Bog wood: the Caledonian forest and climate change
| Exposed bogwood on the shores of the channel between Loch Bad an Sgalaig and Dubh Loch, near Gairloch |
I recently read Emma Wood's 'Peatbogs, Plague and Potatoes', an excellent book that traces the evolution of the landscape we see around us today and provides a particularly good account of the chronology of afforestation and deforestation since the end of the last ice age. She concludes that climate change rather than human activity was responsible for the decline of the great forests that once cloaked the Scottish landscape.
Over the years I have heard many theories regarding about how Scotland transformed from forest to bog: that the trees had been chopped down by farmers; eaten by over stocked sheep and deer; consumed by wood hungry industrial activity such as shipbuilding or iron smelting. Doubtless all of those causes have played a part at various points in history and in the present day, but when evidence from pollen samples preserved in loch sediments are considered alongside indicators of past climate such as Greenland ice cores, the evidence points to the main culprit being the worsening climate. The loss of tree cover from areas with little or no human intervention, such as Rannoch Moor, supports this version of events.
The age of the landscape that we see around us today is measured not, like the age of the underlying rocks, in millions or even billions of years, but in mere thousands. The individual landforms that make up this landscape, the glacier sculpted hills, the mounds of meltwater transported rock and gravel, did not exist until the ice receded at the end of the last ice age around 11,000 years ago.
Though the landforms themselves have maintained broadly the same shape since the ice melted, they have appeared in various guises. For a couple of hundred years after the ice melted the landscape would have been of bare tundra, home to mammoths, woolly rhinoceros, elk, wild horses, reindeer, Arctic fox and lemmings. Once soil formed from the glacial till, around 11,000 years ago, trees began to colonise the land, obscuring the landforms. At first there were tundra plants: willow, juniper and rowan. Then followed birch and hazel. Finally, 8 - 9 thousand years ago came elm, oak and Scots pine. As the climate continued to warm, this mixed forest cover reached up the flanks of the mountains. Of the tundra animals only the elk adapted, but forest animals walked over the land bridge that connected Britain to continental Europe to colonise this newly formed habitat; red and roe deer, a massive bovine called an auroch, wild boar, badgers, squirrels, otter, beaver, lynx, bear and wolves. In short, Scotland was at least as diverse an environment as the contemporary north American wilderness, literally teeming with animal life.
a turn for the worse. Conditions had been getting warmer, reaching an optimum around six thousand years ago. This warming was also melting the polar ice caps and around this time the sea levels rose sufficiently to make Britain was an island, and by five thousand years or so ago the conditions were warm and dry enough to be unfavourable to large stands of trees. Meanwhile agriculture was becoming more established and Neolithic monument building was nearing its peak.
Labels: Climate, climate change, Landscape interpretation, prehistory, scotland





