Do 2 H and 18 O in leaf water reflect environmental drivers differently?

© 2022 The Authors New Phytologist © 2022 New Phytologist Foundation.

Bibliographische Detailangaben
Veröffentlicht in:The New phytologist. - 1979. - 235(2022), 1 vom: 30. Juli, Seite 41-51
1. Verfasser: Cernusak, Lucas A (VerfasserIn)
Weitere Verfasser: Barbeta, Adrià, Bush, Rosemary T, Eichstaedt Bögelein, Rebekka, Ferrio, Juan Pedro, Flanagan, Lawrence B, Gessler, Arthur, Martín-Gómez, Paula, Hirl, Regina T, Kahmen, Ansgar, Keitel, Claudia, Lai, Chun-Ta, Munksgaard, Niels C, Nelson, Daniel B, Ogée, Jérôme, Roden, John S, Schnyder, Hans, Voelker, Steven L, Wang, Lixin, Stuart-Williams, Hilary, Wingate, Lisa, Yu, Wusheng, Zhao, Liangju, Cuntz, Matthias
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2022
Zugriff auf das übergeordnete Werk:The New phytologist
Schlagworte:Journal Article Research Support, U.S. Gov't, Non-P.H.S. Research Support, Non-U.S. Gov't evaporative enrichment isotopic biomarker leaf water relative humidity stable isotopes Oxygen Isotopes Water 059QF0KO0R
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520 |a We compiled hydrogen and oxygen stable isotope compositions (δ2 H and δ18 O) of leaf water from multiple biomes to examine variations with environmental drivers. Leaf water δ2 H was more closely correlated with δ2 H of xylem water or atmospheric vapour, whereas leaf water δ18 O was more closely correlated with air relative humidity. This resulted from the larger proportional range for δ2 H of meteoric waters relative to the extent of leaf water evaporative enrichment compared with δ18 O. We next expressed leaf water as isotopic enrichment above xylem water (Δ2 H and Δ18 O) to remove the impact of xylem water isotopic variation. For Δ2 H, leaf water still correlated with atmospheric vapour, whereas Δ18 O showed no such correlation. This was explained by covariance between air relative humidity and the Δ18 O of atmospheric vapour. This is consistent with a previously observed diurnal correlation between air relative humidity and the deuterium excess of atmospheric vapour across a range of ecosystems. We conclude that 2 H and 18 O in leaf water do indeed reflect the balance of environmental drivers differently; our results have implications for understanding isotopic effects associated with water cycling in terrestrial ecosystems and for inferring environmental change from isotopic biomarkers that act as proxies for leaf water 
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650 4 |a Research Support, U.S. Gov't, Non-P.H.S. 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a evaporative enrichment 
650 4 |a isotopic biomarker 
650 4 |a leaf water 
650 4 |a relative humidity 
650 4 |a stable isotopes 
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650 7 |a Water  |2 NLM 
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700 1 |a Barbeta, Adrià  |e verfasserin  |4 aut 
700 1 |a Bush, Rosemary T  |e verfasserin  |4 aut 
700 1 |a Eichstaedt Bögelein, Rebekka  |e verfasserin  |4 aut 
700 1 |a Ferrio, Juan Pedro  |e verfasserin  |4 aut 
700 1 |a Flanagan, Lawrence B  |e verfasserin  |4 aut 
700 1 |a Gessler, Arthur  |e verfasserin  |4 aut 
700 1 |a Martín-Gómez, Paula  |e verfasserin  |4 aut 
700 1 |a Hirl, Regina T  |e verfasserin  |4 aut 
700 1 |a Kahmen, Ansgar  |e verfasserin  |4 aut 
700 1 |a Keitel, Claudia  |e verfasserin  |4 aut 
700 1 |a Lai, Chun-Ta  |e verfasserin  |4 aut 
700 1 |a Munksgaard, Niels C  |e verfasserin  |4 aut 
700 1 |a Nelson, Daniel B  |e verfasserin  |4 aut 
700 1 |a Ogée, Jérôme  |e verfasserin  |4 aut 
700 1 |a Roden, John S  |e verfasserin  |4 aut 
700 1 |a Schnyder, Hans  |e verfasserin  |4 aut 
700 1 |a Voelker, Steven L  |e verfasserin  |4 aut 
700 1 |a Wang, Lixin  |e verfasserin  |4 aut 
700 1 |a Stuart-Williams, Hilary  |e verfasserin  |4 aut 
700 1 |a Wingate, Lisa  |e verfasserin  |4 aut 
700 1 |a Yu, Wusheng  |e verfasserin  |4 aut 
700 1 |a Zhao, Liangju  |e verfasserin  |4 aut 
700 1 |a Cuntz, Matthias  |e verfasserin  |4 aut 
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