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  • 1
    Keywords: Electronic books
    Description / Table of Contents: Intro -- Preface -- Acknowledgements -- Contents -- Contributors -- Part I Introduction -- 1 Isotope Dendrochronology: Historical Perspective -- 1.1 Introduction -- 1.2 Origins -- 1.3 Advances -- 1.3.1 20th Century Spin Up -- 1.3.2 21st Century Expansion -- 1.4 Emerging Directions -- 1.5 Conclusions -- References -- 2 Dendrochronology: Fundamentals and Innovations -- 2.1 The Annual Ring-The Keeper of Time in Dendrochronology -- 2.1.1 Inter-Annual Variations in Tree-Rings and Tree-Ring Parameters -- 2.2 Crossdating -- 2.3 Sampling and Site Selection -- 2.4 Deconstructing Variability in Tree-Ring Data -- 2.4.1 The Linear Aggregate Model -- 2.4.2 Detrending and Standardization -- 2.4.3 Long-Term Trends in Tree-Ring Data -- 2.5 Chronology Development, Confidence, Sample Replication, Coherence, and Variance -- 2.5.1 Tree-Ring Chronologies -- 2.5.2 Assessment of Chronology Confidence -- 2.5.3 Variance Changes in Composite Time-Series -- 2.6 Conclusions -- References -- 3 Anatomical, Developmental and Physiological Bases of Tree-Ring Formation in Relation to Environmental Factors -- 3.1 Introduction -- 3.2 Wood Structure and Functions -- 3.2.1 Xylem Anatomy -- 3.2.2 Xylem Cell Wall Structure and Composition -- 3.3 The Biological Basis of Wood Formation in Relation to Tree Development -- 3.3.1 The Successive Stages of Xylem Cell Differentiation -- 3.3.2 Heartwood Formation -- 3.3.3 Influence of Environmental Factors on Wood Formation Processes -- 3.4 Seasonal Dynamics of Wood Formation in Relation to Tree Phenology -- 3.4.1 The Phenology of Cambium and Xylem -- 3.4.2 The Phenology of Leaves, Roots and Reserves -- 3.4.3 Seasonal Dynamics of Wood Formation in Relation to Organ Phenology -- 3.4.4 Influence of Environment on Seasonal Dynamics of Wood Formation and Tree Phenology -- 3.5 Kinetics of Tracheid Differentiation in Relation with Tree Physiology.
    Type of Medium: Online Resource
    Pages: 1 online resource (775 pages)
    ISBN: 9783030926984
    Series Statement: Tree Physiology Ser. v.8
    RVK:
    Language: English
    Note: Description based on publisher supplied metadata and other sources
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  • 2
    Keywords: Plant physiology. ; Forestry. ; Environment. ; Paleontology .
    Description / Table of Contents: PART I INTRODUCTION: 1. Isotope Dendrochronology: Historical Perspective -- 2. Dendrochronology: Fundamentals and Innovations -- 3. Anatomical, developmental and physiological bases of tree-ring formation in relation to environmental factors -- PART II METHODS: 4. Sample collection and preparation for annual and intra-annual tree-ring isotope chronologies -- 5. Stable isotope signatures of wood, its constituents and methods of cellulose extraction -- 6. Tree-Ring Stable Isotope Measurements: The Role of Quality Assurance and Quality Control to Ensure High Quality Data -- 7. Newer Developments in Tree-Ring Stable Isotope Methods -- PART III: ISOTOPIC FRACTIONATIONS FROM SOURCE TO WOOD: 8. Isotopes – terminology, definitions and properties -- 9. Carbon isotope effects in relation to CO2 assimilation by tree canopies -- 10. Environmental, physiological and biochemical processes determining the oxygen isotope ratio of tree-ring cellulose -- 11. The stable hydrogen isotopic signature: From source water to tree rings -- 12. Nitrogen isotopes in tree rings – Challenges and prospects -- 13. Postphotosynthetic fractionation in leaves, phloem and stem -- PART IV PHYSIOLOGICAL INTERPRETATIONS: 14. Environmental fingerprints in tree-ring stable isotopes: Limits and strengths in mirroring environmental impacts -- 15. Post-photosynthetic carbon, oxygen and hydrogen isotope signal transfer to tree rings – how timing of cell formations and turnover of stored carbohydrates affect intra-annual isotope variations -- 16. Probing tree physiology using the dual-isotope approach -- 17. Intrinsic water-use efficiency derived from stable carbon isotopes of tree-rings -- PART V: ENVIRONMENTAL FACTORS IMPACTING THE ISOTOPIC FRACTIONATION: 18. Spatial and temporal variations in plant source water: O and H isotope ratiosfrom precipitation to xylem water -- 19. Climate signals in stable isotope tree ring records -- 20. Stable isotopes in tree rings of Boreal Forests -- 21. Stable isotopes in tree rings of Mediterranean Forests -- 22. Stable isotopes in tree rings of Tropical forests -- 23. Forest Management and Tree-Ring Isotopes -- 24. Impact of increasing CO2, and air pollutants (NOx, SO2, O3) on the stable isotope ratios in tree rings -- 25. Insect and pathogen influences on tree-ring stable isotopes -- 26. Process-based ecophysiological models of tree-ring stable isotopes.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XXI, 773 p. 106 illus., 76 illus. in color.)
    Edition: 1st ed. 2022.
    ISBN: 9783030926984
    Series Statement: Tree Physiology 8
    RVK:
    Language: English
    Note: Open Access
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  • 3
    ISSN: 1432-1939
    Keywords: Pacific silver fir ; Light acclimation ; Resource distribution ; Leaf nitrogen ; Aging
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Variation in the photosynthetic function ofAbies amabilis foliage within a canopy was examined and related to three different processes that affect foliage function: foliage aging, sun-shade acclimation that occurred while foliage was expanding, and reacclimation after expansion was complete. Foliage produced in the sun had higher photosynthesis at light saturation (A max, μmol·m-2·s-1), dark respiration (μmol·m-2·s-1), nitrogen content (g·m-2), chlorophyll content (g·m-2), and chlorophylla:b ratio, and a lower chlorophyll to nitrogen ratio (chl:N), than foliage produced in the shade. As sun foliage becomes shaded, it becomes physiologically similar to shade foliage, even though it still retains a sun morphology. Shaded sun foliage exhibited lowerA max, dark respiration, nitrogen content, and chlorophylla:b ratio, and a higher chl:N ratio than sun foliage of the same age remaining in the open. However, shaded sun foliage had a higher chlorophyll content than sun foliage remaining in the open, even though true shade foliage had a lower chlorophyll content than sun foliage. This anomaly arises because as sun foliage becomes shaded, it retains a higher nitrogen content than shade foliage in a similar light environment, but the two forms have similar chl:N ratios. Within the canopy, most physiological indicators were more strongly correlated with the current light environment than with foliage age or leaf thickness, with the exception of chlorophyll content.A max decreased significantly with both decreasing current light environment of the foliage and increasing foliage age. The same trend with current light and age was found for the chlorophylla:b ratio. Foliage nitrogen content also decreased with a decrease in current light environment, but no distinct pattern was found with foliage age. Leaf thickness was also important for predicting leaf nitrogen content: thicker leaves had more nitrogen than thinner leaves regardless of light environment or age. The chl:N ratio had a strong negative correlation with the current light environment, and, as with nitrogen content, no distinct pattern was found with foliage age. Chlorophyll content of the foliage was not well correlated with any of the three predictor variables: current light environment, foliage age or leaf thickness. On the other hand, chlorophyll content was positively correlated with the amount of nitrogen in a leaf, and once nitrogen was considered, the current light environment was also highly significant in explaining the variation in chlorophyll content. It has been suggested that the redistribution of nitrogen both within and between leaves is a mechanism for photosynthetic acclimation to the current light environment. Within theseA. amabilis canopies, both leaf nitrogen and the chl:N ratio were strongly correlated with the current light environment, but only weakly with leaf age, supporting the idea that changing light is the driving force for the redistribution of nitrogen both within and between leaves. Thus, our results support previous theories on nitrogen distribution and partitioning. However,A max was significantly affected by both foliage age and the current light environment, indicating that changes in light alone are not enough to explain changes inA max with time.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2014-07-01
    Description: Cellulose δ18O and δD can provide insights on climates and hydrological cycling in the distant past and how these factors differ spatially. However, most studies of plant cellulose have used only one isotope, most commonly δ18O, resulting in difficulties partitioning variation in δ18O of precipitation vs. evaporative conditions that affect leaf water isotopic enrichment. Moreover, observations of pronounced diurnal differences from conventional steady-state model predictions of leaf water isotopic fractionation have cast some doubt on single isotope modeling approaches for separating precipitation and evaporation drivers of cellulose δ18O or δD. We explore a dual isotope approach akin to the concept of deuterium-excess (d), to establish deuterium deviations from the global meteoric water line in leaf water (?dl) as driven by relative humidity (RH). To demonstrate this concept, we survey studies of leaf water δ18O and δD in hardwood vs. conifer trees. We then apply the concept to cellulose δ18O and δD using a mechanistic model of cellulose δ18O and δD to reconstruct deuterium deviations from the global meteoric water line (?dc) in Quercus macrocarpa, Q. robur, and Pseudotsuga menziesii. For each species, ?dc showed strong correlations with RH across sites. ?dc agreed well with steady-state predictions for Q. macrocarpa, while for Q. robur, the relationship with RH was steeper than expected. The slope of ?dc vs. RH of P. menziesii was also close to steady-state predictions, but ?dc were more enriched than predicted. This is in agreement with our leaf water survey showing conifer ?dl was more enriched than predicted. Our data reveal that applications of this method should be appropriate for reconstructing RH from cellulose δ18O and δD after accounting for differences between hardwoods and conifers. Hence, ?dc should be useful for understanding variability in RH associated with past climatic cycles, across regional climates, or across complex terrain where climate modeling is challenging. Furthermore, ?dc and inferred RH values should help in constraining variation in source water δ18O. # doi:10.1890/13-0988.1
    Print ISSN: 1051-0761
    Electronic ISSN: 1939-5582
    Topics: Biology
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