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珊瑚生长带记录了与 Fundão 水坝溃坝事件相关的微量元素。

Coral growth bands recorded trace elements associated with the Fundão dam collapse.

机构信息

Programa de Pós-Graduação em Ecologia and Núcleo Professor Rogério Vale de Produção Sustentável-SAGE/COPPE, Universidade Federal do Rio de Janeiro, 21941-900 Rio de Janeiro, RJ, Brazil.

Programa de Pós-Graduação em Ecologia and Núcleo Professor Rogério Vale de Produção Sustentável-SAGE/COPPE, Universidade Federal do Rio de Janeiro, 21941-900 Rio de Janeiro, RJ, Brazil; Departamento de Tecnologias e Linguagens, Instituto Multidisciplinar, Universidade Federal Rural do Rio de Janeiro, 26020-740 Nova Iguaçu, RJ, Brazil.

出版信息

Sci Total Environ. 2022 Feb 10;807(Pt 2):150880. doi: 10.1016/j.scitotenv.2021.150880. Epub 2021 Oct 9.

Abstract

In November 2015, the collapse of the Fundão dam (Minas Gerais, Brazil) carried over 40 × 10 m of iron ore tailings into the Doce river and caused massive environmental and socioeconomic impacts across the watershed. The downstream mudslide scavenged contaminants deposited in the riverbed, and several potentially toxic elements were further released through reduction and solubilization of Fe oxy-hydroxides under estuarine conditions. A turbidity plume was formed off the river mouth, but the detection of contaminants' dispersion in the ocean remains poorly assessed. This situation is specially concerning because Southwestern Atlantic's largest and richest reefs are located 70-250 km to the north of the Doce river mouth, and the legal dispute over the extent of monitoring, compensation and restoration measures are based either on indirect evidence from modeling or on direct evidence from remote sensing and contaminated organisms. Coral skeletons can incorporate trace elements and are considered good monitors of marine pollution, including inputs from open cut mining. Here, we studied a Montastraea cavernosa (Linnaeus 1767) coral colony collected 220 km northward to the river mouth, using X-rays for assessing growth bands and Laser Ablation Inductively Coupled Plasma Mass Spectrometry to recover trace elements incorporated in growth bands formed between 2014 and 2018. A threefold positive Fe anomaly was identified in early 2016, associated with negative anomalies in several elements. Variation in Ba and Y was coherent with the region's sedimentation dynamics, but also increased after 2016, akin to Pb, V and Zn. Coral growth rates decreased after the disaster. Besides validating M. cavernosa as a reliable archive of ocean chemistry, our results evidence wide-reaching sub-lethal coral contamination in the Abrolhos reefs, as well as different incorporation mechanisms into corals' skeletons.

摘要

2015 年 11 月,费顿大坝(巴西米纳斯吉拉斯州)崩塌,超过 40×10^6 立方米的铁矿石尾矿流入多斯雷斯河,对整个流域造成了巨大的环境和社会经济影响。下游的泥石流扫荡了河床中沉积的污染物,而在河口条件下,铁的氧化氢化物的还原和溶解进一步释放了几种潜在的有毒元素。河口形成了一个浑浊带,但污染物在海洋中的分散情况仍未得到很好的评估。这种情况特别令人担忧,因为南大西洋最大、最富有的珊瑚礁位于多斯雷斯河口以北 70-250 公里处,关于监测、赔偿和恢复措施范围的法律争议要么基于建模的间接证据,要么基于遥感和受污染生物的直接证据。珊瑚骨骼可以包含微量元素,被认为是海洋污染的良好监测物,包括露天采矿的输入。在这里,我们研究了一个采集于多斯雷斯河口以北 220 公里处的 Montastraea cavernosa(Linnaeus 1767)珊瑚群,使用 X 射线评估生长带,并用激光烧蚀电感耦合等离子体质谱法恢复在 2014 年至 2018 年间形成的生长带中包含的微量元素。2016 年初,我们发现了三倍的正铁异常,与几个元素的负异常相关。钡和钇的变化与该地区的沉积动力学一致,但在 2016 年后也增加了,类似于铅、钒和锌。灾难发生后,珊瑚的生长速度下降了。除了验证 M. cavernosa 是海洋化学的可靠档案外,我们的结果还证明了阿布鲁罗什珊瑚礁的广泛的亚致死珊瑚污染,以及不同的元素在珊瑚骨骼中的结合机制。

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