Berge Jørgen, Cottier Finlo, Varpe Oystein, Renaud Paul E, Falk-Petersen Stig, Kwasniewski Sawomir, Griffiths Colin, Søreide Janne E, Johnsen Geir, Aubert Anais, Bjærke Oda, Hovinen Johanna, Jung-Madsen Signe, Tveit Martha, Majaneva Sanna
Faculty of Biosciences, Fisheries and Economics , University of Tromsø , 9037 Tromsø , Norway ; The University Centre in Svalbard , N-9171 Longyearbyen , Norway.
Scottish Association for Marine Science , Scottish Marine Institute , Oban, Argyll PA37 1QA , UK.
J Plankton Res. 2014 Sep;36(5):1279-1297. doi: 10.1093/plankt/fbu059. Epub 2014 Jul 9.
Diel vertical migration (DVM) of zooplankton is a global phenomenon, characteristic of both marine and limnic environments. At high latitudes, patterns of DVM have been documented, but rather little knowledge exists regarding which species perform this ecologically important behaviour. Also, in the Arctic, the vertically migrating components of the zooplankton community are usually regarded as a single sound scattering layer (SSL) performing synchronized patterns of migration directly controlled by ambient light. Here, we present evidence for hitherto unknown complexity of Arctic marine systems, where zooplankton form multiple aggregations through the water column seen via acoustics as distinct SSLs. We show that while the initiation of DVM during the autumnal equinox is light mediated, the vertical positioning of the migrants during day is linked more to the thermal characteristics of water masses than to irradiance. During night, phytoplankton biomass is shown to be the most important factor determining the vertical positioning of all migrating taxa. Further, we develop a novel way of representing acoustic data in the form of a Sound Image (SI) that enables a direct comparison of the relative importance of each potential scatterer based upon the theoretical contribution of their backscatter. Based on our comparison of locations with contrasting hydrography, we conclude that a continued warming of the Arctic is likely to result in more complex ecotones across the Arctic marine system.
浮游动物的昼夜垂直迁移(DVM)是一种全球现象,在海洋和淡水环境中均有体现。在高纬度地区,DVM的模式已有记录,但对于哪些物种表现出这种具有重要生态意义的行为,人们了解得还很少。此外,在北极地区,浮游动物群落的垂直迁移部分通常被视为一个单一的声散射层(SSL),其迁移模式受环境光直接控制,呈现同步性。在此,我们提供证据表明北极海洋系统存在迄今未知的复杂性,即浮游动物通过水柱形成多个聚集层,在声学上表现为不同的SSL。我们发现,虽然秋分期间DVM的起始受光介导,但白天迁移者的垂直定位与水体的热特性联系更为紧密,而非光照强度。夜间,浮游植物生物量是决定所有迁移类群垂直定位的最重要因素。此外,我们开发了一种以声像(SI)形式呈现声学数据 的新方法,能够基于每个潜在散射体后向散射的理论贡献,直接比较它们的相对重要性。基于对具有不同水文特征地点的比较,我们得出结论,北极地区持续变暖可能导致整个北极海洋系统出现更复杂的生态交错带。