Biogeochemical consequences of grassland degradation on linked soil, stream, and lake ecosystems in watersheds: A short review

Ze Ren
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Abstract

Grasslands are among one of the largest terrestrial biomes in the world, suffering severe threat from ongoing degradation. Grassland degradation not only alter terrestrial biogeochemical processes but also have strong potentials to affect nutrient stoichiometry and limitation in aquatic ecosystems. Moreover, the impacts of grassland degradation are likely to differentially affect the cycling of carbon (C), nitrogen (N), and phosphorus (P) in the linked terrestrial-aquatic ecosystems in watersheds, leading to multiple possible scenarios of nutrient stoichiometry and limitation in soil, stream, and lake ecosystems. However, we lack of integrated studies to consider biogeochemical consequences of grassland degradation transferring from soil to stream, and finally to the lake ecosystems. An integrated case study was conducted in the Qinghai Lake Watershed on the Qinghai-Tibet Plateau to reveal the influences of grassland degradation on soil, stream, and lake ecosystems from the perspectives of C:N:P stoichiometry , nutrient limitation, and bacterial communities. This case study demonstrated a clear cascading influence from terrestrial to aquatic ecosystem, that grassland degradation differentially influenced N and P in soil with soil N decreased but P did not change (N:P decreased in soil), influencing the nutrients delivered to streams with streamwater N decreased but P increased (N:P decreased in stream), alleviating P limitation of stream biofilms which are sensitive to P variation, and ultimately stimulating phytoplankton growth in the P-limited Qinghai Lake. This case study supported one scenario of biogeochemical consequences of grassland degradation, and other scenarios might be also possible in watersheds that have different geochemistry background, different landcover, and/or different lake trophic status. Integrated studies considering the coupled terrestrial-aquatic ecosystems can provide insights for protection and management of grassland watersheds in the rapidly changing world.

流域草地退化对土壤、河流和湖泊生态系统的生物地球化学影响:综述
草原是世界上最大的陆地生物群落之一,受到持续退化的严重威胁。草地退化不仅改变了陆地生物地球化学过程,而且对水生生态系统的营养化学计量和限制也有很强的影响。此外,草地退化的影响可能会对流域陆水生态系统中碳(C)、氮(N)和磷(P)的循环产生不同的影响,从而导致土壤、河流和湖泊生态系统中营养化学计量和限制的多种可能情景。然而,我们缺乏考虑草地退化从土壤到河流并最终到湖泊生态系统的生物地球化学后果的综合研究。以青藏高原青海湖流域为研究对象,从C:N:P化学计量学、养分限制和细菌群落等方面揭示了草地退化对土壤、河流和湖泊生态系统的影响。本案例研究表明,从陆地生态系统到水生生态系统存在明显的级联效应,草地退化对土壤N和P的影响存在差异,土壤N减少而P不变(土壤N:P减少),对河流养分的影响存在差异,河流水体N减少而P增加(河流中N:P减少),缓解了对P变化敏感的河流生物膜对P的限制。并最终刺激了磷含量有限的青海湖浮游植物的生长。本案例研究支持草地退化的生物地球化学后果的一种情景,并且在具有不同地球化学背景、不同土地覆盖和/或不同湖泊营养状况的流域也可能存在其他情景。考虑陆水耦合生态系统的综合研究可以为快速变化的世界中草地流域的保护和管理提供见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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