How to Build the White Cliffs of Dover

By Tom Evans

The White Cliffs of Dover are one of Britain’s greatest natural wonders. Indeed, the oldest known name for our sceptered isle is Albion—based on the Indo-European root for “white”, an allusion to this majestic landscape. The cliffs, which reach up 110 metres high, are composed of a fine, soft chalk that mostly consists of layers of intricate structures known as coccoliths, thin plates of calcium carbonate.

public domain, no creditThe plates are produced by microscopic photosynthetic algae in the sea known as coccolithophores and these single-celled creatures assemble their plates to form a protective shell, known as a coccosphere. The most abundant of these algae is Emiliania huxleyi, or EHUX. This algae is famous for its ability to bloom: dense populations of the phytoplankton can cover up to 100,000 square kilometers and are easily visible by satellites in orbit as the chalk plates turn the colour of the water a milky white.

Eventually the bloom fades away as the algae gradually die. And remarkably, their cause of death is quite often a virus. We usually think of viruses living in the air or inside our bodies, but in fact the ocean is teeming with viruses – up to as many as 100 billion viruses can be found in just one litre of seawater! EHUX virus 86 infects the algal bloom, and just as quickly as they bloomed, the algae die off. When the algae die, their coccosphere sinks to the seabed. Their boom and bust lifestyle means it gradually accumulates. And if you wait a few million years you end up with the vast and glittering White Cliffs of Dover.

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