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Both respiration and photosynthesis determine the scaling of plankton metabolism in the oligotrophic ocean

机译:呼吸作用和光合作用决定贫营养海洋中浮游生物代谢的尺度

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摘要

Despite its importance to ocean-climate interactions, the metabolic state of the oligotrophic ocean has remained controversial for 415 years. Positions in the debate are that it is either hetero- or autotrophic, which suggests either substantial unaccounted for organic matter inputs, or that all available photosynthesis (P) estimations (including C-14) are biased. Here we show the existence of systematic differences in the metabolic state of the North (heterotrophic) and South (autotrophic) Atlantic oligotrophic gyres, resulting from differences in both P and respiration (R). The oligotrophic ocean is neither auto-nor heterotrophic, but functionally diverse. Our results show that the scaling of plankton metabolism by generalized P:R relationships that has sustained the debate is biased, and indicate that the variability of R, and not only of P, needs to be considered in regional estimations of the ocean's metabolic state.
机译:尽管它对海洋-气候相互作用具有重要意义,但贫营养海洋的代谢状态一直存在争议415年。辩论中的立场是它是异养的还是自养的,这表明要么根本无法解释有机物质的输入,要么表明所有可用的光合作用(P)估算值(包括C-14)都是有偏差的。在这里,我们显示了北(异养)和南(自养)大西洋贫营养回旋的代谢状态存在系统性差异,这是由于P和呼吸(R)的差异所致。贫营养性海洋既不是自体也不是异养性的,而是功能多样的。我们的研究结果表明,通过持续存在争议的广义P:R关系对浮游生物代谢的缩放是有偏差的,并且表明在海洋代谢状态的区域估计中需要考虑R的可变性,而不仅仅是P的可变性。

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