How do precipitation events modify the stable isotope ratios in leaf water at Lhasa on the southern Tibetan Plateau?

References

• Galewsky J, Steen-Larsen HC, Field RD, et al. Stable isotopes in atmospheric water vapor and applications to the hydrologic cycle. Rev Geophys. 2016;54:809–865.
   PubMed Web of Science ®Google Scholar
• Yao T, Masson-Delmotte V, Gao J, et al. A review of climatic controls on δ18O in precipitation over the Tibetan Plateau: Observations and simulations. Rev Geophys. 2013;51:525–548.
   Web of Science ®Google Scholar
• Sprenger M, Leistert H, Gimbel K, et al. Illuminating hydrological processes at the soil–vegetation–atmosphere interface with water stable isotopes. Rev Geophys. 2016;54:674–704.
   Web of Science ®Google Scholar
• Dubbert M, Werner C. Water fluxes mediated by vegetation: emerging isotopic insights at the soil and atmosphere interfaces. New Phytol. 2019;221:1754–1763.
   PubMedGoogle Scholar
• Yakir D, Wang XF. Fluxes of CO2 and water between terrestrial vegetation and the atmosphere estimated from isotope measurements. Nature. 1996;380:515–517.
   Web of Science ®Google Scholar
• Hoffmann G, Cuntz M, Weber C, et al. A model of the Earth’s Dole effect. Glob Biogeochem Cycl. 2004;18:GB1008.
   Google Scholar
• Griffis TJ, Lee X, Baker JM, et al. Oxygen isotope composition of evapotranspiration and its relation to C4 photosynthetic discrimination. J Geophys Res Biogeosci. 2011;116:G01035.
   Google Scholar
• Roden JS, Lin G, Ehleringer JR. A mechanistic model for interpretation of hydrogen and oxygen isotope ratios in tree-ring cellulose. Geochim Cosmochim Acta. 2000;64:21–35.
   Web of Science ®Google Scholar
• McCarroll D, Loader NJ. Stable isotopes in tree rings. Quat Sci Rev. 2004;23:771–801.
   Web of Science ®Google Scholar
• Kahmen A, Sachse D, Arndt SK, et al. Cellulose δ18O is an index of leaf-to-air vapor pressure difference (VPD) in tropical plants. Proc Natl Acad Sci USA. 2011;108:1981–1986.
   PubMed Web of Science ®Google Scholar
• Kahmen A, Hoffmann B, Schefuss E, et al. Leaf water deuterium enrichment shapes leaf wax n-alkane δD values of angiosperm plants II: Observational evidence and global implications. Geochim Cosmochim Acta. 2013;111:50–63.
   Web of Science ®Google Scholar
• Treydte KS, Boda S, Pannatier EG, et al. Seasonal transfer of oxygen isotopes from precipitation and soil to the tree ring: source water versus needle water enrichment. New Phytol. 2014;202:772–783.
   PubMedGoogle Scholar
• Yu W, Xu B, Lai C, et al. Influences of relative humidity and Indian monsoon precipitation on leaf water stable isotopes from the southeastern Tibetan Plateau. Geophys Res Lett. 2014;41:7746–7753.
   Google Scholar
• Liu H, Schaufele R, Gong X, et al. δ18O and δ2H of water in the leaf growth-and-differentiation zone of grasses is close to source water in both humid and dry atmospheres. New Phytol. 2017;214:1423–1431.
   PubMedGoogle Scholar
• Barbour MM. Stable oxygen isotope composition of plant tissue: a review. Funct Plant Biol. 2007;34(2):83–94.
   PubMed Web of Science ®Google Scholar
• Zeng X, Liu X, Evans MN, et al. Seasonal incursion of Indian Monsoon humidity and precipitation into the southeastern Qinghai–Tibetan Plateau inferred from tree ring δ18O values with intra-seasonal resolution. Earth Planet Sci Lett. 2016;443:9–19.
   Google Scholar
• Wernicke J, Hochreuther P, Grießinger J, et al. Multi-century humidity reconstructions from the southeastern Tibetan Plateau inferred from tree-ring δ18O. Glob Planet Change. 2017;149:26–35.
   Google Scholar
• Grießinger J, Bräuning A, Helle G, et al. Late Holocene Asian summer monsoon variability reflected by δ18O in tree-rings from Tibetan junipers. Geophys Res Lett. 2011;38:L03701.
   Web of Science ®Google Scholar
• Sano M, Tshering P, Komori J, et al. May–September precipitation in the Bhutan Himalaya since 1743 as reconstructed from tree ring cellulose δ18O. J Geophys Res Atmos. 2013;118:8399–8410.
   Web of Science ®Google Scholar
• Xu C, Shao X, An W, et al. Negligible local-factor influences on tree ring cellulose δ18O of Qilian juniper in the Animaqing Mountains of the eastern Tibetan Plateau. Tellus Ser B–Chem Phys Meteorol. 2017;69:1391663.
   Web of Science ®Google Scholar
• Treydte KS, Schleser GH, Helle G, et al. The twentieth century was the wettest period in northern Pakistan over the past millennium. Nature. 2006;440:1179–1182.
   PubMed Web of Science ®Google Scholar
• Liu X, Shao X, Liang E, et al. Climatic significance of tree-ring δ18O in the Qilian Mountains, northwestern China and its relationship to atmospheric circulation patterns. Chem Geol. 2009;268:147–154.
   Google Scholar
• Huang R, Zhu H, Liang E, et al. Temperature signals in tree-ring oxygen isotope series from the northern slope of the Himalaya. Earth Planet Sci Lett. 2019;506:455–465.
   Google Scholar
• Wang XT, Wen XF. Leaf water δD and δ18O enrichment process and influencing factors in spring maize (Zea mays) grown in the middle reaches of Heihe River Basin. Chin J Plant Ecol. 2016;40:912–924.
   Google Scholar
• Yu W, Yao T, Tian L, et al. Relationships between δ18O in precipitation and air temperature and moisture origin on a south–north transect of the Tibetan Plateau. Atmos Res. 2008;87:158–169.
   Web of Science ®Google Scholar
• Lai CT, Ometto JPHB, Berry JA, et al. Life form-specific variations in leaf water oxygen-18 enrichment in Amazonian vegetation. Oecologia. 2008;157:197–210.
   PubMedGoogle Scholar
• Yu W, Tian L, Ma Y, et al. Simultaneous monitoring of stable oxygen isotope composition in water vapour and precipitation over the central Tibetan Plateau. Atmos Chem Phys. 2015;15:14445–14472.
   Google Scholar
• Yu W, Tian L, Risi C, et al. δ18O records in water vapor and an ice core from the eastern Pamir Plateau: Implications for paleoclimate reconstructions. Earth Planet Sci Lett. 2016;456:146–156.
   Google Scholar
• West AG, Patrickson SJ, Ehleringer JR. Water extraction times for plant and soil materials used in stable isotope analysis. Rapid Commun Mass Spectrom. 2006;20:1317–1321.
   PubMed Web of Science ®Google Scholar
• Farris F, Strain BR. The effects of water-stress on leaf H218O enrichment. Radiat Environ Biophys. 1978;15:167–202.
   PubMed Web of Science ®Google Scholar
• Zhao L, Wang L, Cernusak LA, et al. Significant difference in hydrogen isotope composition between xylem and tissue water in Populus euphratica. Plant Cell Environ. 2016;39:1848–1857.
   PubMed Web of Science ®Google Scholar
• Craig H, Gordon LI. Deuterium and oxygen 18 variations in the ocean and the marine atmosphere. In: Tongiorgi E, editor. Stable isotopes in oceanographic studies and paleotemperatures. Pisa: Consiglio nazionale delle richerche, Laboratorio de geologia nucleare. 1965: 9–72.
   Google Scholar
• Flanagan LB, Comstock JP, Ehleringer JR. Comparison of modeled and observed environmental influences on the stable oxygen and hydrogen isotope composition of leaf water in Phaseolus vulgaris L. Plant Physiol. 1991;96(2):588–596.
   PubMedGoogle Scholar
• Farquhar GD, Hubick KT, Condon AG, et al. Carbon isotope fractionation and plant water-use efficiency. In: Rundel PW, Ehleringer JR, Nagy KA, editor. Stable isotopes in ecological research. New York: Springer; 1989. p. 21–40.
   Google Scholar
• Leaney FW, Osmond CB, Allison GB, et al. Hydrogen-isotope composition of leaf water in C3 and C4 plants: its relationship to the hydrogen-isotope composition of dry matter. Planta. 1985;164(2):215–220.
   PubMedGoogle Scholar
• Dongmann G, Nürnberg HW, Förstel H, et al. On the enrichment of H218O in the leaves of transpiring plants. Radiat Environ Biophys. 1974;11:41–52.
   PubMed Web of Science ®Google Scholar
• Farquhar GD, Cernusak LA. On the isotopic composition of leaf water in the non-steady state. Funct Plant Biol. 2005;32:293–303.
   PubMed Web of Science ®Google Scholar
• Cuntz M, Ogée J, Farquhar GD, et al. Modelling advection and diffusion of water isotopologues in leaves. Plant Cell Environ. 2007;30:892–909.
   PubMedGoogle Scholar
• Ogée J, Cuntz M, Peylin P, et al. Non-steady-state, non-uniform transpiration rate and leaf anatomy effects on the progressive stable isotope enrichment of leaf water along monocot leaves. Plant Cell Environ. 2007;30:367–387.
   PubMed Web of Science ®Google Scholar
• Majoube M. Fractionnement en oxygène 18 et en deutérium entre l'eau et sa vapeur. J Chim Phys Phys Chim Biol. 1971;10:1423–1436. French.
   Web of Science ®Google Scholar
• Merlivat L. The dependence of bulk evaporation coefficients on air–water interfacial conditions as determined by the isotopic method. J Geophys Res. 1978;83:2977–2980.
   Web of Science ®Google Scholar
• Phillips DL, Gregg JW. Source partitioning using stable isotopes: coping with too many sources. Oecologia. 2003;136(2):261–269.
   PubMed Web of Science ®Google Scholar
• Chen YL, Helliker BR, Tang XH, et al. Stem water cryogenic extraction biases estimation in deuterium isotope composition of plant source water. Proc Natl Acad Sci USA. 2020;117:33345–33350.
   PubMedGoogle Scholar
• Tian L, Yu W, Schuster PF, et al. Control of seasonal water vapor isotope variations at Lhasa, southern Tibetan Plateau. J Hydrol. 2020;580:124237.
   Google Scholar
• Dansgaard W. Stable isotopes in precipitation. Tellus. 1964;16:436–468.
   Google Scholar
• Cernusak LA, Pate JS, Farquhar GD. Diurnal variation in the stable isotope composition of water and dry matter in fruiting Lupinus angustifolius under field conditions. Plant Cell Environ. 2002;25:893–907.
   Web of Science ®Google Scholar
• Kannenberg SA, Fiorella RP, Anderegg WRL, et al. Seasonal and diurnal trends in progressive isotope enrichment along needles in two pine species. Plant Cell Environ. 2021;44:143–155.
   PubMedGoogle Scholar
• Snyder KA, Monnar R, Poulson SR, et al. Diurnal variations of needle water isotopic ratios in two pine species. Trees–Struct Funct. 2010;24:585–595.
   Google Scholar
• Welp LR, Lee X, Kim K, et al. δ18O of water vapour, evapotranspiration and the sites of leaf water evaporation in a soybean canopy. Plant Cell Environ. 2008;31:1214–1228.
   PubMed Web of Science ®Google Scholar
• Plavcová L, Hronková M, Šimková M, et al. Seasonal variation of δ18O and δ2H in leaf water of Fagus sylvatica L. and related water compartments. J Plant Physiol. 2018;227:56–65.
   PubMedGoogle Scholar
• Cernusak LA, Pate JS, Farquhar GD. Diurnal variation in the stable isotope composition of water and dry matter in fruiting Lupinus angustifolius under field conditions. Plant Cell Environ. 2002;25:893–907.
   Web of Science ®Google Scholar
• Cernusak LA, Mejia-Chang M, Winter K, et al. Oxygen isotope composition of CAM and C3 Clusia species: non-steady-state dynamics control leaf water 18O enrichment in succulent leaves. Plant Cell Environ. 2008;31:1644–1662.
   PubMedGoogle Scholar
• Cooper LW, DeNiro MJ. Covariance of oxygen and hydrogen isotopic compositions in plant water: species effects. Ecology. 1989;70:1619–1628.
   Web of Science ®Google Scholar
• Kahmen A, Simonin K, Tu KP, et al. Effects of environmental parameters, leaf physiological properties and leaf water relations on leaf water δ18O enrichment in different Eucalyptus species. Plant Cell Environ. 2008;31:738–751.
   PubMed Web of Science ®Google Scholar
• Zhao W, Liu B. The response of sap flow in shrubs to rainfall pulses in the desert region of China. Agric For Meteorol. 2010;150:1297–1306.
   Web of Science ®Google Scholar
• Hovenden MJ, Seppelt RD. Uptake of water from the atmosphere by lichens in continental Antarctica. Symbiosis. 1995;18:111–118.
   Google Scholar
• Farquhar GD, Graham D, Cernusak LA. Heavy water fractionation during transpiration. Plant Physiol. 2007;143:11–18.
   PubMed Web of Science ®Google Scholar
• Cernusak LA, Barbour MM, Arndt SK, et al. Stable isotopes in leaf water of terrestrial plants. Plant Cell Environ. 2016;39:1087–1102.
   PubMed Web of Science ®Google Scholar
• Hussain MZ, Saraswathi G, Lalrammawia C, et al. Leaf and ecosystem gas exchange responses of buffel grass-dominated grassland to summer precipitation. Pedosphere. 2015;25:112–123.
   Google Scholar
• Bögelein R, Thomas FM, Kahmen A. Leaf water 18O and 2H enrichment along vertical canopy profiles in a broadleaved and a conifer forest tree. Plant Cell Environ. 2017;40:1086–1103.
   PubMedGoogle Scholar
• Roden JS, Ehleringer JR. Observations of hydrogen and oxygen isotopes in leaf water confirm the Craig–Gordon model under wide-ranging environmental conditions. Plant Physiol. 1999;120:1165–1173.
   PubMed Web of Science ®Google Scholar
• Song X, Loucos KE, Simonin KA. Measurements of transpiration isotopologues and leaf water to assess enrichment models in cotton. New Phytol. 2015;206:637–646.
   PubMedGoogle Scholar
• Volkmann THM, Haberer K, Gessler A, et al. High-resolution isotope measurements resolve rapid ecohydrological dynamics at the soil–plant interface. New Phytol. 2016;210:839–849.
   PubMed Web of Science ®Google Scholar
• Porporato A, Daly E, Rodriguez-Iturbe I. Soil water balance and ecosystem response to climate change. Am Nat. 2004;164:625–632.
   PubMed Web of Science ®Google Scholar
• Goldsmith GR, Muñoz-Villers LE, Holwerda F, et al. Stable isotopes reveal linkages among ecohydrological processes in a seasonally dry tropical montane cloud forest. Ecohydrology. 2012;5:779–790.
   Google Scholar
• Simonin KA, Roddy AB, Link P, et al. Isotopic composition of transpiration and rates of change in leaf water isotopologue storage in response to environmental variables. Plant Cell Environ. 2013;36:2190–2206.
   PubMedGoogle Scholar