Resilience at the Cost of Productivity: Biological Soil Crusts Mediate Vegetation Spatial Self-Organization in Drylands

IF 2.5 3区 环境科学与生态学 Q2 ECOLOGY
Ecohydrology Pub Date : 2025-04-29 DOI:10.1002/eco.70028
Daniel J. Kozar, Yu Zhang, Rachata Muneepeerakul, Xiaoli Dong
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Abstract

Water redistribution during rain events in drylands plays a critical role in the persistence and spatial pattern of vascular plants in these patchy ecosystems. Biological soil crusts (BSCs) form a membrane in the soil surface and mediate ecohydrological dynamics. However, little is known about their influence on dryland ecosystem state and spatial pattern under changing climate, which may alter total annual rainfall and intraannual rainfall regime. Building on existing models, we develop a model that considers BSC–vascular plant interactions and realistic ecohydrological dynamics under rainfall pulses. We find that the presence of BSCs often increases ecosystem resilience by promoting runoff to plants under high aridity. However, the benefit of BSCs comes at the cost of plant biomass under relatively wetter conditions; a threshold in BSC effect occurs when water losses from BSCs exceed the benefit by their surface water routing to plants. Increased resilience from BSCs, and their own persistence, can be promoted in finer soils and under rainfall regimes of less frequent events—projected for many drylands. Lastly, we find that BSCs alter feedbacks underlying plant spatial self-organization and hence their formed patterns. In high aridity, BSCs likely ameliorate competition between plants through large scale runoff promotion, reducing plant spatial pattern regularity. Our analysis highlights that BSCs significantly shape drylands' response to climate change and their positive effects on resilience may be stronger and more pervasive in a drier future, but such benefits come at a cost of ecosystem biomass and productivity when aridity is outside a critical range.

以生产力为代价的恢复力:生物土壤结皮介导旱地植被空间自组织
旱地降雨过程中的水分再分配对斑块生态系统中维管植物的持久性和空间格局起着至关重要的作用。生物土壤结皮(BSCs)在土壤表面形成一层膜并调节生态水文动力学。然而,在气候变化条件下,它们对旱地生态系统状态和空间格局的影响可能会改变年总降雨量和年内降雨量。在现有模型的基础上,我们开发了一个考虑bsc -维管植物相互作用和降雨脉冲下现实生态水文动力学的模型。我们发现,在高度干旱的情况下,BSCs的存在通常通过促进植物径流来增加生态系统的恢复能力。然而,在相对潮湿的条件下,BSCs的好处是以牺牲植物生物量为代价的;当BSC的水损失超过其地表水输送到植物的收益时,BSC效应的阈值就会出现。在较细的土壤和降雨较少的情况下,BSCs增强的恢复力及其自身的持久性可以得到促进——预计许多旱地都是如此。最后,我们发现BSCs改变了植物空间自组织的反馈,从而改变了它们的形成模式。在高干旱条件下,BSCs可能通过大规模的径流促进改善植物间的竞争,降低植物空间格局的规律性。我们的分析强调,BSCs显著地塑造了旱地对气候变化的响应,在干旱的未来,它们对恢复力的积极影响可能会更强、更普遍,但当干旱超出临界范围时,这些好处是以生态系统生物量和生产力为代价的。
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来源期刊
Ecohydrology
Ecohydrology 环境科学-生态学
CiteScore
5.10
自引率
7.70%
发文量
116
审稿时长
24 months
期刊介绍: Ecohydrology is an international journal publishing original scientific and review papers that aim to improve understanding of processes at the interface between ecology and hydrology and associated applications related to environmental management. Ecohydrology seeks to increase interdisciplinary insights by placing particular emphasis on interactions and associated feedbacks in both space and time between ecological systems and the hydrological cycle. Research contributions are solicited from disciplines focusing on the physical, ecological, biological, biogeochemical, geomorphological, drainage basin, mathematical and methodological aspects of ecohydrology. Research in both terrestrial and aquatic systems is of interest provided it explicitly links ecological systems and the hydrologic cycle; research such as aquatic ecological, channel engineering, or ecological or hydrological modelling is less appropriate for the journal unless it specifically addresses the criteria above. Manuscripts describing individual case studies are of interest in cases where broader insights are discussed beyond site- and species-specific results.
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