Seregin Alexey P
Department of Geobotany, Faculty of Biology, Lomonosov Moscow State University, Moscow, Russia, 119991,
Environ Sci Pollut Res Int. 2014 Nov;21(22):12883-97. doi: 10.1007/s11356-014-3152-9. Epub 2014 Jul 1.
Eutrophication remains a major threat to the flora of Western Europe despite measures to reduce nitrogen emissions. Although nutrient enrichment has been recorded for both inland waters and adjacent seas, there is almost no evidence from Russia for large-scale anthropogenic eutrophication of soils and its impact on terrestrial biota. I used the distribution grid data (337 grid squares, ca. 96 km(2)) on 1,384 vascular plants of Vladimir Oblast for two periods (1869-1999 vs. 2000-2012) to estimate the shifts in mean Ellenberg's indicator values for nitrogen and soil reaction. Decadal changes in the flora of acid sandy Meshchera Lowlands were observed directly during two grid surveys of 2002 and 2012 based on a coarser grid (50 squares, ca. 24 km(2)). Despite the spatial correlation of Ellenberg's indicator values for soil reaction and nitrogen, mean grid values for nitrogen are growing in areas with both acid and neutral soils. The changes in mean grid indicator values for nitrogen are caused by either local extinctions of species from nutrient-poor habitats or spread of nitrophilous plants. I found that oligotrophic habitats are declining rapidly within the eutrophic loamy landscapes. In contrast, changes in landscapes with acid sandy soils are caused by increasing number of records of nitrophilous species, both invasive and native. These two processes have different spatial patterns caused by varying levels of geochemical buffer capacity and should be considered separately. Fragmentary historical data on Vladimir Oblast flora agrees with the overall European picture of eutrophication in the twentieth century.
尽管采取了减少氮排放的措施,但富营养化仍然是西欧植物群面临的主要威胁。虽然在内陆水域和邻近海域都有营养物质富集的记录,但在俄罗斯,几乎没有证据表明土壤存在大规模人为富营养化及其对陆地生物群的影响。我利用弗拉基米尔州1384种维管植物在两个时期(1869 - 1999年与2000 - 2012年)的分布网格数据(337个网格方块,约96平方千米)来估计氮和土壤反应的平均埃伦贝格指示值的变化。基于更粗的网格(50个方块,约24平方千米),在2002年和2012年的两次网格调查中直接观察了酸性沙质梅谢拉低地植物群的年代际变化。尽管土壤反应和氮的埃伦贝格指示值存在空间相关性,但在酸性和中性土壤地区,氮的平均网格值都在增加。氮平均网格指示值的变化是由贫营养生境中物种的局部灭绝或嗜氮植物的扩散引起的。我发现,在富营养化的壤土地景观中,贫营养生境正在迅速减少。相比之下,酸性沙质土壤景观的变化是由嗜氮物种(包括入侵物种和本地物种)记录数量的增加引起的。这两个过程由于地球化学缓冲能力水平不同而具有不同的空间模式,应分别加以考虑。弗拉基米尔州植物群的零碎历史数据与20世纪欧洲富营养化的总体情况相符。