Laboratorio de Limnología, Departamento de Acuicultura y Recursos Agroalimentarios, Universidad de Los Lagos, Campus Osorno, Osorno, Chile.
Laboratorio de Limnología, Departamento de Acuicultura y Recursos Agroalimentarios, Universidad de Los Lagos, Campus Osorno, Osorno, Chile; Centro de Investigación en Recursos Naturales y Sustentabilidad (CIRENYS), Universidad Bernardo O'Higgins, Avenida Viel 1497, Santiago, Chile.
Sci Total Environ. 2022 Feb 10;807(Pt 3):150978. doi: 10.1016/j.scitotenv.2021.150978. Epub 2021 Oct 14.
In June 2011 the Puyehue-Cordón Caulle volcanic complex (PCCVC) erupted, ejecting around 950 million metric tons of volcanic ash and pyroclastic rock, generating habitat destruction, environmental deterioration and devastation of ecological communities in rivers near the volcanic fissure. We evaluate the long-term effect of this eruptive event on the recovery of the diversity of aquatic macroinvertebrates, collecting biological and environmental information from 2011 to 2018 in visibly impacted Chilean rivers (Gol-Gol and Nilahue) and not visibly impacted rivers (Calcurrupe and Chanleufu). With the macroinvertebrate records we developed a recovery coefficient based on their diversity before and after the eruption. The results show that before the eruption (2009-2010), the accumulated family richness and mean diversity in the Gol-Gol River were higher than that observed post-eruption in rivers visibly impacted and not visibly impacted. Between 2013 and 2018, 17 families recolonized the Gol-Gol River, as well as 10 new families that were not recorded before the eruption. The richness of families post-eruption was negatively related to the increase in the concentration of total suspended solids, affecting the successional changes and recovery in the medium term. The recovery coefficient indicates that seven years after the eruption the diversity of macroinvertebrates still shows lower levels than those recorded before the eruptive event, with predominance of a slow recovery phase. Families of orders Ephemeroptera, Plecoptera and Trichoptera that were dominant before the eruption of the PCCVC began to recover the richness of taxa two years later, Plecoptera reaching 50% recolonization in 2018, Ephemeroptera 33.3% and Trichoptera 30%. In contrast, Diptera reached 100% recovery by 2018 and chironomids increased since 2015, becoming the dominant taxon during intermediate recovery in the Gol-Gol River. The recovery of macroinvertebrates in the Gol-Gol River is related to their modes of dispersal, feeding and the decrease in ash concentration.
2011 年 6 月,普耶韦-科登-卡尔布火山复合体(Puyehue-Cordon Caulle Volcanic Complex,PCCVC)喷发,喷出约 9.5 亿吨火山灰和火山碎屑岩,破坏了火山裂隙附近河流的栖息地,导致环境恶化和生态群落破坏。我们评估了这次喷发事件对水生大型无脊椎动物多样性恢复的长期影响,从 2011 年到 2018 年,在受明显影响的智利河流(戈尔戈尔河和尼拉乌埃河)和不受明显影响的河流(卡尔库里普河和查莱乌富河)收集生物和环境信息。根据喷发前后的多样性,我们用大型无脊椎动物的记录建立了一个恢复系数。结果表明,喷发前(2009-2010 年),戈尔戈尔河的累积科丰富度和平均多样性高于喷发后受明显影响和不受明显影响的河流。2013 年至 2018 年间,17 个科重新出现在戈尔戈尔河,其中 10 个是喷发前未记录的新科。喷发后科的丰富度与总悬浮物浓度的增加呈负相关,影响了中期的演替变化和恢复。恢复系数表明,喷发后七年,大型无脊椎动物的多样性仍低于喷发前的水平,处于缓慢恢复阶段。在 PCCVC 喷发之前占主导地位的蜉蝣目、襀翅目和毛翅目科开始在两年后恢复分类群的丰富度,襀翅目在 2018 年达到 50%的再殖民化,蜉蝣目 33.3%,毛翅目 30%。相比之下,2018 年摇蚊目达到 100%的恢复,并且 2015 年以来,摇蚊目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目目