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首页> 外文期刊>Scientific reports. >Diel patterns of microphytobenthic primary production in intertidal sediments: the role of photoperiod on the vertical migration circadian rhythm
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Diel patterns of microphytobenthic primary production in intertidal sediments: the role of photoperiod on the vertical migration circadian rhythm

机译:跨期沉积物中微生物的初级生产的Diel模式:光周期对垂直迁移昼夜节律的作用

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Diel primary production patterns of intertidal microphytobenthos (MPB) have been attributed to short-term physiological changes in the photosynthetic apparatus or to diel changes in the photoautotrophic biomass in the sediment photic layer due to vertical migration. Diel changes in primary production and vertical migration are entrained by external factors like photoperiod and tides. However, the role of photoperiod and tides has not been experimentally separated to date. Here, we performed laboratory experiments with sediment cores kept in immersion, in the absence of tides, with photoperiod or under continuous light. Measurements of net production, made with Osub2/sub microsensors, and of spectral reflectance at the sediment surface showed that, in intertidal sediments, the photoperiod signal was the major driver of the diel patterns of net primary production and sediment oxygen availability through the vertical migration of the MPB photoautotrophic biomass. Vertical migration was controlled by an endogenous circadian rhythm entrained by photoperiod in the absence of tides. The pattern progressively disappeared after 3 days in continuous light but was immediately reset by photoperiod. Even though a potential contribution of a subjective in situ tidal signal cannot be completely discarded, Fourier and cross spectral analysis of temporal patterns indicated that the photosynthetic circadian rhythm was mainly characterized by light/dark migratory cycles.
机译:二氧化局部掺主生产模式的透射性微粒(MPB)归因于光合仪器中的短期生理变化或由于垂直迁移而在沉积物光层中的光学营养生物质中的Diel变化。主要生产和垂直迁移的DIEL变化由外部因素如PhotoCeriod和Tides夹带。但是,光周期和潮汐的作用尚未通过实验分开至今。在这里,我们对沉积物芯进行了实验室实验,在没有潮汐的情况下,具有光周期或连续光。用O 2 微传感器和沉积物表面的光谱反射率制成的净生产的测量表明,在跨沉积物中,光周期信号是净初级生产和沉积物的二极管模式的主要驱动器通过MPB光拍营养生物质的垂直迁移来氧气可用性。垂直迁移是通过潮汐缺失的光周期夹带的内源性昼夜节律来控制。在连续光线3天后,图案逐渐消失,但是通过光周期立即重置。尽管无法完全丢弃主体潮汐信号的潜在贡献,但是时间图案的傅里叶和跨光谱分析表明光合昼夜节律主要是光/黑暗迁徙循环的特征。

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