promoted or constrained the EPE in xeric and mesic ecosystems, respectively. Moreover, the increase in short vegetation cover and atmospheric water demand contributed positively or negatively to EPE changes in xeric and mesic ecosystems, respectively. Main conclusions: Our study shows that greening of the Earth is associated with decreasing EPE, revealing that current rates of carbon sequestration do not increase proportionally to greening of the Earth and highlighting that soil moisture is a key controller of EPE. These results help to reduce the uncertainties in future climate change impacts on vegetation dynamics, thus having implications for sustainable ecosystem management and climate change mitigation.

OriginalsprogEngelsk
TidsskriftGlobal Ecology and Biogeography
Vol/bind31
Udgave nummer9
Sider (fra-til)1824–1837
ISSN1466-8238
DOI
StatusUdgivet - 2022

Bibliografisk note

Funding Information:
This work has been supported by the National Key Research and Development Program of China (2017YFA0604700) and the Chinese Academy of Sciences (QYZDY‐SSW‐DQC025). We thank the two anonymous reviewers for their valuable and constructive suggestions to improve the study.

Publisher Copyright:
© 2022 John Wiley & Sons Ltd.

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