|
|
|
|
| LEADER |
01000naa a22002652 4500 |
| 001 |
NLM361776225 |
| 003 |
DE-627 |
| 005 |
20231226085843.0 |
| 007 |
cr uuu---uuuuu |
| 008 |
231226s2023 xx |||||o 00| ||eng c |
| 024 |
7 |
|
|a 10.1111/nph.19248
|2 doi
|
| 028 |
5 |
2 |
|a pubmed24n1205.xml
|
| 035 |
|
|
|a (DE-627)NLM361776225
|
| 035 |
|
|
|a (NLM)37680025
|
| 040 |
|
|
|a DE-627
|b ger
|c DE-627
|e rakwb
|
| 041 |
|
|
|a eng
|
| 100 |
1 |
|
|a Holloway-Phillips, Meisha
|e verfasserin
|4 aut
|
| 245 |
1 |
0 |
|a Covariation between oxygen and hydrogen stable isotopes declines along the path from xylem water to wood cellulose across an aridity gradient
|
| 264 |
|
1 |
|c 2023
|
| 336 |
|
|
|a Text
|b txt
|2 rdacontent
|
| 337 |
|
|
|a ƒaComputermedien
|b c
|2 rdamedia
|
| 338 |
|
|
|a ƒa Online-Ressource
|b cr
|2 rdacarrier
|
| 500 |
|
|
|a Date Completed 03.11.2023
|
| 500 |
|
|
|a Date Revised 03.11.2023
|
| 500 |
|
|
|a published: Print-Electronic
|
| 500 |
|
|
|a Citation Status MEDLINE
|
| 520 |
|
|
|a © 2023 The Authors. New Phytologist © 2023 New Phytologist Foundation.
|
| 520 |
|
|
|a Oxygen and hydrogen isotopes of cellulose in plant biology are commonly used to infer environmental conditions, often from time series measurements of tree rings. However, the covariation (or the lack thereof) between δ18 O and δ2 H in plant cellulose is still poorly understood. We compared plant water, and leaf and branch cellulose from dominant tree species across an aridity gradient in Northern Australia, to examine how δ18 O and δ2 H relate to each other and to mean annual precipitation (MAP). We identified a decline in covariation from xylem to leaf water, and onwards from leaf to branch wood cellulose. Covariation in leaf water isotopic enrichment (Δ) was partially preserved in leaf cellulose but not branch wood cellulose. Furthermore, whilst δ2 H was well-correlated between leaf and branch, there was an offset in δ18 O between organs that increased with decreasing MAP. Our findings strongly suggest that postphotosynthetic isotope exchange with water is more apparent for oxygen isotopes, whereas variable kinetic and nonequilibrium isotope effects add complexity to interpreting metabolic-induced δ2 H patterns. Varying oxygen isotope exchange in wood and leaf cellulose must be accounted for when δ18 O is used to reconstruct climatic scenarios. Conversely, comparing δ2 H and δ18 O patterns may reveal environmentally induced shifts in metabolism
|
| 650 |
|
4 |
|a Journal Article
|
| 650 |
|
4 |
|a Australia
|
| 650 |
|
4 |
|a aridity
|
| 650 |
|
4 |
|a cellulose
|
| 650 |
|
4 |
|a hydrogen isotopes
|
| 650 |
|
4 |
|a isotope tree-ring
|
| 650 |
|
4 |
|a oxygen isotopes
|
| 650 |
|
4 |
|a paleo-environmental reconstruction
|
| 650 |
|
7 |
|a Oxygen
|2 NLM
|
| 650 |
|
7 |
|a S88TT14065
|2 NLM
|
| 650 |
|
7 |
|a Cellulose
|2 NLM
|
| 650 |
|
7 |
|a 9004-34-6
|2 NLM
|
| 650 |
|
7 |
|a Carbon Isotopes
|2 NLM
|
| 650 |
|
7 |
|a Hydrogen
|2 NLM
|
| 650 |
|
7 |
|a 7YNJ3PO35Z
|2 NLM
|
| 650 |
|
7 |
|a Water
|2 NLM
|
| 650 |
|
7 |
|a 059QF0KO0R
|2 NLM
|
| 650 |
|
7 |
|a Oxygen Isotopes
|2 NLM
|
| 700 |
1 |
|
|a Cernusak, Lucas A
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Nelson, Daniel B
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Lehmann, Marco M
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Tcherkez, Guillaume
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Kahmen, Ansgar
|e verfasserin
|4 aut
|
| 773 |
0 |
8 |
|i Enthalten in
|t The New phytologist
|d 1979
|g 240(2023), 5 vom: 07. Dez., Seite 1758-1773
|w (DE-627)NLM09818248X
|x 1469-8137
|7 nnns
|
| 773 |
1 |
8 |
|g volume:240
|g year:2023
|g number:5
|g day:07
|g month:12
|g pages:1758-1773
|
| 856 |
4 |
0 |
|u http://dx.doi.org/10.1111/nph.19248
|3 Volltext
|
| 912 |
|
|
|a GBV_USEFLAG_A
|
| 912 |
|
|
|a SYSFLAG_A
|
| 912 |
|
|
|a GBV_NLM
|
| 912 |
|
|
|a GBV_ILN_350
|
| 951 |
|
|
|a AR
|
| 952 |
|
|
|d 240
|j 2023
|e 5
|b 07
|c 12
|h 1758-1773
|