Data Entry: Please note that the research database will be replaced by UNIverse by the end of October 2023. Please enter your data into the system https://universe-intern.unibas.ch. Thanks

Login for users with Unibas email account...

Login for registered users without Unibas email account...

 
Tracing plant source water dynamics during drought by continuous transpiration measurements: An in-situ stable isotope approach
JournalArticle (Originalarbeit in einer wissenschaftlichen Zeitschrift)
 
ID 4684104
Author(s) Kübert, Angelika; Dubbert, Maren; Bamberger, Ines; Kühnhammer, Kathrin; Beyer, Matthias; van Haren, Joost; Bailey, Kinzie; Hu, Jia; Meredith, Laura K; Ladd, Sarah Nemiah; Werner, Christiane
Author(s) at UniBasel Ladd, Sarah Nemiah
Year 2023
Title Tracing plant source water dynamics during drought by continuous transpiration measurements: An in-situ stable isotope approach
Journal Plant, cell & environment
Volume 46
Number 1
Pages / Article-Number 133-149
Keywords CRDS, cryogenic vacuum extraction, herbaceous species, laser spectrometry, method comparison, nonwoody, woody, xylem water
Abstract

The isotopic composition of xylem water (δX) is of considerable interest for plant source water studies. In-situ monitored isotopic composition of transpired water (δT) could provide a nondestructive proxy for δX-values. Using flow-through leaf chambers, we monitored 2-hourly δT-dynamics in two tropical plant species, one canopy-forming tree and one understory herbaceous species. In an enclosed rainforest (Biosphere 2), we observed δT-dynamics in response to an experimental severe drought, followed by a 2H deep-water pulse applied belowground before starting regular rain. We also sampled branches to obtain δX-values from cryogenic vacuum extraction (CVE). Daily flux-weighted δ18OT-values were a good proxy for δ18OX-values under well-watered and drought conditions that matched the rainforest's water source. Transpiration-derived δ18OX-values were mostly lower than CVE-derived values. Transpiration-derived δ2HX-values were relatively high compared to source water and consistently higher than CVE-derived values during drought. Tracing the 2H deep-water pulse in real-time showed distinct water uptake and transport responses: a fast and strong contribution of deep water to canopy tree transpiration contrasting with a slow and limited contribution to understory species transpiration. Thus, the in-situ transpiration method is a promising tool to capture rapid dynamics in plant water uptake and use by both woody and nonwoody species.

 
ISSN/ISBN 0140-7791
URL https://onlinelibrary.wiley.com/doi/10.1111/pce.14475
Full Text on edoc
Digital Object Identifier DOI https://doi.org/10.1111/pce.14475
   

MCSS v5.8 PRO. 0.550 sec, queries - 0.000 sec ©Universität Basel  |  Impressum   |    
02/03/2024