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High trophic level feedbacks on global ocean carbon uptake and marine ecosystem dynamics under climate change

机译:气候变化下全球海洋碳吸收和海洋生态系统动态的高营养级反馈

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摘要

Abstract Despite recurrent emphasis on their ecological and economic roles, the importance of high trophic levels (HTLs) on ocean carbon dynamics, through passive (fecal pellet production, carcasses) and active (vertical migration) processes, is still largely unexplored, notably under climate change scenarios. In addition, HTLs impact the ecosystem dynamics through top‐down effects on lower trophic levels, which might change under anthropogenic influence. Here we compare two simulations of a global biogeochemical–ecosystem model with and without feedbacks from large marine animals. We show that these large marine animals affect the evolution of low trophic level biomasses, hence net primary production and most certainly ecosystem equilibrium, but seem to have little influence on the 21st‐century anthropogenic carbon uptake under the RCP8.5 scenario. These results provide new insights regarding the expectations for trophic amplification of climate change through the marine trophic chain and regarding the necessity to explicitly represent marine animals in Earth System Models.
机译:摘要 尽管人们一再强调其生态和经济作用,但高营养级(HTLs)通过被动(粪便颗粒生产、尸体)和主动(垂直迁移)过程对海洋碳动力学的重要性仍未得到充分探索,特别是在气候变化情景下。此外,HTLs通过对较低营养级的自上而下效应影响生态系统动态,而低营养级可能在人为影响下发生变化。在这里,我们比较了全球生物地球化学-生态系统模型的两个模拟,有和没有大型海洋动物的反馈。我们发现,这些大型海洋动物影响了低营养级生物量的演化,从而影响了净初级生产,当然也影响了生态系统平衡,但在RCP8.5情景下,似乎对21世纪人为碳吸收的影响很小。这些结果为通过海洋营养链对气候变化进行营养放大的预期以及在地球系统模型中明确表示海洋动物的必要性提供了新的见解。

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