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  • 1
    Call number: AWI G6-92-0403
    In: Ecological studies, 68
    Description / Table of Contents: The analysis of stable isotope ratios represents one of the most exciting new technical advances in environmental sciences. In this book, leading experts offer the first survey of applications of stable isotope analysis to ecological research. Central topics are plant physiology studies, food webs and animal metabolism, bio-geochemical fluxes. Extensive coverage is given to natural isotopes of carbon, hydrogen, oxygen, nitrogen, sulfur, and strontium in both terrestrial and marine ecosystems. Ecologists of diverse research interests, as well as agronomists, anthropologists, and geochemists, will value this overview for its wealth of information on theoretical background, experimental approaches, and technical design of studies utilizing stable isotope ratios.
    Type of Medium: Monograph available for loan
    Pages: XV, 525 Seiten , Illustrationen
    ISBN: 0387967125
    Series Statement: Ecological studies 68
    Language: English
    Note: Contents: Preface Contributors 1. Stable Isotopes: History, Units, and Instrumentation / J. R. Ehleringer and P. W. Rundel Section I Ecophysiological Studies in Plants 2.Carbon Isotope Fractionation and Plant Water-Use Efficiency / G. D. Farquhar, K. T. Hubick, A. G. Condon, and R. A. Richards 3. Carbon Isotope Ratios and Physiological Processes in Aridland Plants / J. R. Ehleringer 4. Stable Carbon Isotope Ratio as an Index of Water-Use Efficiency in C3 Halophytes - Possible Relationship to Strategies for Osmotic Adjustment / R. D. Guy, P. G. Warne, and D. M. Reid 5. Stable Carbon Isotopes in Vernal Pool Aquatics of Differing Photosynthetic Pathways / J. E. Keeley 6. Studies of Mechanisms Affecting the Fractionation of Carbon Isotopes in Photosynthesis / J. A. Berry 7. Intertree Variability of δ13C in Tree Rings / S. W. Leavitt, and A. Long 8. Hydrogen Isotope Fractionation in Plant Tissues / H. Ziegler 9. Oxygen and Hydrogen Isotope Ratios in Plant Cellulose: Mechanisms and Applications / L. Da Silveira Lobo Sternberg 10. Stable Hydrogen Isotope Ratios in Plants: A Review of Current Theory and Some Potential Applications / J. W. C. White Section II Animal Food Webs and Feeding Ecology 11. Stable Carbon Isotopes in Terrestrial Ecosystem Research / L. L. Tieszen and T. W. Boutton 12. δ13C Measurements as Indicators of Carbon Flow in Marine and Freshwater Ecosystems / B. Fry and E. B. Sherr 13. Natural Carbon Isotope Tracers in Arctic Aquatic Food Webs / D. M. Schell and P. J. Ziemann 14. Some Problems and Potentials of Strontium Isotope Analysis for Human and Animal Ecology / J. E. Ericson 15. Natural Isotope Abundances in Bowhead Whale (Balaena mysticetus) Baleen: Markers of Aging and Habitat Usage / D. M. Schell, S. M. Saupe, and N. Haubenstock 16. Doubly-Labeled Water Studies of Vertebrate Physiological Ecology / K. A. NAGY 17. A δ13C and δ15N Tracer Study of Nutrition in Aquaculture: Penaeus vannamei in a Pond Growout System / P. L. Parker, R. K. Anderson, and A. Lawrence Section III Ecosystem Process Studies 18. Stable Isotope Ratios and the Dynamics of Caliche in Desert Soils / W. H. Schlesinger, G. M. Marion, and P. J. Fonteyn 19. The Use of Stable Isotopes in Assessing the Effect of Agriculture on Arid and Semi-Arid Soils / R. Amundson 20. Estimates of N2 Fixation in Ecosystems: The Need for and Basis of the 15N Natural Abundance Method / G. Shearer and D. H. Kohl 21. The Use of Variation in the Natural Abundance of 15N to Assess Symbiotic Nitrogen Fixation by Woody Plants / R. A. Virginia, W. M. Jarrell, P. W. Rundel, G. Shearer, and D. H. Kohl 22. 13C/12C Ratios in Atmospheric Methane and Some of Its Sources / S. C. Tyler 23. Temperature-Dependent Hydrogen Isotope Fractionation in Cyanobacterial Sheaths: Applications to Studies of Modern and Precambrian Stromatolites / G. E. Strathearn 24. Sulfur Isotope Studies of the Pedosphere and Biosphere / H. R. Krouse 25. Sulfate Fertilization and Changes in Stable Sulfur Isotopic Compositions of Lake Sediments / B. Fry 26. The Use of Stable Sulfur and Nitrogen Isotopes in Studies of Plant Responses to Air Pollution / W. E. Winner, V. S. Berg, and P. J. Langston-Unkefer 27. The Use of Stable Sulfur Isotope Ratios in Air Pollution Studies: An Ecosystem Approach in South Florida / L. L. Jackson and L. P. Gough 28. 87Sr/86Sr Ratios Measure the Sources and Flow of Strontium in Terrestrial Ecosystems / W. C. Graustein Index
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Ecology, Evolution, and Systematics 24 (1993), S. 411-439 
    ISSN: 0066-4162
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: We tested the hypothesis that the stable carbon isotope signature of ecosystem respiration (δ13CR) was regulated by canopy conductance (Gc) using weekly Keeling plots (n=51) from a semiarid old-growth ponderosa pine (Pinus ponderosa) forest in Oregon, USA. For a comparison of forests in two contrasting climates we also evaluated trends in δ13CR from a wet 20-year-old Douglas-fir (Pseudotsuga menziesii) plantation located near the Pacific Ocean. Intraannual variability in δ13CR was greater than 8.0‰ at both sites, was highest during autumn, winter, and spring when rainfall was abundant, and lowest during summer drought. The δ13CR of the dry pine forest was consistently more positive than the wetter Douglas-fir forest (mean annual δ13CR: −25.41‰ vs. −26.23‰, respectively, P=0.07). At the Douglas-fir forest, δ13CR–climate relationships were consistent with predictions based on stomatal regulation of carbon isotope discrimination (Δ). Soil water content (SWC) and vapor pressure deficit (vpd) were the most important factors governing δ13CR in this forest throughout the year. In contrast, δ13CR at the pine forest was relatively insensitive to SWC or vpd, and exhibited a smaller drought-related enrichment (∼2‰) than the enrichment observed during drought at the Douglas-fir forest (∼5‰). Groundwater access at the pine forest may buffer canopy–gas exchange from drought. Despite this potential buffering, δ13CR at the pine forest was significantly but weakly related to canopy conductance (Gc), suggesting that δ13CR remains coupled to canopy–gas exchange despite groundwater access. During drought, δ13CR was strongly correlated with soil temperature at both forests. The hypothesis that canopy-level physiology is a critical regulator of δ13CR was supported; however, belowground respiration may become more important during rain-free periods.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: The δ13C values of atmospheric carbon dioxide (CO2) can be used to partition global patterns of CO2 source/sink relationships among terrestrial and oceanic ecosystems using the inversion technique. This approach is very sensitive to estimates of photosynthetic 13C discrimination by terrestrial vegetation (ΔA), and depends on δ13C values of respired CO2 fluxes (δ13CR). Here we show that by combining two independent data streams – the stable isotope ratios of atmospheric CO2 and eddy-covariance CO2 flux measurements – canopy scale estimates of ΔA can be successfully derived in terrestrial ecosystems. We also present the first weekly dataset of seasonal variations in δ13CR from dominant forest ecosystems in the United States between 2001 and 2003. Our observations indicate considerable summer-time variation in the weekly value of δ13CR within coniferous forests (4.0‰ and 5.4‰ at Wind River Canopy Crane Research Facility and Howland Forest, respectively, between May and September). The monthly mean values of δ13CR showed a smaller range (2–3‰), which appeared to significantly correlate with soil water availability. Values of δ13CR were less variable during the growing season at the deciduous forest (Harvard Forest). We suggest that the negative correlation between δ13CR and soil moisture content observed in the two coniferous forests should represent a general ecosystem response to the changes in the distribution of water resources because of climate change. Shifts in δ13CR and ΔA could be of sufficient magnitude globally to impact partitioning calculations of CO2 sinks between oceanic and terrestrial compartments.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Plant Physiology and Plant Molecular Biology 40 (1989), S. 503-537 
    ISSN: 1040-2519
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Plant, cell & environment 19 (1996), S. 0 
    ISSN: 1365-3040
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Studies that quantify plant δ15N often assume that fractionation during nitrogen uptake and intra-plant variation in δ15N are minimal. We tested both assumptions by growing tomato (Lycopersicon esculetum Mill. cv. T-5) at NH4+ or NO−3 concentrations typical of those found in the soil. Fractionation did not occur with uptake; whole-plant δ15N was not significantly different from source δ15 N for plants grown on either nitrogen form. No intra-plant variation in δ15N was observed for plants grown with NH+4. In contrast. δ15N of leaves was as much as 5.8% greater than that of roots for plants grown with NO−3. The contrasting patterns of intra-plant variation are probably caused by different assimilation patterns. NH+4 is assimilated immediately in the root, so organic nitrogen in the shoot and root is the product of a single assimilation event. NO−3 assimilation can occur in shoots and roots. Fractionation during assimilation caused the δ15N of NO−3 to become enriched relative to organic nitrogen; the δ15N of NO−3 was 11.1 and 12.9% greater than the δ15N of organic nitrogen in leaves and roots, respectively. Leaf δ15N may therefore be greater than that of roots because the NO−3 available for assimilation in leaves originates from a NO−3 pool that was previously exposed to nitrate assimilation in the root.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Plant, cell & environment 14 (1991), S. 0 
    ISSN: 1365-3040
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Abstract. The effects of modification of photon flux density (PFD, 400-700 nm) on paraheliotropic leaf movement were examined in Phaseolus vulgaris L. under controlled environmental conditions. The cosine of the angle of incidence to directional PFD (cos(i)), a measure of leaf movement, was linearly and negatively related to PFD. That is, leaflets progressively oriented away from a direct light beam in response to increasing PFD. The minimum PFD causing paraheliotropic movement was approximately 25 μmol m−2 s−1. When PFD was varied, tissue temperature changed due to an altered energy balance. Since a change in pulvinus temperature can affect leaf movement, experiments were conducted to distinguish the effects of PFD signal and pulvinis temperature. Leaflets oriented to reduce incident PFD levels in response to increasing PFD (either white light or blue light) when pulvinis temperature was kept constant. From these results, we conclude that changes in PFD signals alone can control paraheliotropic leaf movements. Phaseolus vulgaris grown outdoors oriented their leaflets to face towards the sun in the morning and again in late afternoon, but avoided the sun's direct rays at midday. This diurnal pattern of paraheliotropic leaf movements can be explained on the basis of known paraheliotropic movements in response to PFD and air temperature.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Plant, cell & environment 9 (1986), S. 0 
    ISSN: 1365-3040
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Abstract Leaves of Lotus scoparius Nutt., a Mediterranean-climate shrub, exhibited higher photosynthetic capacities when grown under winter (10/14 h, day/night) than summer (14/10 h) photo-periods, even though total daily photon irradiance was higher under summer photoperiods. Photosynthetic dependence on natural variations in photo-period, such that activity was higher under photo-periods associated with expected precipitation, may be a more dependable environmental parameter than total irradiance in temperate habitats with winter-spring precipitation patterns and where seasonal cloudiness may cause total daily irradiance levels to be highly variable.
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Plant, cell & environment 16 (1993), S. 0 
    ISSN: 1365-3040
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Photosynthetic gas exchange and the stable isotopic composition of foliage water were measured for a xylem tapping mistletoe, Phoradendron juniperinum, and its host tree, Juniperus osteosperma, growing in southern Utah. The observed isotopic composition of water extracted from foliage was compared to predictions of the Craig-Gordon model of isotopic enrichment at evaporative sites within leaves. Assimilation rates of juniper were higher and stomatal conductance was lower than the values observed for the mistletoe. This resulted in lower intercellular/ ambient CO2 values in the juniper tree relative to its mistletoe parasite. For mistletoe, the observed foliage water hydrogen and oxygen isotopic enrichment was less than that predicted by the model. In juniper, foliage water hydrogen isotopic enrichment was also lower than that predicted by the evaporative enrichment model. In contrast, the oxygen isotopic enrichment in juniper foliage water was slightly greater than that predicted for the evaporative sites within leaves. Hydrogen isotopic enrichment in mistletoe foliage shows systematic variation with stem segment, being highest near the tips of the youngest stems and decreasing toward the base of the mistletoe, where isotopic composition is close to that of stem water in the host tree. In a correlated pattern, mid-day stomatal conductance declined abruptly in mistletoe foliage of increasing age.
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Plant, cell & environment 19 (1996), S. 0 
    ISSN: 1365-3040
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: The carbon isotope composition of C4 grasses has the potential to be used as an indicator of changes in the isotopic composition and concentration of atmospheric CO2, especially for climate reconstruction. The usefulness of C4 grasses for this purpose hinges on the assumption that their photosynthetic discrimination against 13C remains constant in a wide range of environmental conditions. We tested this assumption by examining the effects of light and water stress on the carbon isotope composition of C4 grasses using different biochemical subtypes (NADP-ME, NAD-ME, PCK) in glasshouse experiments. We grew 14 different C4 grass species in four treatments: sun-watered, sun-drought, shade-watered and shade-drought. Carbon isotope discrimination (Δ) rarely remained constant. In general, Δ values were lowest in sun-watered grasses, greater for sun-drought plants and even higher for plants of the shade-watered treatment. The highest Δ values were generally found in the most stressed grasses, the shade-drought plants. Grasses of the NADP-ME subtype were the least influenced by a change in environmental variables, followed by PCK and NAD-ME subtypes. Water availability affected the carbon isotope discrimination less than light limitation in PCK and NAD-ME subtypes, but similarly in NADP-ME subtypes.In another experiment, we studied the effect of increasing light levels (150 to 1500 μmol photons m−2 s−1) on the Δ values of 18 well-watered C4 grass species. Carbon isotope discrimination remained constant until photon flux density (PFD) was less than 700 μmol photons m−2 s−1. Below this light level, Δ values increased with decreasing irradiance for all biochemical subtypes. The change in A was less pronounced in NADP-ME and PCK than in NAD-ME grasses. Grasses grown in the field and in the glasshouse showed a similar pattern. Thus, caution should be exercised when using C4 plants under varying environmental conditions to monitor the concentration or carbon isotopic composition of atmospheric CO2 in field/glasshouse studies or climate reconstruction.
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