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Elodea, the great invader

Elodea colonising europe

British biologists called Elodea 'Canadian pondweed', suggesting that they knew where it originally came from. It was observed in Scotland at Berwick-upon-Tweed in August 1842, and this is the first recorded sighting in Britain.

The arrival in England appears to been delayed for five years, when it was found growing in reservoirs at Foxton locks near Market Harborough in Leicestershire. It was probably brought in from Canada attached to timber imported for building the railway at Rugby.

Elodea spread rapidly from Foxton locks: within twelve months it was very common in Northamptonshire and Nottinghamshire. A year later it was well established in Staffordshire, Warwickshire and Derbyshire.

Cuttings from the Foxton Lock plants were grown in a tub at the Botanical Gardens in Cambridge in 1848. The curator, a Mr Murray, introduced the plant into a waterway running alongside the Gardens. By 1851 it had choked the rivers Cam and Ouse, and much of the low-lying fens of Cambridgeshire and Lincolnshire. At this time it was a major problem to boats trying to sail through the waterways.

Elodea continued its rapid advance through Europe: France and Belgium by 1860, Germany by 1865. By 1870 it had reached east to Russia and Hungary and north to Denmark and Sweden. Its advance was stopped at about 66° N by the low temperatures.

Elodea is still common in all of the areas that it colonised, but it is no longer clogging up the rivers in the way that it once did. Elodea grows vigorously for a few years after colonising a new area, and takes over the waterways. After about five years its growth slows down, and it stops being a troublesome weed. No one fully understands why, but it is thought that the amount of iron at the bottom of the streams and lakes might be a limiting factor for further growth.

If your school has a pond, try and find out how quickly the Elodeais growing. It may have already started to slow down. Some people think that it grows best when there is little oxygen in the mud at the bottom of the pond.