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Haberstroh, S.

Publications and source records attributed to Haberstroh, S..

8 recordsLinked to original sources

13CO2 pulse labelling reveals species-specific alterations in carbon allocation and volatile organic compound emissions under heat stress

Temperate forests increasingly face extreme air temperature, but plant physiological responses, particularly alterations in carbon allocation or protection via volatile organic compound (VOC) emissions, remain poorly understood. We pulse-labelled well-watered saplings of Fagus sylvatica and Pseudotsuga menziesii in a controlled heat stress experiment with 13CO2 to quantify heat-induced shifts in CO2, VOC and C pool exchange, specifically analyzing compound-specific {delta}13C of terpenoids, water-soluble organic matter (WSOM) and dark respiration. Under heat stress, up to 50% of fresh assimilates were directed to maintenance respiration and 1-2% to VOC emissions, while net assimilation and water use efficiency decreased by 50-75% in both species. Heat directly affected metabolic processes and reduced turnover rates of fresh assimilates in F. sylvatica, but accelerated them in P. menziesii. Strong 13C labelling of some compounds, particularly acyclic ones, suggested increased de novo synthesis of specific terpenoids for heat stress protection. By tracing the fate of recently assimilated 13CO2 we demonstrate that heat stress reduces net carbon uptake and water use efficiency, disrupts turnover of C pools and increases carbon loss via respiration and de novo synthesis of specific VOCs, potentially diminishing net carbon uptake of forests under future heat extremes.

plant biology↗

Early warning indicators for heat-induced mortality in temperate tree saplings

{middle dot} Globally, forest ecosystems face widespread mortality events. However, the independent impacts of distinct stressors, such as heat stress vs edaphic drought, remain poorly understood and physiological early warning indicators for tree mortality are urgently required. {middle dot} We exposed well-watered saplings of Fagus sylvatica, Pseudotsuga menziesii and Picea abies to summer heat waves and subsequent natural winter-desiccation. Physiological parameters (e.g. gas exchange, water uptake velocity via 2H labelling, and volatile organic compound emissions) were monitored throughout the growing season and survival was assessed regularly until subsequent spring to capture immediate and delayed mortality as a consequence of legacy effects. {middle dot} Heat exposure without soil water deficit, followed by winter desiccation, triggered species-specific mortality rates (51.8% F. sylvatica, 48.2% P. abies, 16.9% P. menziesii), with P. abies exhibiting significantly faster mortality response than the other species. Reduced water uptake, lower stomatal conductance, impaired photosynthetic efficiency, and altered VOC emissions distinguished non-surviving from surviving saplings months before visible damage in all three species. {middle dot} Heat stress drives mortality independent of edaphic drought, with sub-lethal physiological indicators detectable up to 10 months before visual signs. These early warning indicators could enable damage detection before lethal thresholds are crossed, offering new strategies for mitigating climate change-driven forest decline.

ecology↗

Synergistic effect of heat and drought on leaf VOC emissions and root exudates in Norway spruce saplings

Compound droughts, i.e. the co-occurrences of heat and drought, represent a serious challenge for temperate forest trees leading to significant losses in forest biomass. We studied the physiological response of Norway spruce (Picea abies) saplings to heat and drought individually, and in combination. Continuous measurements of leaf gas exchange and VOC emission allowed us to identify fast-response reactions, while discrete VOC and root exudate samplings added qualitative information on compositional changes. Additionally, we used 13CO2 and 2H2O label pulses to investigate C-allocation and root water uptake in response to stress. Heat as well as drought reduced assimilation rates in the saplings, whereas transpiration, leaf VOC emission and root exudation rates increased in response to heat. Drought alone increased VOC emission but decreased exudation rates. Combined heat and drought triggered an amplified response in both processes despite negative net CO2 assimilation rates. Label incorporation showed compromised water uptake capacity of drought-stressed plants and illustrated de novo C-allocation to VOC emission and root exudates. The results point at the high susceptibility of Norway spruce saplings to drought and heat. Combined stress resulted in synergistic responses in VOC emissions and root exudates, showing the detrimental effect of compound droughts on Norway spruce. HighlightIn this study, we found synergistic effects of heat and drought on carbon losses from leaf VOC emission and root exudates despite negative assimilation rates in Norway spruce saplings.

plant biology↗

Seasonal dynamics and sun/shade heterogeneity of leaf gas exchange and VOC emissions inside a tall temperate forest canopy

Leaf gas exchange is the key driver of forest carbon uptake and directly determines forest carbon sink activity. Additionally, plants release a variety of biogenic volatile organic compounds (VOCs) acting as stress signals of trees. However, continuous hourly resolved measurements of leaf gas exchange and VOC emissions in tall tree canopies are challenging and remain scarce. To this end, we developed a sophisticated in-situ leaf gas exchange measurement system with 24 cuvettes deployed on mature Fagus sylvatica (n=3) and Pseudotsuga menziesii (n=3) individuals in a mixed temperate forest. We additionally measured sap flux density (Js), radial growth and tree water deficit (TWD) to gain a holistic picture of seasonal leaf and stem water and carbon flux dynamics during the summer of 2024. During midsummer, we found a gradual reduction of stomatal conductance (gs) and VOC emissions of sun, but not shade branchlets of P. menziesii in response to moderate atmospheric and edaphic drying. Decreased gs led to a downregulation of transpiration (E), Js, and carbon isotope discrimination accompanied by an increase in TWD and intrinsic water used efficiency. Leaf gas exchange of shade branchlets remained unaffected due to microclimatic buffering effects. Contrarily, sun leaves of F. sylvatica, profited from sunny midsummer conditions and increased leaf gas exchange, whereas shade leaves benefitted from more diffuse light during early summer exhibiting similar carbon assimilation, transpiration and VOC emissions as sun leaves. For both species we found a clear time lag of four to five hours between maximum leaf and stem water fluxes and a delay of up to 20 hours for the recovery of TWD, highlighting the role of stem water reserves. Pronounced seasonal and diurnal differences of leaf gas exchange, stem water fluxes and VOC emissions showed, that continuous data are essential to better understand variability of ecosystem flux dynamics.

plant biology↗

Continuous chlorophyll fluorescence measurements trace sudden cold spell effects on photosynthetic efficiency in a temperate mixed forest

Air temperature extremes and fluctuations are expected to become more frequent and have been shown to affect the physiological functioning of temperate forests across Europe. The exposure to sudden cold spells during summer combined with high light intensities can lead to photoinhibition of photosystem II (PSII) and thereby reduce photosynthetic efficiency. In this study, we aimed to analyse the dynamics of photoinhibition as well as related protection mechanisms of tall tree canopies during such cold spells. Therefore, we continuously assessed leaf level chlorophyll fluorescence (ChlF) and ecosystem carbon fluxes by eddy covariance in a temperate mixed forest in southern Germany during growing season 2024. While the deciduous, broadleaved F. sylvatica indicated chronic photoinhibition as a response to sudden cold spells, the evergreen, coniferous P. menziesii showed higher tolerance to low air temperatures. Both species increased thermal energy dissipation at PSII during cold spells indicating the activation of protective mechanisms. Likewise, both species exhibited mainly the sustained form of non-photochemical quenching (NPQs) as a reaction to chilling temperatures and high light intensities which maintained elevated during the recovery phases. However, the dynamics of upregulation of photoprotection and recovery processes differed between the two tree species. Furthermore, the integration of ecosystem carbon exchange and continuous leaf level ChlF measurements gave valuable insights into the photosynthetic dynamics of the mixed forest canopy. This study emphasises the importance of the assessment of dynamic responses to future climate impacts on forest ecosystem on different scales.

ecology↗

Eavesdropping roots: Fagus sylvatica detects belowground stress signals from conspecific and heterospecific (Picea abies) neighbors, triggering increased shoot VOC emissions

O_LIVolatile organic compounds (VOCs) facilitate aboveground plant communication, but belowground signaling remains less understood. C_LIO_LIThis study explored root-root interactions between Picea abies and Fagus sylvatica saplings in monospecific (Fagus-Fagus) and heterospecific (Picea-Fagus) pairs (n=6), excluding shoot-level VOC communication. Sender plants were treated with jasmonic acid to simulate herbivory and labeled with 13CO2 and 15NH4NO3 to trace nutrient transfer in a split-root design. VOC emissions and gas exchange were measured over ten days using PTR-TOF-MS and 13CO2-spectroscopy and 13C and 15N were analyzed in roots and shoots via EA-IRMS. C_LIO_LIOur findings reveal, that (i) JA treatment induced strong de novo terpenoid emissions from P. abies and enhanced emissions of oxygenated VOCs and benzenoids from F. sylvatica, (ii) F. sylvatica receiver plants responded similarly to JA-treated neighbors, indicating belowground signaling, and (iii) responses of receiver plants were more pronounced in the heterospecific treatment. Furthermore, formic acid emissions from soils increased following JA treatment, suggesting altered soil microbial activity. Isotopic analysis revealed C exudation into the rhizosphere and N transfer to receiver plants. C_LIO_LIThese results suggest that belowground signaling enables early priming of herbivore-induced defenses in neighboring plants, and that the response intensity is modulated by species identity. C_LI

plant biology↗

Water stable isotopes reveal the ecohydrological importance of stemflow for mature and juvenile European beech

O_LIStemflow of forest trees can contribute a significant fraction of water to forests water fluxes; however, it is still unclear if and to what extent trees use stemflow for water supply and how much stemflow is lost by percolating below the root zone. C_LIO_LIWe applied deuterium-enriched stemflow equivalent to a throughfall depth of 23 mm to adult Fagus sylvatica trees to trace stemflow through the soil and trees. We continuously measured in-situ water stable isotope compositions in soil and xylem water and destructively sampled xylem water in the crowns of adult labelled (n=18), unlabelled F. sylvatica (n=15) and unlabeled Picea abies (n=9), complemented by destructive xylem water sampling of neighboring juvenile F. sylvatica (n=45). C_LIO_LIStemflow water supported 3.9 - 14.0% of daily sap flux of adult labelled F. sylvatica trees. In the soil, deuterium-enriched stemflow was detectable at a max. of 0 - 0.40 m to the labelled tree. However, unlabeled juvenile trees within a distance of [~]2 m showed label water uptake, indicating rooting into soil compartments affected by stemflow label. C_LIO_LIWe demonstrate the importance of stemflow as a water source for both adult and neighboring juvenile F. sylvatica, strongly profiting from stemflow infiltration. C_LI

plant biology↗

Spatio-temporal plasticity of root exudation in three temperate tree species: effects of season, site and soil characteristics

Root exudation provides a constant carbon input to the rhizosphere and is therefore a very important factor in shaping this hotspot of biological activity. Nonetheless, root exudation data and its spatio-temporal plasticity is scarce. This study provides insights into compound-specific root exudation in three temperate tree species in two seasons (late spring and late summer) and two soil compartments (forest floor and the top mineral soil), including the effect of soil chemistry. At four sites with differing mean annual temperature and soil phosphorus level, root exudates were sampled using an in-situ cuvette-based system and analysed by gas chromatography-mass spectrometry. We found seasonally and spatially varying site- and species-specific exudation patterns. While the seasonal pattern was similar among species and sites, with higher exudation rates in late spring, soil compartment-specific exudation depended on species and site. Acer pseudoplatanus tended to exude more into the mineral soil at warmer sites, while Picea abies exuded more in the mineral soil at all sites. Exudation by Fagus sylvatica was independent from the soil compartment. Significant correlation between exchangeable soil cations and specific compounds exuded by F. sylvatica and P. abies were found. Exudation of specific compounds in F. sylvatica increased with the concentration of exchangeable Mg, Al and Fe, whereas exudation rates in P. abies decreased with most base cations concentration, while sugar exudation increased with the exchangeable non-base cations Al and Fe. These results demonstrate that root exudation is dynamically adjusted to the species-specific nutritional needs governed by site, season and soil characteristics.

plant biology↗