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  • 1
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    PANGAEA
    In:  Supplement to: Spiegel, Johanna K; Aemisegger, F; Scholl, M; Wienhold, F G; Collett, Tim S; Lee, T; van Pinxteren, Dominik; Mertes, Stephan; Tilgner, A; Herrmann, H; Werner, R A; Buchmann, N; Eugster, Werner (2012): Temporal evolution of stable water isotopologues in cloud droplets in a hill cap cloud in central Europe (HCCT-2010). Atmospheric Chemistry and Physics, 12(23), 11679-11694, https://doi.org/10.5194/acp-12-11679-2012
    Publication Date: 2024-01-27
    Description: Cloud samples for the isotopic analysis were collected in the framework of the Hill Cap Cloud Thuringia 2010 (HCCT-2010) campaign on Schmücke (50° 39'N/ 10° 46'E, 937 m a.s.l.; Germany) in September and October 2010 with a three-stage Caltech Active Strand Cloudwater Collector (CASCC) during 13 different cloud events with a temporal resolution of 1 to 3 hours. In a first step, we ensured that no additional fractionation occurred during sampling with the CASCC. The d values of the three sizes classes of the CASCC (4 µm to 16 µm, 16 µm to 22 µm and 〉22 µm) did not differ significantly, revealing that the cloud droplets of different sizes quickly equilibrate their delta value with the one of the surrounding vapor. delta values in the cloud droplets varied from -77 per mil to -15 per mil in d2H and from -12.1 per mil to -3.9 per mil in d18O and were fitted by d2H =7.8*d18O +13*10**-3. delta values decreased with temperature as well as towards the end of the campaign, representing a seasonal trend which is known from d values in precipitation. The deuterium excess of the cloud samples was generally higher than the Local Meteoric Water Line of the closest GNIP (Global Network of Isotopes in Precipitation) station. Rain decreases its deuterium excess during falling through an unsaturated air column, while the cloud droplets conserve the deuterium excess of the initial evaporation and thus have been found to be a good indicator for the airmass source region: higher deuterium excess was measured for polar air masses and lower deuterium excess for Mediterranean air masses. Changes in d values during one cloud event were up to 3.6 per mil (d2H) and 0.23 per mil (d18O), except for frontal passages, which were associated with increases of ~6 per mil per hour (d2H) and ~0.6 per mil per hour (d18O). Using a box model, we showed that the influence of condensation only was able to explain the variation in the isotope signal of two cloud passages. Consequently, we deduced that the water vapor "feeding" the cloud advected the measured changes. A trajectory analysis and moisture source diagnostic revealed that it is very likely that the variations were either related to rain out along the trajectories or to meteorological changes in the moisture source region. This was the first study using stable water isotopologues in cloud water manifesting their potential in the context of atmospheric water vapor circulation.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 2
    Publication Date: 2024-01-27
    Keywords: Calculated average/mean values; DATE/TIME; repeated IRMS measurements; Replicates; Sample ID; δ18O, standard deviation; δ18O, water; δ Deuterium, standard deviation; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
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  • 3
    Publication Date: 2024-01-27
    Keywords: Calculated average/mean values; Caltech Active Strand Cloudwater Collector; CASCC; DATE/TIME; Duration; HCCT-2010; Hill Cap Cloud Thuringia 2010; Mass; repeated IRMS measurements; Replicates; Sample ID; Sampling clouds; schmücke; Schmücke, Thuringia Forest, Germany; δ18O, standard deviation; δ18O, water; δ Deuterium, standard deviation; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 911 data points
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  • 4
    Publication Date: 2024-01-27
    Keywords: Calculated average/mean values; DATE/TIME; repeated IRMS measurements; Replicates; Sample ID; δ18O, standard deviation; δ18O, water; δ Deuterium, standard deviation; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 5
    ISSN: 1432-1939
    Keywords: Populus tremuloides ; Carbon/nutrient balance ; Choristoneura conflictana ; Plant/herbivore interaction ; Secondary metabolite
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary We investigated the effects of nitrogen fertilization upon the concentrations of nitrogen, condensed tannin and phenolic glycosides of young quaking aspen (Populus tremuloides) leaves and the quality of these leaves as food for larvae of the large aspen tortrix (Choristoneura conflictana), a Lepidopteran that periodically defoliates quaking aspen growing in North America. Nitrogen fertilization resulted in decreased concentrations of condensed tannin and phenolic glycosides in aspen leaves and an increase in their nitrogen concentration and value as food for the large aspen tortrix. These results indicate that plant carbon/nutrient balance influences the quality of aspen leaves as food for the large aspen tortrix in two ways, by increasing the concentrations of positive factors (e.g. nitrogen) and decreasing the concentrations of negative factors (eg. carbon-based secondary metabolites) in leaves. Addition of purified aspen leaf condensed tannin and a methanol extract of young aspen leaves that contained condensed tannin and phenolic glycosides to artificial diets at high and low levels of dietary nitrogen supported this hypothesis. Increasing dietary nitrogen increased larval growth whereas increasing the concentrations of condensed tannin and phenolic glycosides decreased growth. Additionally, the methanol extract prevented pupation. These results indicate that future studies of woody plant/insect defoliator interactions must consider plant carbon/nutrient balance as a potentially important control over the nutritional value of foliage for insect herbivores.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1573-1561
    Keywords: Large aspen tortrix ; oak leaf shredder ; Choristoneura conflictana ; Choristoneura fumiferana ; Choristoneura fractivittana ; Croesia semipurpurana ; Cenopis acerivorana ; cis-11-tetradecenal ; attractant ; field tests ; trans-11-tetradecenal
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology
    Notes: Abstract Blends containingcis-11-tetradecenal with the trans isomer orcis-11-tetradecen-1-ol were field tested against the tortricine speciesChoristoneura conflictana andCroesia semipurpurana. The results indicate thatcis-11-tetradecenal alone is a very potent attractant for maleC. conflictana whereas maleCroesia semipurpurana were strongly attracted to blends oftrans/cis-11-tetradecenal in the range 80∶20–90∶ 10.Cenopis acerivorana andChoristoneura fumiferana were also caught with mixtures of 11-tetradecenal isomers whileChoristoneura fractivittana was very strongly attracted to the mixture ofcis-11-tetradecen-1-ol/cis-11-tetradecenal in the ratio 95/5.
    Type of Medium: Electronic Resource
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  • 7
    Publication Date: 2015-06-25
    Description: The response of carbon allocation to drought has often been studied in terms of short-term transport velocity of recently fixed carbon from leaves to roots and root respiration. However, its dynamic response to other environmental conditions, e.g., to changes in temperature, is less clear. Here, we investigated the effects of drought, increased temperatures and their combination on transport velocity as well as on distribution of recent photoassimilates for different compounds, such as sugars, starch, organic acids and amino acids. We used a 13 CO 2 pulse-labelling approach and studied the recovery of 13 C in different plant tissues and compounds of beech saplings ( Fagus sylvatica L.) during a 9-day chase period. Neither total dry biomass nor dry weights of leaves or roots were affected by drought or increased temperatures. Generally, the fast transfer of recently fixed assimilates from leaves to roots took about 1 day, while 13 C enrichment in soil CO 2 efflux peaked only 2 days after labelling. Increased temperatures prolonged mean transfer times of recent photoassimilates from the leaves to the roots, probably caused by enhanced intermediate storage alongside basipetal transfer, clearly impacting short-term carbon allocation. This temperature effect was seen in the delayed peak in 13 C excess of root sugars, decoupling the roots from the leaves in the short term. On average, ~40% of the 13 C label initially present in the plant was recovered in the roots (over all treatment combinations), providing strong evidence for preferred carbon allocation into the roots at the end of the growing season. Root starch was the principal compound for long-term storage of carbon, whereas leaf (transitory) starch was remobilized again after some days, exhibiting the longest mean residence times under dry and warm conditions. These observation clearly point to different functionalities of the same compound (i.e., starch) in different plant tissues and the crucial role of roots for long-term carbon storage.
    Print ISSN: 0829-318X
    Electronic ISSN: 1758-4469
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 8
    Publication Date: 2015-11-21
    Description: Significant gaps still exist in our knowledge about post-photosynthetic leaf level and downstream metabolic processes and isotopic fractionations. This includes their impact on the isotopic climate signal stored in the carbon isotope composition ( 13 C) of leaf assimilates and tree rings. For the first time, we compared the seasonal 13 C variability of leaf sucrose with intra-annual, high-resolution 13 C signature of tree rings from larch ( Larix gmelinii Rupr.). The trees were growing at two sites in the continuous permafrost zone of Siberia with different growth conditions. Our results indicate very similar low-frequency intra-seasonal trends of the sucrose and tree ring 13 C records with little or no indication for the use of ‘old’ photosynthates formed during the previous year(s). The comparison of leaf sucrose 13 C values with that in other leaf sugars and in tree rings elucidates the cause for the reported 13 C-enrichment of sink organs compared with leaves. We observed that while the average 13 C of all needle sugars was 1.2 more negative than 13 C value of wood, the 13 C value of the transport sugar sucrose was on an average 1.0 more positive than that of wood. Our study shows a high potential of the combined use of compound-specific isotope analysis of sugars (leaf and phloem) with intra-annual tree ring 13 C measurements for deepening our understanding about the mechanisms controlling the isotope variability in tree rings under different environmental conditions.
    Print ISSN: 0829-318X
    Electronic ISSN: 1758-4469
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 9
    Publication Date: 2014-09-04
    Description: The mechanistic understanding of isotope fractionation processes is increasing but we still lack detailed knowledge of the processes that determine the isotopic composition of the tree-ring archive over the long term. Especially with regard to the path from leaf photosynthate production to wood formation, post-assimilation fractionations/processes might cause at least a partial decoupling between the leaf isotope signals that record processes such as stomatal conductance, transpiration and photosynthesis, and the wood or cellulose signals that are stored in the paleophysiological record. In this review, we start from the rather well understood processes at the leaf level such as photosynthetic carbon isotope fractionation, leaf water evaporative isotope enrichment and the issue of the isotopic composition of inorganic sources (CO 2 and H 2 O), though we focus on the less explored ‘downstream’ processes related to metabolism and transport. We further summarize the roles of cellulose and lignin as important chemical constituents of wood, and the processes that determine the transfer of photosynthate (sucrose) and associated isotopic signals to wood production. We cover the broad topics of post-carboxylation carbon isotope fractionation and of the exchange of organic oxygen with water within the tree. In two case studies, we assess the transfer of carbon and oxygen isotopic signals from leaves to tree rings. Finally we address the issue of different temporal scales and link isotope fractionation at the shorter time scale for processes in the leaf to the isotopic ratio as recorded across longer time scales of the tree-ring archive.
    Print ISSN: 0829-318X
    Electronic ISSN: 1758-4469
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 10
    Publication Date: 2019-01-18
    Print ISSN: 0029-8549
    Electronic ISSN: 1432-1939
    Topics: Biology
    Published by Springer
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