First evidence of microplastic contamination in the supraglacial debris of an alpine glacier☆
Graphical abstract
Introduction
Accumulation of plastic polymer (hereafter plastic) items is one of the most ubiquitous and long-lasting changes to the earth surface that human activities have produced since mass production of plastic commenced in the 1950s (Barnes et al., 2009; Thompson et al., 2004). Concerns have been raised in recent years on the potential impacts of plastic on ecosystems. Plastic is persistent, it can easily accumulate in the environment and enter the trophic chain, and its impacts on ecosystems have already been demonstrated (Barnes et al., 2009; Cole et al., 2011; Wright et al., 2013). In recent years, particular attention has been focused on microplastics, plastic items smaller than 5 mm. They can be specifically produced to be used in diverse personal care products and in different industrial applications (i.e., primary microplastics), or can be generated by the break-down of macroplastics (secondary microplastics) (Eerkes-Medrano et al., 2015). Surveys on marine and freshwater ecosystems have been established to monitor the temporal trends in the amount of plastic items. Oceanic campaigns have estimated the amount of macro- and microplastics afloat in the sea, and the amount transported to sea by rivers from terrestrial ecosystems (Eriksen et al., 2014). Moreover, recent studies have demonstrated that microplastics can be transported to virtually any part of the globe, also in the so-called remote areas. Indeed, plastic fragments have been found in deep sea, Southern Oceans, Arctic and Antarctica (Hamid et al., 2018), as well as in sub-alpine lake sediments (Imhof et al., 2013), in pelagic water and shoreline debris from high-mountain lakes (Free et al., 2014; Zhang et al., 2016), and floodplain soils in Alpine valleys (Scheurer and Bigalke, 2018). In addition, recent evidence of atmospheric microplastic deposition in a remote, pristine mountain area of the French Pyrenees suggests that microplastics can reach and affect remote, sparsely inhabited areas far from emission sources through atmospheric transport (Allen et al., 2019). However, to the best of our knowledge, no published study has documented the occurrence and the amount of plastic items on glaciers so far.
Glaciers are accumulation sites for aerially transported debris and pollutants as glacier ice forms through the transformation of accumulated snowfalls, which are particularly efficient in scavenging contaminants, including small debris, from the atmosphere (e.g. Lei and Wania, 2004; Lovett and Kinsman, 1990). Temperate glaciers then flow down valley, and the ablation area of valley glaciers thus concentrates the debris and the contaminants collected over the much vaster accumulation area of the glacier (Nakawo et al., 1986). For this reason, supraglacial debris is particularly rich in air-transported pollutants (Cook et al., 2016; Pittino et al., 2018), including radionuclides (Baccolo et al., 2017; Łokas et al., 2016). We thus hypothesized that similar processes may act also for microplastics, and we present here the first evidence of the occurrence and the first estimate of the amount of microplastic in the supraglacial debris of a large valley glacier in the Italian Alps.
Section snippets
Study area
This study was carried out on the ablation tongue of Forni Glacier, one of the widest Italian glaciers, with a total surface area of 11.34 km2 and an ablation area of 0.59 km2 (Azzoni et al., 2018). This glacier is located in the Ortles-Cevedale group (Stelvio National Park, Central Italian Alps) and is rather close to the highly urbanized areas. For instance, the town of Sondrio (∼21,000 inhabitants) is 58 km from the Glacier, and those of Brescia (∼197,000 inhabitants), Bergamo (∼120,000
Results and discussion
We found 2–7 plastic fragments per sample that correspond to 74.4 ± 28.3 SE items kg−1 of sediment (dry weight) on average, with no difference between cryoconite (70.5 ± 32.9 items kg−1) and sparse and fine supraglacial debris (78.3 ± 30.2 items kg−1) (see Supporting Information; Table S1). No plastic item was found in blank samples. Fibres represented 65.2% and fragments 34.8% of items in all samples pooled. Both microplastic fragments and fibres were of diverse colour (Fig. 1). Overall, most
Conclusion
Our findings of microplastic contamination on glaciers, albeit not unexpected, demonstrated that also this contaminant can reach remote, high mountain areas. When trapped in the sediment, microplastics can persist on glaciers for an unknown amount of time and there is therefore the potential for long-term persistence of microplastic on glaciers, which may have already accumulated an unknown amount of plastic since the 1950s, when plastics have started to be released in the environment. These
Conflicts of interest
The authors declare no conflict of interest.
Acknowledgements
The authors warmly thank two anonymous reviewers whose comments greatly improved the quality of the manuscript.
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This Paper has been recommended for acceptance by Lei Wang.