No evidence of homeostatic regulation of leaf temperature in Eucalyptus parramattensis trees : integration of CO2 flux and oxygen isotope methodologies

© 2020 The Authors. New Phytologist © 2020 New Phytologist Foundation.

Bibliographische Detailangaben
Veröffentlicht in:The New phytologist. - 1979. - 228(2020), 5 vom: 21. Dez., Seite 1511-1523
1. Verfasser: Drake, John E (VerfasserIn)
Weitere Verfasser: Harwood, Richard, Vårhammar, Angelica, Barbour, Margaret M, Reich, Peter B, Barton, Craig V M, Tjoelker, Mark G
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2020
Zugriff auf das übergeordnete Werk:The New phytologist
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Eucalyptus parramattensis carbon cycle climate warming endothermy photosynthesis temperature regulation Oxygen Isotopes Carbon Dioxide 142M471B3J
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245 1 0 |a No evidence of homeostatic regulation of leaf temperature in Eucalyptus parramattensis trees  |b integration of CO2 flux and oxygen isotope methodologies 
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500 |a Date Revised 26.04.2021 
500 |a published: Print-Electronic 
500 |a CommentIn: New Phytol. 2020 Dec;228(5):1455-1457. - PMID 33011978 
500 |a Citation Status MEDLINE 
520 |a © 2020 The Authors. New Phytologist © 2020 New Phytologist Foundation. 
520 |a Thermoregulation of leaf temperature (Tleaf ) may foster metabolic homeostasis in plants, but the degree to which Tleaf is moderated, and under what environmental contexts, is a topic of debate. Isotopic studies inferred the temperature of photosynthetic carbon assimilation to be a constant value of c. 20°C; by contrast, leaf biophysical theory suggests a strong dependence of Tleaf on environmental drivers. Can this apparent disparity be reconciled? We continuously measured Tleaf and whole-crown net CO2 uptake for Eucalyptus parramattensis trees growing in field conditions in whole-tree chambers under ambient and +3°C warming conditions, and calculated assimilation-weighted leaf temperature (TL-AW ) across 265 d, varying in air temperature (Tair ) from -1 to 45°C. We compared these data to TL-AW derived from wood cellulose δ18 O. Tleaf exhibited substantial variation driven by Tair , light intensity, and vapor pressure deficit, and Tleaf was strongly linearly correlated with Tair with a slope of c. 1.0. TL-AW values calculated from cellulose δ18 O vs crown fluxes were remarkably consistent; both varied seasonally and in response to the warming treatment, tracking variation in Tair . The leaves studied here were nearly poikilothermic, with no evidence of thermoregulation of Tleaf towards a homeostatic value. Importantly, this work supports the use of cellulose δ18 O to infer TL-AW , but does not support the concept of strong homeothermic regulation of Tleaf 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a Eucalyptus parramattensis 
650 4 |a carbon cycle 
650 4 |a climate warming 
650 4 |a endothermy 
650 4 |a photosynthesis 
650 4 |a temperature regulation 
650 7 |a Oxygen Isotopes  |2 NLM 
650 7 |a Carbon Dioxide  |2 NLM 
650 7 |a 142M471B3J  |2 NLM 
700 1 |a Harwood, Richard  |e verfasserin  |4 aut 
700 1 |a Vårhammar, Angelica  |e verfasserin  |4 aut 
700 1 |a Barbour, Margaret M  |e verfasserin  |4 aut 
700 1 |a Reich, Peter B  |e verfasserin  |4 aut 
700 1 |a Barton, Craig V M  |e verfasserin  |4 aut 
700 1 |a Tjoelker, Mark G  |e verfasserin  |4 aut 
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