Olli Kalle, Nyman Emil, Tamminen Timo
Centre for Limnology, Institute of Agricultural and Environmental Sciences, Estonian University of Life Sciences, Kreutzwaldi 5, Tartu 51006, Estonia.
Institute of Ecology and Earth Sciences, University of Tartu, Liivi 2, 50409, Estonia.
J Plankton Res. 2022 Jun 12;45(1):146-162. doi: 10.1093/plankt/fbac029. eCollection 2023 Jan-Feb.
We analyzed phytoplankton biodiversity trends in a 52 year (1967-2018) monitoring time-series from the archipelago of Helsinki, Gulf of Finland, the Baltic Sea. The community ordination revealed strong ordering of samples along the time axis (generalized additive model-gam fit: = 0.9). Species richness increased in time and was the most influential alpha diversity descriptor related to the community structure (gam fit: = 0.56-0.70). Changes in species richness accounted for 35-36% of the mean between-sample beta diversity. The remaining 64-65% was due to species turnover-the dominant component of the biodiversity trend. The temporal beta diversity trend reflected the eutrophication history of the geographically confined region, with a turning point in mid-1990s demarking the adaptation and recovery phases of the phytoplankton community. Trends in spatial beta diversity revealed homogenization of the communities in the outer archipelago zone, but not in the inner bays. The temporal decay of community similarity revealed high turnover rate, with 23.6 years halving time in the outer archipelago and 11.3 years in the inner bays, revealing the differences in eutrophication strength. The observed phytoplankton trends manifest the regional eutrophication history, and dispersal of new species to the unsaturated brackish species pool.
我们分析了来自波罗的海芬兰湾赫尔辛基群岛52年(1967 - 2018年)监测时间序列中的浮游植物生物多样性趋势。群落排序显示样本沿时间轴有很强的排序(广义相加模型 - gam拟合: = 0.9)。物种丰富度随时间增加,是与群落结构相关的最具影响力的α多样性描述符(gam拟合: = 0.56 - 0.70)。物种丰富度的变化占样本间平均β多样性的35 - 36%。其余64 - 65%归因于物种更替——生物多样性趋势的主导成分。时间β多样性趋势反映了这个地理受限区域的富营养化历史,20世纪90年代中期的一个转折点标志着浮游植物群落的适应和恢复阶段。空间β多样性趋势显示外群岛区域群落同质化,但内湾没有。群落相似性的时间衰减显示出高周转率,在外群岛半衰期为23.6年,在内湾为11.3年,揭示了富营养化强度的差异。观察到的浮游植物趋势体现了区域富营养化历史,以及新物种向不饱和咸淡水物种库的扩散。