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Marine isoprene production and consumption in the mixed layer of the surface ocean – a field study over two oceanic regions

机译:表层海洋混合层中海洋异戊二烯的生产和消费–对两个海洋区域的实地研究

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摘要

Parameterizations of surface ocean isoprene concentrations are numerous, despite the lack of source/sink process understanding. Here we present isoprene and related field measurements in the mixed layer from the Indian Ocean and the eastern Pacific Ocean to investigate the production and consumption rates in two contrasting regions, namely oligotrophic open ocean and the coastal upwelling region. Our data show that the ability of different phytoplankton functional types (PFTs) to produce isoprene seems to be mainly influenced by light, ocean temperature, and salinity. Our field measurements also demonstrate that nutrient availability seems to have a direct influence on the isoprene production. With the help of pigment data, we calculate in-field isoprene production rates for different PFTs under varying biogeochemical and physical conditions. Using these new calculated production rates, we demonstrate that an additional significant and variable loss, besides a known chemical loss and a loss due to air–sea gas exchange, is needed to explain the measured isoprene concentration. We hypothesize that this loss, with a lifetime for isoprene between 10 and 100 days depending on the ocean region, is potentially due to degradation or consumption by bacteria.
机译:尽管缺乏对源/汇过程的了解,但表层海洋异戊二烯浓度的参数化仍然很多。在这里,我们介绍了印度洋和东太平洋混合层中的异戊二烯和相关的野外测量,以研究贫富型大洋和沿海上升区这两个形成鲜明对比的地区的生产和消费速度。我们的数据表明,不同的浮游植物功能类型(PFT)产生异戊二烯的能力似乎主要受光照,海洋温度和盐度的影响。我们的现场测量还表明,养分的可利用性似乎对异戊二烯的生产具有直接影响。借助颜料数据,我们可以在不同的生物地球化学和物理条件下计算不同PFT的现场异戊二烯生产率。使用这些新的计算出的生产率,我们证明,除了已知的化学损失和由于空气-海洋气体交换引起的损失之外,还需要额外的重大和可变损失来解释测得的异戊二烯浓度。我们假设这种损失(异戊二烯的寿命在10到100天之间,具体取决于海洋区域)可能是由于细菌的降解或消耗造成的。

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