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Climate-driven changes in the ecological stoichiometry of aquatic ecosystems

机译:气候驱动的水生生态系统化学计量的变化

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Advances in ecological stoichiometry, a rapidly expanding research field investigating the elemental composition of organisms and their environment, have shed new light on the impacts of climate change on freshwater and marine ecosystems. Current changes in the Earth's climate alter the availability of carbon and nutrients in lakes and oceans. In particular, atmospheric CO _2 concentrations will rise to unprecedented levels by the end of this century, while global warming will enhance stratification of aquatic ecosystems and may thereby diminish the supply of nutrients into the surface layer. These processes enrich phytoplankton with carbon, but suppress nutrient availability. Phytoplankton with a high carbon-to-nutrient content provide poor-quality food for most zooplankton species, which may shift the species composition of zooplankton and higher trophic levels to less nutrient-demanding species. As a consequence, climate-driven changes in plankton stoichiometry may alter the structure and functioning of entire aquatic food webs.
机译:生态化学计量学的进展是一个迅速扩展的研究领域,主要研究有机物及其环境的元素构成,为气候变化对淡水和海洋生态系统的影响提供了新的思路。当前地球气候的变化改变了湖泊和海洋中碳和养分的利用率。特别是,到本世纪末,大气中的CO_2浓度将上升到前所未有的水平,而全球变暖将增强水生生态系统的分层,从而可能减少营养物质向表层的供应。这些过程使浮游植物富含碳,但抑制了养分的利用。碳-营养含量高的浮游植物为大多数浮游动物提供了劣质食物,这可能会将浮游动物的物种组成和较高的营养水平转变为对养分需求较少的物种。结果,气候驱动的浮游生物化学计量变化可能会改变整个水生食物网的结构和功能。

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