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Field Research Laboratories for Trace Metal Ecotoxicology Cambridge.Org/Mbi Philip S Journal of the Marine Mining-contaminated estuaries of Cornwall – Biological Association of the United Kingdom field research laboratories for trace metal ecotoxicology cambridge.org/mbi Philip S. Rainbow Department of Life Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK Review Abstract Cite this article: Rainbow PS (2020). Mining- contaminated estuaries of Cornwall – field A century or so after the cessation of almost all mining in Cornwall, certain estuaries still have research laboratories for trace metal extremely high sediment concentrations of toxic trace metals, particularly copper and arsenic, ecotoxicology. Journal of the Marine Biological but also lead and zinc. These high trace metal loadings in the sediments are to a large degree Association of the United Kingdom 100, bioavailable to the local infauna, especially sediment-ingesting invertebrates. Some sediment 195–210. https://doi.org/10.1017/ S002531541900122X trace metal bioavailabilities are so high as to be of ecotoxicological concern, with deleterious effects on the local biota at levels of biological organization up to and including changed com- Received: 29 April 2019 munity structure. The estuaries of interest here are those of the Rivers Carnon (Restronguet Revised: 6 December 2019 Creek), Tamar (and Tavy), Gannel, West Looe and Hayle. These estuaries are especially Accepted: 19 December 2019 attractive field sites for comparative trace metal ecophysiology and ecotoxicology research First published online: 10 January 2020 for they lack the confounding presence of other anthropogenic contaminants inevitably pre- Key words: sent in most estuaries in the developed world. The estuaries also offer a range of combinations Comparative ecophysiology; ecotoxicology; of different trace metals and a comparative gradient of sediment bioavailabilities of these trace Gannel; Hayle; Restronguet Creek; Tamar; West metals. Looe Author for correspondence: Philip S. Rainbow, E-mail: [email protected] Introduction Mention of Cornwall today raises a vision of a county with holiday beaches and picturesque villages snuggling in coves along a spectacular rugged coast, the home ports of flotillas of small fishing boats. But ‘twas not ever thus. Cornwall in the 19th century and earlier was a mining region of national and international importance, a major player in the world produc- tion of trace metals such as tin and copper, and the metalloid arsenic (included here for con- venience as a trace metal). Then, throw in lead, zinc, iron and historically some silver, as well as much lower amounts of tungsten, manganese, antimony, cobalt, nickel and molybdenum (Dines, 1969; Rainbow, 2018). The mining of the ores of these metals, all potentially toxic, inevitably led to deleterious environmental impacts on local terrestrial habitats, with serious knock-on effects in the streams and rivers draining these mining areas and ultimately their estuaries (Rainbow, 2018). This review highlights the point that several of these Cornish estuaries still today contain sediments derived from mining activities with extremely high concentrations of toxic trace metals. Much of these sediment-associated metals are bioavailable to estuarine biota such as burrowing invertebrates ingesting the sediment as a food source and are of ecotoxicological significance today, decades or more than a century after the cessation of mining in their catchment. These Cornish estuaries are the outflow points of rivers that are very short, barely tens of kilometres long, typically draining catchments without large conurbations or regions of other industrial development. So, unlike most estuaries today, these metal-contaminated estuaries of Cornwall all but lack the usual associated presence of so many other toxic con- taminants resulting from today’s industrialized society – for example organic contaminants such as hydrocarbons in oil, organochlorines (e.g. PCBs) and their ilk. As a result these trace metal-contaminated estuaries provide ideal comparative field sites to study the eco- toxicological effects of high trace metal loadings in estuaries without the confounding effects of these other contaminants. © Marine Biological Association of the United Mining in south-west Britain Kingdom 2020 In Britain, metal ores typically occur in mineral veins in areas where, in the geological past, a mass of igneous granite has been intruded into overlying sedimentary rock strata, causing frac- turing in these strata (Dines, 1969). Hot hydrothermal fluids containing metal salts enter the fractures from below during the intrusion. On cooling these metal salts deposit as veins of metal ores (Dines, 1969). There is an order of deposition of the different ores as temperatures cool, so that they take up a zoned arrangement with depth – tin deepest, then copper, lead, zinc (these two often together) and finally iron in ascending order (Perkins, 1972). Ores of secondary metals are associated with these primary metal ores – tungsten in the tin zone, arsenic in the copper zone, and silver in the lead/zinc zone. The idealized vertical succession of the metal ores may be displaced laterally and often the full vertical succession of metal ore zones will not be present. Furthermore there may be secondary weathering of the metal salts Downloaded from https://www.cambridge.org/core. IP address: 170.106.35.76, on 30 Sep 2021 at 16:10:01, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S002531541900122X 196 Philip S. Rainbow first deposited, for example the oxidation of metal sulphides to of ores of copper and arsenic in the county led to the ecotoxico- oxides and, particularly in the presence of limestone, carbonates. logical predominance of these two trace metals. In what is now south-west England there was a major moun- But what of tin and iron in the aquatic ecosystems of tain building event in the Carboniferous and early Permian, and Cornwall? As it happens neither is a major direct source of granite masses were intruded into overlying sedimentary rock aquatic ecotoxicity. Tin is predominantly found as cassiterite strata (sandstones, mudstones and siltstones) which had typic- (tin oxide), known in Cornwall and Devon as black tin. Tin in ally been laid down in the Devonian period (Dines, 1969). In this form is very strongly bound and not easily released from south-west England today, there are five major granite intru- the ore in dissolved form into fresh water or estuarine waters to sions protruding through the Palaeozoic strata – those of impact directly on the local aquatic biota. The major detrimental Land’s End, Carnmenellis (the area of west Cornwall between environmental impact, for example of tin streaming, is by physical Redruth, Helston and Penryn), St Austell Moor, Bodmin Moor smothering of the flora and fauna by fine sediment. Iron released and Dartmoor (Dines, 1969). The veins containing metal ores into solution from its common sulphide ore iron pyrite rapidly are usually on the margins of the granite intrusions, with tin and oxidizes in oxygenated waters to form iron oxides and hydroxides copper veins expected closer to the edge of the granite, and lead which are practically insoluble and precipitate from the water and zinc veins potentially further away (Dines, 1969). Today the column as ochre. There is little toxic dissolved iron left in solu- granite masses are typically exposed above the Palaeozoic rocks tion in most streams but ochre too has a physical blanketing into which they were intruded, for weathering has stripped off effect to cause depletion of the flora and fauna of streams and much of any remaining cover. rivers. Any remaining dissolved iron, more pronounced for BackintheBronzeAge,tinandcopper,theveryingredients example in acidic fresh waters, will be transported downstream of bronze, were highly sought after. The tin and copper mines to the estuary. Here the dissolved iron ions encounter the of Cornwall were of great international significance, particu- more alkaline pH caused by the admixture of seawater, again larly during the second millennium BC (Atkinson, 1985, promoting precipitation of the dissolved iron as iron oxides 1987; Buckley, 1992). The initial sources of tin ore were alluvial and hydroxides to be incorporated into the now estuarine sedi- deposits in streams and rivers draining catchments with a high ment (Bryan & Gibbs, 1983). Furthermore, the formation of par- representation of tin. These ores were concentrated by the pro- ticulate iron oxides and hydroxides provides surfaces for the cess of tin streaming which caused huge amounts of sifted sedi- adsorption of certain other trace metals including copper and ment to accumulate downstream, particularly at the top of arsenic. These trace metals come out of solution to be deposited the estuaries of the rivers (Buckley, 1992; Rainbow, 2018). in the estuarine sediments in association with the particulate Later, the outcropping of veins containing tin in sea cliffs iron oxides and hydroxides (Bryan & Gibbs, 1983;Langston, such as at Geevor in the St Just area and at St Agnes offered 1983; Bryan & Langston, 1992). a further accessible source of tin in Cornwall. Similarly copper- In contrast to tin and iron, copper, arsenic, lead, zinc and silver rich veins could also be clearly seen in the cliffs at St Just, do have the potential to offer a direct ecotoxicological challenge in Illogan, St Agnes and Perranzabuloe. Mining for tin and cop- dissolved form
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