A study of prehistoric animals has revealed the crucial role of the
English Channel in shaping the course of Britain's natural history.
The Channel acted as a filter, letting some animals in from
mainland Europe, but not others.
Even at times of low sea level, when Britain was not an island,
the Channel posed a major barrier to colonisation.
This was because a massive river system flowed along its bed, UK
researchers told a palaeo-conference in Gibraltar.
Today the English Channel is 520km long, 30-160km wide, about
30-100m in depth and slopes to the south-west.
Even now, the bed of the Channel is incised by a network of
valleys, the remains of the river system, which may have been cut by
catastrophic drainage of meltwater from further north.
"It would have been an incredible barrier at times of high sea
level, but it would also have been a formidable barrier at times of
low sea level for populations trying to move south to north," said
Chris Stringer of London's Natural History Museum.
Professor Stringer presented the results here at the Calpe
conference, a meeting of pre-history experts from all over the
world.
The big flood
The evidence comes from the Ancient Human Occupation of Britain
Project (AHOB). This five-year undertaking by some of the UK's
leading palaeo-scientists has reassessed a mass of scientific data
and filled in big knowledge gaps with new discoveries.
Chris Stringer's co-researchers Andy Currant, Danielle Shreve and
Roger Jacobi have been studying how the mammal fauna of Britain has
changed over the last 500,000 years.
The remains we find today tell a story of Britain's ancient past
During that period, animals have colonised, abandoned and
re-colonised Britain many times as the climate shifted from warm to
cold and back to warm.
The Channel is thought to have formed during a cold period
200,000 years ago or more.
Meltwater from an ice sheet formed a lake, which then overflowed
in a catastrophic flood - cutting through a chalk ridge that
previously connected Britain to France.
Changes in climate were accompanied by changing sea levels. At
the height of an ice age, these would have been low. During
interglacial periods, when the climate was warm, sea levels rose.
But even when water was locked up in the ice sheets and sea
levels plummeted, the Rhine and the Thames rivers dumped meltwater
into a major river system that flowed along the floor of the
Channel.
Unusual collections
This means that once the Channel formed, there was never again a
simple land crossing to be made from northern France to Britain.
"We find we're getting only a selection of the mammals during the
British interglacials that there are in mainland Europe," said
Professor Stringer.
For example, at one pre-historic site, researchers found
hippopotamus and fallow deer; but unlike mainland Europe at the
time, there were no horses and no humans.
"This suggests that the Channel, or the Channel river system, is
acting as a filter to prevent the movement of some of these [mammal]
forms into Britain," Professor Stringer added.
Once sea levels rose high enough for Britain to be an island, the
select fauna that had made it across from mainland Europe could
develop in extraordinary ways.
During one warm stage, about 80,000 years ago, fossils from
Banwell Cave in Somerset show Britain was populated by some very
unusual animals. These included reindeer, bison, and a giant bear
similar to a polar bear.
Interestingly, there are no hyena fossils at Banwell Cave, as
there were in mainland Europe. Instead, it appears, their role in
the food chain may have been taken up by wolves.
"The wolves were developing much larger jaws. Their teeth show
incredible signs of breakage and wear as if they're chomping bones
like hyenas," said Professor Stringer.
The mammals at Banwell seem to be the kinds of animals normally
found today in cold regions. But they lived in Britain during a warm
stage and seemed to be adapting to their new environment.
The team thinks the antecedents of these animals must have
arrived in Britain when the climate was cold. But when conditions
warmed up, sea levels rose and isolated Britain, marooning this
cold-adapted fauna in a warm environment.
See how the English Channel changed through time
The history of humans and other animals in Britain
Major incursions were possible during periods of warmth
A number of important palaeo-sites mark the periods of influx
Extreme cold made Britain uninhabitable for thousands of years