Trees and shrubs that grow in temperate regions, where the seasons alternate (warm / cold, dry /wet) create annual rings.  The rings formed in a deciduous tree (like beech, oak, lime) are generally quite noticeable when the tree is felled.  They may be counted to give an indication of the age of the tree.  Annual rings are formed because there is a difference in the creation of ‘wood’ / xylem tissue when growth is fast in the Spring and slow as Autumn progresses.  The thickness of the rings from year to year reflects the changing climate and environment that the tree experiences during its life. Xylem tissue is one component of a tree’s vascular tissue.  The xylem tissue conducts water and minerals around the plant, whereas phloem tissue transports sugars and other organic molecules.  Lying between these two tissues is the cambium.  This is a layer of dividing cells, which becomes active in the Spring forming new cells some of which will form new phloem tissue and others develop into xylem tissue. The cells that will form the xylem tissue undergo a series of dramatic changes.   The walls of the cells that will form the long tubes of the xylem are made of cellulose to begin with, but then they are strengthened with lignin.  Lignin is the ‘stuff of wood’.  It is a complex material - made from polyphenols and other substances such as pectins and hemicelluloses.  It is a waterproofing material that is highly resistance to decay.  It lines the tubes of the xylem so that water can be transported from the roots, up the trunk / stem to the leaves etc.  The xylem vessels that form in the Spring [early wood] have a greater diameter than those formed later in the year [late wood].  It is this size difference in the vessels that results in the visible ‘rings’ when a tree is felled. Careful study of tree rings can reveal information about climate, sometimes extending back through the centuries   using species such as the long lived Bristlecones. It has given rise to the discipline of dendrochronology [link opens / downloads a PDF].  This information can then be ‘combined’ with tree ring data from intact remains in cold, dry (and often high altitude) environments and material from archaeological sites.   Apart from measuring the ‘width’ of the annual rings by creating thin section of the wood that can be examined under microscope, it is also possible to use staining techniques to reveal which xylem tissue has a higher / lower, lignin / cellulose content.  By using a double staining technique with the dyes Safranin and Astra Blue, it is possible to identify which xylem vessels are rich in lignin, and which have more cellulose.  Tree rings which stain largely blue are formed from cells which have not lignified properly.  Lignin stains red.  A recent study of blue rings in Pine trees and Juniper shrubs suggests that blue rings are indicators of cold summers. These two species are typical of the upper tree line in Northern Norway. Furthermore, blue rings have the potential to weaken the pine trees, leaving them more susceptible to mechanical damage and / or disease.  This study has identified blue rings associated with the cold summers of 1877 and 1902, which might have been caused by the eruptions of volcanoes as far away as Ecuador and Martinique. Note : The xylem tissue in conifers is different to that of broad leaved deciduous trees.  It is made up of shorter structures called tracheids, which pass water from one to the next via pits - ‘pores’ in their lignified walls. For more information on Blue rings in Black Pine, click here  

To see the forests of  The Fens,  you would need to be a time traveller, as they were ‘lost’ some four thousand years ago.  Today, The Fens are a low lying agricultural region that forms part of Norfolk, Lincolnshire and Cambridgeshire.    The Fens contain some of the best agricultural land in the U.K., growing potatoes, sugar beet, and wheat.  A naturally marshy area, it was drained centuries ago and is now maintained through a complex system of drainage canals, dykes and pumping stations.  As a result of the drainage, the level of the land in many places has shrunk.  Indeed, in places, the land level is below sea level.  There are occasional ‘hills’ or islands, which have remained dry even when the surrounding area has been flooded.  The city of Ely and its cathedral was built on such a clay island. Deeper ploughing (e.g. for potatoes) in this area has over the years exposed  ’bog oaks’, large logs between two and eight metres in length.  The trunks were sometimes piled up in so-called clearance  cairns on the edges of a field, or allowed to dry out and later used for fuel.  Recently, ‘oaks’ from a number of farms across the region have been examined by researchers at Cambridge University and many have been identified as the remains of ancient yew trees.  The various logs were often well preserved in the peaty soils of the area, and this allowed detailed analysis of the annual rings (dendrochronology). The rings showed that some of the Yews were 400 years old, when they died.  Tree ring analysis plus examination of the pollen grains* (found in the peat), suggests that the area had dense yew (and oak) woodlands some 4500 years ago.  However, these woods were lost about 4200 years before today, probably due to an abrupt rise in sea level.   The trees would have been unable to tolerate the salt water (nor salt spray) when the area around The Wash was inundated.  Quite what was responsible for the rise in sea level is not clear, though other significant climatic events in different parts of the world have been recorded at this time. the 'wall' of pollen grains  [the exine] is made from a chemical [sporopollenin] that is extremely resistant to decay / degradation, so the grains  retain their shape / markings for thousands of years;  this means that plant species can be identified [palynology].  

Earlier flowering times. A survey has shown that plants are flowering earlier in the year.  Cambridge University researchers compared the dates of flowering of some four hundred plus species before and after 1986. They found that plants are now flowering roughly one month earlier.  More recent decades have been associated with rising air temperatures. This change in flowering time may have profound consequences for the plants.  The vast majority of plants are dependent on pollinating insects (bees, bumblebees, hoverflies) to set seed and complete their life cycles.  By flowering early their cycle, plants may not match up  with the activities of their pollinators. They may flower but their pollinators bee ‘missing’. Their pollinators need to emerge from their overwintering stage earlier. Earlier flowering may not matter for those plants that are visited by several pollinators but for those that are dependent on one or two specific visitors - it may critical.  For example, Sainfoin.  Sainfoin is host to a particular (solitary) bee Melitta dimidiata (remote image here).   It is a monolectic bee; i.e., a bee that collects food (nectar and pollen) from only one species of flower - the sainfoin.  If the sainfoin flowers earlier in the year and the bee does not match the shift in flowering, then the bee has a problem. Work on the effects of climate change on pollinators has been somewhat limited to date, but studies in Japan suggest that bees / bumblebees are somewhat behind plants in their response to environmental changes. Bee and bumblebee news. Recent research data provide evidence that (buff tailed) bumblebees are not able to detect or avoid concentrations of pesticides [imidacloprid, thiamethoxam, clothianidin, or sulfoxaflor], as used ‘on the farm’ - from signals sent by their mouthparts. The mouthparts are covered with tiny hairs and these hairs have ‘pores’ in them. Chemicals pass through these ‘pores’ to sensory cells; this is how the bee tastes and smells. It seems likely that the bumblebees are at considerable risk of consuming pesticides in their search for nectar when visiting pesticide-treated crops. [caption id="attachment_19675" align="alignleft" width="300"] Bumbles foraging in artichoke[/caption] Another agrochemical,  Roundup,  has been found to affect the learning and memory of bumblebees. Roundup, which contains glyphosate, affects their ability to learn and memorise connections between colour and taste.  Impaired colour vision is likely to affect the foraging and nesting success of the bees.  The research was conducted in Finland by researchers at the University of Turku. In yet another concerning study, researchers at the University of Maryland have found that the life span of laboratory-raised honey bees has reduced considerably.    Five decades ago, the lifespan for a worker honeybee (Apis mellifera) under controlled laboratory conditions was about 34 days. Now it is some 17/ 18 days - according the report in Nature.  The study also reviewed the scientific literature [from the 1970s to now] and noted a trend in the life span of bees.   Shortened worker bee lifespan has implications for colony health and survivorship.  The work at the University of Maryland is ongoing. Methane release. Ghost forests are found in coastal areas.  As a consequence of climate change, sea water has ‘invaded’ low laying areas and trees have died. The dead trees are sometimes referred to as ‘snags.  A  number of woodland / forest communities along the eastern coast of the United States have been affected.  Recent work by North Carolina State University has shown that these ghost forests release methane.  The methane is generated by bacteria in the soil but then ‘escapes’ by means of the ‘snags’.  As it passes through the wood of the ‘snags’, microbes may consume and alter the methane.   As methane is a potent greenhouse gas, understanding the nature and extent of these methane emissions from ‘ghost forests’ is important. Tree rings The study of tree rings has been invaluable in dating many historic objects ./ archaeological sites.  Now, it seems that they could play a role in estimating the amount of carbon that trees are actually absorbing (carbon sequestration), if woodland / forest inventories are coupled with core samples of the trees. The measurement of the annual rings from such cores could create a record of ‘tree growth across space and time’, yielding a more accurate estimate of the amount of carbon being taken up by woodland and forests. Forests, soils and oceans are major ‘carbon sinks’.

Dendrochronology seeks to gather information from the annual rings of trees, dated to their year of formation.   As trees age, they form new distinctive rings, outward from the centre, and each year a circle of new, dead wood is formed (by the cambium) around the trunk of most trees. The annual rings form because the water conducting xylem vessels or early wood formed in late spring and early summer (when growth is rapid) are wider and lighter than those formed in late summer and early autumn, which are narrower and darker (sometimes called the late wood).  A light and dark ring together constitute one year’s growth.   In winter, there is no growth. Trees and their annual rings are essentially long term recording devices that ‘house’ information about climatic variations, past climates and ecosystems; they can even offer insights into historical events. From an annual ring, it is possible to extract information about precipitation, temperature and other climate data about that year. Read more...

Twelve thousand years ago (during the late glacial maximum) massive ice sheets and glaciers extended across much of the world. Then, the climate began to warm and about ten thousand years ago, our landscape started to look very different from today - not just because there were no roads, towns or cities but because the newly exposed land was being colonised by plants, trees, animals – and lastly by people.  The forests and woodlands that slowly developed in the post Ice Age period were different to the forests and woodlands that we see today. The land was colonised (at this time) by the plants and animals that lived on ‘the edge of the ice’. Read more...

Yew woodland (in Southern England) tends to develop on the thin soils that form over chalk, often on the sides of dry valleys . They can be found along the North Downs, and in West Sussex on parts of the South Downs. Yew woodlands can also be found in the Cotswolds and in the Wye Valley (on limestone). In Ireland, there is a significant Yew wood near Killarney, again growing on top of limestone. Yew woodland may develop from chalk grassland, when grazing by sheep or rabbits is removed. With no grazing, Juniper and / or Hawthorn start to grow.  Then, between these, shade-tolerant Yew seedlings begin to grow.   Eventually, the Yew will overtake the Juniper / Hawthorn, and shade them out. The dead remains of juniper and hawthorn sometimes may be seen on the floor of a Yew woodland. Read more...

With the recent spell of fine weather, some people may have wandered down memory lane and recalled “the summer of 76”.  Then, the temperature reached 80oF from June 22nd through to the 16th July, and for two weeks the temperatures in some areas exceeded 90oF. However, temperature was not the only environmental factor to stress plants – lack of rainfall or drought was also a major factor.  The previous autumn had been quite dry, as was the winter of  1975–76.   The drought became most severe during the summer months - with woodland, forest and heath fires breaking out.  Crop production was also severely affected, and there was water rationing (and stand pipes) in some areas. Ecologists* from the University of Stirling (Professor Alistair Jump) and the JNCC have recently investigated the (long term) effects of the 1976 drought on native woodland.   They examined the records of Lady Park Wood in the Wye Valley.  This 45 hectare Nature Reserve was ideal for a detailed study as there existed long term records  / surveys Read more...

Dendrochronology seeks to gather information on tree rings, dated to their year of formation, and to use this information to established the age of artefacts (like the timbers of a boat or remains of house) or determine the nature of the climate in times past. Annual rings form in temperate trees because the xylem vessels or early wood formed in late spring and early summer (when lots of growth occurs) are wider and lighter than those formed in late summer & early autumn, which are narrower and darker (sometimes called the late wood).  A light and dark ring together constitute one year’s growth.   In winter, there is no growth. The various branches of dendrochronology (dendroarchaeology, dendroclimatology) are based on the uniformitarian principle.  This says that the various factors that currently influence tree growth and hence tree ring development will have operated in the past.  Through knowledge of these factors (physical and biological) that have influenced current and recent tree ring growth, it is possible when looking at tree ring samples from old wood artefacts / timbers to ‘reconstruct’ the climate of the past. Read more...