‘Trees for Life’ and ‘Woodland Trust Scotland’ are trying to revive lost pinewoods, that once formed part of the Caledonian Forest.  This forest supported a rich and diverse flora and fauna, including serrated wintergreen, distinctive lichens, crossbills, capercaillie, wild cats and red squirrels.   After the last Ice Age, plant and animal species moved across the 'land bridge' that connected us with continental Europe.   Pines (Scots Pine aka Pinus sylvestris) were ‘quick’ to move into Scotland and the land vacated by the glaciers.  Now less than 2% of this once great forest survives. To find pockets of ancient and ‘lost’ pine trees, these two organisations have adopted a number of approaches. Making use of old maps and texts, for example, those produced by the Reverend Timothy Pont (a Scottish minister and cartographer) in the 1500s. He was the first to produce a detailed map of Scotland.  These can point to areas that were formerly populated by “fir trees”, ie pine. Examining Gaelic place names, which might reference woodland or pine trees. Using the original ordnance survey maps (which often had fir tree symbols) to produce digital copies, which can be overlain on modern maps - hopefully to reveal former woodland sites. Using ecological evidence.  For example, wild pine often grows with old birch trees, whereas planted pine is usually found with larch and other ‘commercial conifers’. Old pine trees often have a distorted shape, with thick, gnarled and twisted trunks; they survive in remote gorges and crags.  Areas that previously supported wild pine, often have old stumps still present and / or certain distinctive lichens / plants - remnants of once diverse ecosystem. Using these various techniques, dozens of lost pine woodland areas have been identified and located.  Much of the original Caledonian Forest was lost through felling (for timber and / or fuel) over the centuries.   Later came sheep farming and this was followed in Victorian times by deer and grouse shooting.  In the last century, commercial forestry resulted in the further loss of ancient woodland. However, restoration is possible.  Where some old trees have survived, there is often a seed bank in the soil and these seeds can germinate if the dense canopy of commercial conifers is removed.  Many pine seeds that do germinate are lost as seedlings due to grazing due to deer or sheep - who seem to prefer them to Sitka etc.  Hopefully as areas with pine grow on, so other species such as rowan, birch and hazel will develop and in time a ‘full’ woodland will develop.

In 2018, the blog reported on the extensive fires in Sweden, a country noted for its forests and woodlands, which cover approximately half of the country. Once the trees were mainly broad leaved species, but then oaks and alders began to decline.  By the middle of the  twentieth century,  Spruces and Pines were dominant.  This was mainly due to forestry management, to produce wood for fuel, charcoal [used in iron smelting], potash, tar and timber (for building). Fires burnt from the extreme north down to Malmo in the south. These fires affected some 20,000 hectares and destroyed woodlands valued at [circa] £50 million.  Now work by scientists at Uppsala University, the Swedish University of Agricultural Sciences (SLU), and the Swedish Meteorological and Hydrological Institute (SMHI) have examined the effects of the fires (of 2014) in the Vastmänland province, where the fires were ferocious, burning down into the soils. They have found that the 'forested areas' continued to lose carbon for several years after the fire, and that nitrate and phosphate input to streams and rivers increased after the fires. This spring and summer have again witnessed intense and widespread fires across the Mediterranean region, Canada and the United States. Fires are a problem not only because of their immediate destructive potential, but because they result in the release of carbon dioxide - which further contributes to global warming and climate change.  The United Nations Secretary-General said recently “The era of global warming has ended; the era of global boiling has arrived.” Data on these fires is not available as yet, but studies of the boreal fires in 2021 suggest those fires released some 1.76 billion tonnes of carbon dioxide into the atmosphere.  The fires contributed nearly one quarter of world wide carbon dioxide emissions from fires in that year.  [caption id="attachment_35352" align="aligncenter" width="650"] Woodland recovering from a fire[/caption] Boreal forests store roughly twice as much carbon in their trees and soil as tropical forests.  These forests (often referred to as the Taiga) surround the Arctic Circle and research suggests the Taiga is warming faster than the global average, so areas like Northern Canada and Siberia now experience more heat and drought than in the past, and consequently are more likely to suffer from fires. Clearly, when there is a fire, carbon dioxide (and many other carbon compounds eg soot / small particles) are released by the burning of the trees but there is also the effect of fire on the soil and its organic content - the humus.   Research indicates that during the fires in the boreal area some 150 tonnes of carbon dioxide may be released into the atmosphere per hectare.  Furthermore, even after the fire, carbon continues to be lost from the soil.  It may take some three years for carbon uptake by the soil to be recorded.   Fires also lead to the rapid loss (leaching) of nutrients (e.g. phosphate) to local lakes and rivers - as there is little or no vegetation to absorb the nutrients.   Rainfall is not intercepted by vegetation and so the flow of streams increases ( sometimes by 50%).    A research paper produced by the Desert Research Institute (in Nevada) has indicated that smoke from the burning of pines has the effect of making soil particles more water-repellent.  This repellency of smoke-affected soil particles could help explain the increased flooding, erosion, and surface runoff in fire damaged areas.  

Checking through my emails, I came across a link sent by a friend to one of the winter talks in the program offered by the Botanical Society of Scotland - specifically “The Scottish Uplands: how to revive a degraded landscape” by Dr Helen Armstrong.  The talk was live-streamed but was also recorded and is available here.   Dr Armstrong spent 24 years at the Nature Conservancy Council, the Macaulay Land Use Research Institute, Scottish Natural Heritage and Forest Research carrying out research and advisory work. The following is an attempt to summarise some of the key features of her informative and enlightening talk. Read more...

The autumnal fall of leaves in deciduous trees is a well recognised event; their changing colours prior to being shed often make for spectacular displays - the New England Fall. Evergreens (with certain exceptions) do not undergo a similar loss of leaves but that is not to say that their leaves are forever green or permanent.  Indeed, each year, evergreens have a seasonal drop of their needle-shaped leaves, it is normal part of the tree’s cycle.  The leaves / needles of conifers have varying life spans; they are not a ‘permanent fixture’.  Many conifer needles will turn yellow then as they age, falling off the tree after one to several years. This change can be gradual or in some species quite rapid.  White Pines (Pinus strobus) typically retain their leaves for 2 to 3 years, whereas Scots Pines (Pinus sylvestris) usually retain their needles for three years. Larches, which are conifers (Larix sp) are somewhat unusual in that they shed their leaves every autumn.  The stress that a tree experiences through drought may result in more rapid browning and greater loss of leaves. Read more...

Pine trees are found across the world, there are over one hundred different species.  Many are native to the coniferous forests  (Taiga) of the Northern Hemisphere.  Their evergreen needles (leaves) offer shade in summer, and the trees may offer a degree of shelter from the winds of autumn and winter.  Gardeners and foresters 'like' Pines as they generally tolerate nutrient poor and somewhat dry soils.   In the period after WW2,  considerable areas of ‘low grade’ land were pressed into service (in the U.K.).   Areas around Thetford and Kielder were used, as were some sandy coastal sites (for example,  Holkham in Norfolk) and many large tracts of land in Scotland.  Pines are central to the business of agroforestry in places like the U.K,  New Zealand and Brazil, providing a source of lumber.    Read more...

As we sat outside The Middle Earth pub on Whitby’s harbour front, enjoying the early evening autumn sunshine, my wife looked at me and said “There’s something I want to talk to you about”. For a heart stopping moment my mind raced and I felt a mixture of emotions as I feared some dreadful news was coming my way. Instead, Jackie completely floored me by asking “How do feel you about us buying a wood?”   In the first instance I was speechless then apprehensive, confused and finally, elated!   Looking back, how I managed to hold onto my pint I’ll never know. Read more...

Half term is coming, and perhaps you will be visiting your own wood  or walking through woodland during the holiday period.   Below is a simple activity (that you could supervise) which might interest younger members of the family. Did you know that sometimes pine cones stay on the trees for some years, before falling to the ground? During that time, seeds form under the scales of the pine cones.   The scales have two important functions to protect the seeds from bad weather and to protect the seeds from foraging, hungry animals. Eventually, the seeds are released so that they can grow into new trees. To have the best chance of finding fertile soil and growing successfully, the pine cone scales stay tightly closed (see featured image) when the weather is cold and wet as these conditions are not suitable for germination and growth of a young seedling.   Read more...

It is a truism to say that trees provide wood or timber.  Timber (or lumber in the States) is wood that has been processed into planks or beams, part of the process of wood production. Timber may be supplied either rough-sawn, or surfaced on one or more of its faces. It is available from many species, usually hardwoods; but it is also available in softwoods, such as white pine and red pine, because of their low cost. Finished timber is supplied in various standard sizes, mostly for the construction industry—primarily softwood, from coniferous species, including pine, fir and spruce, cedar, and hemlock, whereas hardwoods are for high-grade flooring and furniture. Read more...