Shengjie Wang , Chenxi Xu , Yuanqiao Li , Jiayan Shen , Jia Tang , Shuai Yuan
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引用次数: 0
Abstract
Tree stems act as the primary carbon storage organs, with leaf growth variability regulating storage intensity. However, how environmental factors influence carbon storage via leaf growth remains unclear. This study examines the relationship between tree stem growth (tree-ring width index, RWI) and leaf growth (normalized difference vegetation index, NDVI) across different forest types globally. We analyzed the potential influencing factors of this relationship and identified the pathway from environmental conditions to leaves and then stems. We found that MODIS NDVI, with higher spatial resolution, better reflects stem growth in broadleaf forests, while GIMMS NDVI, with a longer time series, is more effective in characterizing stem growth in coniferous forests. Forest type and moisture availability are the dominant factors shaping the leaf-stem growth relationship. Coniferous trees growing under increasingly drier conditions, with higher tree density and poorer soil fertility, tend to exhibit a stronger coupling between leaf and stem growth. Further analysis showed that in moist environments, especially in broadleaf forests, leaf and stem growth become increasingly decoupled. In contrast, conifers maintain stronger coordination. This may be related to trade-offs in resource allocation driven by the varying relative importance of external environmental stress and internal biological connections affecting leaf and stem growth under different moisture conditions. Leaf growth is influenced by soil moisture, soil temperature, and air temperature, but their relative contributions vary across forest types and moisture regimes. These findings suggest caution when using leaf growth (e.g., NDVI) as a proxy for forest productivity in humid broadleaf ecosystems, where decoupling may mask actual carbon allocation patterns.
期刊介绍:
The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems.
Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged.
Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.