Dendrochronology and dendrochemistry

A look inside the city trees

In Germany, about one third of the population lives in cities. In view of increasing sealing, urban heat islands and high emission loads, cities are particularly affected by heat stress in climate change. Therefore, adaptation measures are needed to sustainably improve the inner-city microclimate, air quality and living conditions of the urban population. Urban green spaces and, in particular, urban trees make an important contribution to counteracting the effects of climate change. They reduce urban heat in summer, provide shade and keep our air clean.

Sampling of a plane tree in Rheinstetten.
Sampling of a plane tree in Rheinstetten.

In order to be able to maintain these services of our urban trees in the future, some crucial questions arise: which tree species react particularly sensitively to the consequences of air pollution and climate change, such as heat and drought? Which tree species are particularly resilient and thus suitable for mitigating the effects of climate change in cities in the future? A look inside urban trees helps to clarify these questions. By taking cores, dendrochronological and isotope-based approaches were carried out in this subproject. This allowed conclusions to be drawn about the suitability of different tree species in urban environments. Dendrochronology, i.e. tree-ring research, was used to determine the resistance, recovery ability and resilience of selected tree species from Karlsruhe, allowing conclusions to be drawn about the tree species' tolerance to drought, among other things. The influence of heat stress and drought on tree physiology was also determined by isotope analysis. In addition, isotope analysis provided evidence of air pollution in Karlsruhe.

  

What and the annual rings of urban trees reveal

Example of a tree core sample.
Example of a tree core sample.

For the investigations, cores were first taken manually using a special drill. The cores are about the thickness of a pencil and provide a cross-section of the tree up to the center of the tree. This allows the annual rings to be seen, but the tree itself may continue to live. In addition to the age of the tree (number of annual rings), the width of the rings provides information about annual tree growth. The wider the ring, the more favorable the environmental conditions were, and vice versa. Extreme weather events, such as drought and heat, as well as environmental stresses, such as exhaust gases or fine dust, can cause disturbances in growth and can be additionally analyzed with the help of weather and climate records. For example, it is possible to find out how well an individual tree has recovered from a drought year (2003, 2008, 2011, 2015), i.e. how resilient it is and how this ability differs among different tree species. Year by year, a tree also archives a kind of isotopic fingerprint in its annual rings. This stores, for example, the ratio of stable isotopes. The isotope ratio depends on environmental conditions, so that conclusions can be drawn about environmental influences at the time. 

The five tree species investigated

Within the scope of the subproject, about 30 trees each of the most common tree species in Karlsruhe and Rheinstetten - Norway maple, littleleaf linden, English oak, hornbeam and Plane tree - were examined. The drought response of the five tree species was investigated for the years 2003, 2011, and 2015, during which pronounced dry periods occurred during the growing season. A tree ring chronology was created for each of the sample trees, mapping the variation in stem thickness growth based on the measured tree ring widths. To determine how stem thickness growth responded to drought, the indices resistance and resilience were calculated. Resistance indicates how much the growth slump is compared to the previous year. Resilience is a measure of the extent to which a tree is able to return to previous growth levels after a dry period. In addition to tree ring width, isotopic signatures of carbon and oxygen in wood were analyzed, which can be used as indicators of a tree's water availability and physiological drought stress. Both tree ring width and carbon and oxygen isotopes were examined for their relationship with weathering. 

The importance of precipitation in spring

Tree-ring chronologies of Norway maple (Acer platanoides), maple-leaved sycamore (Platanus × hispanica), English oak (Quercus robur), littleleaf linden (Tilia cordata), and hornbeam (Carpinus betulus) during 2000-2018.
Tree-ring chronologies of Norway maple (Acer platanoides), maple-leaved sycamore (Platanus × hispanica), English oak (Quercus robur), littleleaf linden (Tilia cordata), and hornbeam (Carpinus betulus) during 2000-2018.

The studies of the tree interior revealed that water availability in the spring, in particular, has a decisive influence on stem thickness growth and the response of urban trees to drought. Higher precipitation has been shown to be associated with higher stem thickness growth. In particular, precipitation in May - for Norway maple, hornbeam, English oak, and littleleaf linden - proved to be the most important influencing factor. The dependence of stem thickness growth on sufficient water availability in spring, is also reflected in the low resistance of all tree species (except sycamore) in the drought year 2011 compared to the drought year 2003, because in 2011 the most severe drought occurred in spring and in 2003 only later in summer. The drought years (2003, 2011 and 2015) are marked in light red in the figure. 

Proven in drought conditions: Maple-leaved plane tree and English oak

Based on our results, sycamore and pedunculate oak in particular prove to be suitable for urban areas with regularly occurring dry periods. This became particularly clear in 2011, when spring precipitation was very low. Except for maple-leaved sycamore, no tree species showed sufficient resistance to drought and heat. In 2015, English oak and maple-leaved sycamore proved to be the most resistant tree species to persistent drought.

 

In addition, analysis of carbon and oxygen isotopic signatures showed physiological adaptation to drought in Norway maple and sycamore in 2003 and 2015, and in 2011 Norway maple and littleleaf linden were found to have increased water use efficiency as an adaptation to drought. Sycamore and English oak did not show increased values in the same year, so comparatively low drought stress can be assumed here.

 

Site characteristics, on the other hand, showed only a minor effect on the resistance and resilience of the tree species studied. Thus, an influence of the distance to roads as well as the level of traffic emissions could not be confirmed. A slight influence of soil properties was only found with respect to soil type and organic carbon content. Fast growing trees also showed a lower recovery of growth after drought than slow growing trees.

Traffic emissions are reflected in the wood

Immission pre-pollution (NO2) in the study area.
Immission pre-pollution (NO2) in the study area.

Nitrogen isotope analysis proved to be a useful method to determine the exposure of trees to traffic emissions. In our studies, tree species was shown to be the most important factor in explaining the variability of the isotopic composition of nitrogen. The distance to the nearest road and the intensity of traffic emissions also had a significant influence. The estimated values for the ratio of stable nitrogen isotopes were higher the closer the tree was to a road and the higher the nitrogen oxide emissions at that location. This result confirms that exposure to traffic emissions is reflected in the isotopic composition of nitrogen in the wood of urban trees.

Now what?

The investigations clearly show that the five tree species studied, which together make up more than one third of the tree population in the study area, differ in terms of stem thickness growth, in some cases strongly, in their tolerance to drought. Based on our surveys, maple-leaved sycamore and pedunculate oak prove to be particularly suitable for urban areas with regularly occurring dry periods. With the exception of sycamore, it is clear across all tree species that spring water availability, in particular, plays a critical role in stem thickness growth and drought response. These findings are important for translating the results into specific irrigation strategies. Thus, for sycamore and English oak, where resistance and resilience are generally higher, irrigation does not seem to be absolutely necessary, or for English oak only in case of drought in spring, to which it reacts particularly sensitively. This is also true for the tree species European linden, hornbeam and Norway maple, so that irrigation would probably have a positive effect on stem thickness growth in the absence of precipitation in spring/early summer. Based on these results, a tool will be developed in the follow-up project GrüneLunge 2.0 to help municipalities select appropriate tree species. More information on our planned activities in the GrüneLunge 2.0 project can be found here: Urban tree suitability in climate change.

Photos: Friederike Stoll/FVA