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地貌瞬态缓和了地形对热带冠层叶特征的控制。

Geomorphic transience moderates topographic controls on tropical canopy foliar traits.

机构信息

Department of Earth System Science, Stanford University, Stanford, CA, USA.

Earth and Environmental Sciences Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USA.

出版信息

Ecol Lett. 2020 Aug;23(8):1276-1286. doi: 10.1111/ele.13531. Epub 2020 May 25.

Abstract

Tropical ecosystems that exist on mountainous terrain harbour enormous species and functional diversity. In addition, the morphology of these complex landscapes is dynamic. Stream channels respond to mountain uplift by eroding into rising rock bodies. Many local factors determine whether channels are actively downcutting, in relative steady-state, or aggrading. It is possible to assess the trajectory of catchment-level landscape evolution utilising lidar-based models, but the effect of these trajectories on biogeochemical gradients and organisation of canopy traits across climatic and geochemical conditions remain uncertain. We use canopy trait maps to assess how variable erosion rate within catchments influence hillslope controls on canopy traits across Mt. Kinabalu, Borneo. While foliar nutrient content generally increased along hillslopes, these relationships were moderated by catchment responses to changing erosion pressure, with active downcutting associated with greater turnover in canopy traits along hillslopes. These results provide an understanding of geomorphic process controls on forest functional diversity.

摘要

存在于多山地形上的热带生态系统蕴藏着巨大的物种和功能多样性。此外,这些复杂景观的形态是动态的。溪流河道通过侵蚀上升的岩体来响应山体抬升。许多局部因素决定了河道是在积极下切、处于相对稳定状态还是在淤积。利用基于激光雷达的模型可以评估集水区水平景观演化的轨迹,但这些轨迹对生物地球化学梯度和冠层特征在气候和地球化学条件下的组织的影响仍不确定。我们使用冠层特征图来评估集水区内侵蚀速率的变化如何影响沙巴京那巴鲁山的山坡对冠层特征的控制。虽然叶片养分含量通常随山坡升高而增加,但这些关系受到集水区对侵蚀压力变化的响应的调节,活跃的下切与山坡上冠层特征的更大周转率有关。这些结果提供了对地貌过程控制森林功能多样性的理解。

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