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12C/13C in cellulose and lignin as palaeothermometers

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Outgoing claims: the papers this work cites, builds on, or argues with.

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Depletion of Carbon-13 in Young Kauri Tree
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Climatic implications of stable carbon isotopes in tree rings
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Seasonal Variation in the Ultrastructure of the Cambium in New Zealand Grown Pinus radiata D. Don
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Tree Rings and Climate
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The Concentration and Isotopic Abundances of Carbon Dioxide in the Atmosphere

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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An Improved Method for Extraction of Α-Cellulose from Fossil Wood and its Paleoclimate Implications
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A rapid and simple method to isolate pure alpha-cellulose
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Cosmic ray event in 994 C.E. recorded in radiocarbon from Danish oak
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Post‐photosynthetic fractionation of stable carbon isotopes between plant organs—a widespread phenomenon
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Stable isotope analysis of safety matches using isotope ratio mass spectrometry–a forensic case study
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Carbon, hydrogen and oxygen stable isotope ratios of whole wood, cellulose and lignin methoxyl groups of Picea abies as climate proxies
inferred← citeshttps://doi.org/10.1002/rcm.7388openalex-snapshot
Comparison of δ 18 O and δ 13 C values between tree‐ring whole wood and cellulose in five species growing under two different site conditions
inferred← citeshttps://doi.org/10.1002/rcm.7995openalex-snapshot
Evaluating climate signal recorded in tree‐ring δ 13 C and δ 18 O values from bulk wood and α‐cellulose for six species across four sites in the northeastern US
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ISOTOPES IN TREE RINGS
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Climate Signals in Stable Isotope Tree-Ring Records
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Anatomical, Developmental and Physiological Bases of Tree-Ring Formation in Relation to Environmental Factors
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Stable Isotope Signatures of Wood, its Constituents and Methods of Cellulose Extraction
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Integrating dendroecology with other disciplines improves understanding of upper and latitudinal treelines
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δ13C of Tree-Ring Lignin as an Indirect Measure of Climate Change
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13C discrimination by fossil leaves during the late-glacial climate oscillation 12-10 ka BP: measurements and physiological controls
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inferred← citeshttps://doi.org/10.1007/s11430-007-0043-7openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s11707-025-1153-2openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s12665-014-3960-8openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s13369-020-04629-wopenalex-snapshot
Climate-Sensitivity Comparisons for Whole Wood, Holocellulose, and α-Cellulose Carbon Isotope Series in Masson Pine
inferred← citeshttps://doi.org/10.1016/0009-2541(91)90069-4openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/0009-2541(92)90006-qopenalex-snapshot
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inferred← citeshttps://doi.org/10.1016/0009-2541(95)00097-6openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/0012-821x(79)90032-3openalex-snapshot
13C/12C ratio variations in Pinus longaeva (bristlecone pine) cellulose during the last millennium
inferred← citeshttps://doi.org/10.1016/0012-821x(83)90031-6openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/0016-7037(81)90046-6openalex-snapshot
Hydrogen and carbon isotopes of petroleum and related organic matter
inferred← citeshttps://doi.org/10.1016/0016-7037(87)90323-1openalex-snapshot
The effects of early diagenesis on the chemical and stable carbon isotopic composition of wood
inferred← citeshttps://doi.org/10.1016/0016-7037(95)00152-2openalex-snapshot
Carbon isotopes of trees from arid environments and implications for reconstructing atmospheric CO2 concentration
inferred← citeshttps://doi.org/10.1016/0016-7037(95)00401-7openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/0020-7381(78)80096-5openalex-snapshot
A suggested procedure for calculating measured uncorrected δ values for high precision mass spectrometric analysis
inferred← citeshttps://doi.org/10.1016/0031-0182(94)90096-5openalex-snapshot
Stable isotopes of nitrogen and carbon of North American white-tailed deer and implications for paleodietary and other food web studies
inferred← citeshttps://doi.org/10.1016/0168-9622(91)90033-sopenalex-snapshot
Seasonal stable-carbon isotope variability in tree rings: possible paleoenvironmental signals
inferred← citeshttps://doi.org/10.1016/0198-0149(81)90034-0openalex-snapshot
Anatomy of a cyclonic ring in the drake passage
inferred← citeshttps://doi.org/10.1016/0277-3791(85)90017-4openalex-snapshot
A review of various factors influencing the stable carbon isotope ratio of organic lake sediments by the change from glacial to post-glacial environmental conditions
inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.01224-9openalex-snapshot
Stable Isotopes in Forensics Applications
inferred← citeshttps://doi.org/10.1016/b978-0-444-81546-0.50029-xopenalex-snapshot
Isotopes as Indicators of Environmental Change
inferred← citeshttps://doi.org/10.1016/b978-044451114-0/50053-3openalex-snapshot
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A Novel Cellulose-Preparation Method
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BATCH PROCESSING OF TREE-RING SAMPLES FOR RADIOCARBON ANALYSIS
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14C PREPARATION PROTOCOLS FOR ARCHAEOLOGICAL SAMPLES AT THE LMC14, SACLAY, FRANCE
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Possibility of Climatically Induced Variations in the 14C and 13C Enrichment Patterns as Recorded by a 300-Year-Old Norwegian Pine
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14C in Extractives from Wood
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Evaluation of Wood Pretreatments on Oak and Cedar
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Seasonal Fluctuation of Stable Carbon Isotopic Composition in Japanese Cypress Tree Rings from the Last Glacial Period–Possibility of Paleoenvironment Reconstruction
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δ13C of Tree-Ring Lignin as an Indirect Measure of Climate Change
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Analysis of δ18O in tree rings: Wood‐cellulose comparison and method dependent sensitivity
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Response of central Siberian Scots pine to soil water deficit and long‐term trends in atmospheric CO 2 concentration
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Spatial expression of ENSO, drought, and summer monsoon in seasonal δ13C of ponderosa pine tree rings in southern Arizona and New Mexico
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Isotopic composition ( δ 13 C, δ 18 O) in wood and cellulose of Siberian larch trees for early Medieval and recent periods
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Bond13C/12C ratios reflect (palaeo‐)climatic variations
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High‐resolution δ13C measurements of oak show a previously unobserved spring depletion
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Environmental information from13C/12C Ratios of Wood
inferred← citeshttps://doi.org/10.1029/jd089id07p11731openalex-snapshot
13C/12C ratios in tree rings and the transfer of biospheric carbon to the atmosphere
inferred← citeshttps://doi.org/10.1029/rg017i007p01813openalex-snapshot
Carbon dioxide and climate
inferred← citeshttps://doi.org/10.1034/j.1600-0889.1991.t01-2-00005.xopenalex-snapshot
Stable isotopes in tree ring cellulose and climatic change
inferred← citeshttps://doi.org/10.1034/j.1600-0889.1998.00002.xopenalex-snapshot
Climate variation and the stable carbon isotope composition of tree ring cellulose: an intercomparison of Quercus robur, Fagus sylvatica and Pinus silvestris
inferred← citeshttps://doi.org/10.1038/271093a0openalex-snapshot
Climatic interpretation of δ18O and δD in tree rings (reply)
inferred← citeshttps://doi.org/10.1038/271234a0openalex-snapshot
Chemical pretreatment and radial flow of 14C in tree rings
inferred← citeshttps://doi.org/10.1038/273040a0openalex-snapshot
Pioneer agriculture explosion and CO2 levels in the atmosphere
inferred← citeshttps://doi.org/10.1038/276334a0openalex-snapshot
Tree-ring evidence of past climatic variability
inferred← citeshttps://doi.org/10.1038/279229a0openalex-snapshot
Problems in interpreting tree-ring δ 13C records
inferred← citeshttps://doi.org/10.1038/287432a0openalex-snapshot
Carbon-13 in tree-ring cellulose as an indicator of past climates
inferred← citeshttps://doi.org/10.1038/297028a0openalex-snapshot
An explanation of 13C/12C variations in tree rings
inferred← citeshttps://doi.org/10.1038/298742a0openalex-snapshot
Evidence for 13C/12C fractionation between tree leaves and wood
inferred← citeshttps://doi.org/10.1038/s41467-018-07701-0openalex-snapshot
Northern forest tree populations are physiologically maladapted to drought
inferred← citeshttps://doi.org/10.1046/j.0016-8025.2002.00931.xopenalex-snapshot
Seasonal variation in δ13C and δ18O of cellulose from growth rings of Pinus radiata
inferred← citeshttps://doi.org/10.1046/j.1354-1013.2001.00444.xopenalex-snapshot
Changes in wood and foliar δ13C in sugar maple at Gatineau Park, Quebec, Canada
inferred← citeshttps://doi.org/10.1046/j.1365-2435.1998.00230.xopenalex-snapshot
δ 13 C of wood in growth‐rings indicates cambial activity of drought‐stressed trees of Eucalyptus globulus
inferred← citeshttps://doi.org/10.1046/j.1365-3040.1998.00304.xopenalex-snapshot
Changes of tree‐ringδ13C and water‐use efficiency of beech (Fagus sylvaticaL.) in north‐eastern France during the past century
inferred← citeshttps://doi.org/10.1051/forest:2003001openalex-snapshot
The ?13C of Scots pine (Pinus sylvestris L.) needles: spatial and temporal variations
inferred← citeshttps://doi.org/10.1071/fp06228openalex-snapshot
Stable oxygen isotope composition of plant tissue: a review
inferred← citeshttps://doi.org/10.1071/fp07064openalex-snapshot
d13C of organic matter transported from the leaves to the roots in Eucalyptus delegatensis: short-term variations and relation to respired CO2
inferred← citeshttps://doi.org/10.1071/fp08216openalex-snapshot
Why are non-photosynthetic tissues generally 13C enriched compared with leaves in C3 plants? Review and synthesis of current hypotheses
inferred← citeshttps://doi.org/10.1080/03067319508027636openalex-snapshot
Evaluation of Cellulose Extraction Procedures for Stable Carbon Isotope Measurement in Tree Ring Research
inferred← citeshttps://doi.org/10.1080/03680770.1977.11896938openalex-snapshot
Stable carbon isotope study of a 200-m core sample from Lake Biwa
inferred← citeshttps://doi.org/10.1080/03746609609480374openalex-snapshot
Reconstructing Past Environmental Change Using Stable Isotopes in Tree-rings
inferred← citeshttps://doi.org/10.1080/1025601031000102206openalex-snapshot
Potential for assessing long-term dynamics in soil nitrogen availability from variations in δ 15N of tree rings
inferred← citeshttps://doi.org/10.1080/10256010410001671032openalex-snapshot
Stable carbon isotopic composition of tree rings from a pine tree from Augustów Wilderness, Poland, as a temperature and local environment conditions indicator
inferred← citeshttps://doi.org/10.1080/10256016.2015.1056181openalex-snapshot
δ2H, δ13C and δ18O from whole wood,α-cellulose and lignin methoxyl groups inPinus sylvestris: a multi-parameter approach
inferred← citeshttps://doi.org/10.1080/10256016.2016.1161622openalex-snapshot
Comparison of δ13C and δ18O from cellulose, whole wood, and resin-free whole wood from an old high elevation Pinus uncinata in the Spanish central Pyrenees
inferred← citeshttps://doi.org/10.1093/treephys/19.12.831openalex-snapshot
A rapid and simple method for processing wood to crude cellulose for analysis of stable carbon isotopes in tree rings
inferred← citeshttps://doi.org/10.1093/treephys/20.16.1121openalex-snapshot
Stable carbon isotope discrimination: an indicator of cumulative salinity and boron stress in Eucalyptus camaldulensis
inferred← citeshttps://doi.org/10.1093/treephys/25.2.129openalex-snapshot
Environmental and physiological controls over oxygen and carbon isotope composition of Tasmanian blue gum, Eucalyptus globulus
inferred← citeshttps://doi.org/10.1093/treephys/25.6.745openalex-snapshot
Long-term trends in cellulose 13 C and water-use efficiency of tropical Cedrela and Swietenia from Brazil
inferred← citeshttps://doi.org/10.1093/treephys/26.6.767openalex-snapshot
A multi-species comparison of 13C from whole wood, extractive-free wood and holocellulose
inferred← citeshttps://doi.org/10.1093/treephys/28.11.1619openalex-snapshot
Biochemical composition is not the main factor influencing variability in carbon isotope composition of tree rings
inferred← citeshttps://doi.org/10.1093/treephys/tpag073openalex-snapshot
Consistent δ13C offsets between whole wood and α-cellulose of Pinus sylvestris confirmed across contrasting forest stand types and a climatic gradient
inferred← citeshttps://doi.org/10.1093/treephys/tpu064openalex-snapshot
Do tree-ring stable isotope compositions faithfully record tree carbon/water dynamics?
inferred← citeshttps://doi.org/10.1098/rsta.2001.0965openalex-snapshot
The carbon isotope composition of ancient CO 2 based on higher-plant organic matter
inferred← citeshttps://doi.org/10.1111/j.0016-8025.2003.01159.xopenalex-snapshot
Beyond CO 2 ‐fixation by Rubisco – an interpretation of 13 C/ 12 C variations in tree rings from novel intra‐seasonal studies on broad‐leaf trees
inferred← citeshttps://doi.org/10.1111/j.1365-3040.1996.tb00413.xopenalex-snapshot
Carbon isotope fractionation in tree ring early and late wood in relation to intra‐growing season water balance
inferred← citeshttps://doi.org/10.1111/j.1365-3040.2005.01343.xopenalex-snapshot
Temporal photosynthetic carbon isotope signatures revealed in a tree ring through 13CO2 pulse‐labelling
inferred← citeshttps://doi.org/10.1111/j.1365-3040.2009.01989.xopenalex-snapshot
A single‐substrate model to interpret intra‐annual stable isotope signals in tree‐ring cellulose
inferred← citeshttps://doi.org/10.1111/j.1469-185x.1977.tb00838.xopenalex-snapshot
TREE RINGS: A NATURAL DATA‐STORAGE SYSTEM
inferred← citeshttps://doi.org/10.1111/j.1469-8137.2004.00970.xopenalex-snapshot
Intramolecular, compound‐specific, and bulk carbon isotope patterns in C3 and C4 plants: a review and synthesis
inferred← citeshttps://doi.org/10.1111/j.1469-8137.2007.02213.xopenalex-snapshot
Stable hydrogen isotope ratios of lignin methoxyl groups as a paleoclimate proxy and constraint of the geographical origin of wood
inferred← citeshttps://doi.org/10.1111/j.1502-3931.1993.tb01541.xopenalex-snapshot
Carbon isotopic abundances in Mesozoic and Cenozoic fossil plants: Palaeoecological implications
inferred← citeshttps://doi.org/10.1111/j.1502-3931.1998.tb00482.xopenalex-snapshot
Carbon‐isotope analyses of fossil plants as a chemostratigraphic and palaeoenvironmental tool
inferred← citeshttps://doi.org/10.1111/j.1600-0889.2008.00370.xopenalex-snapshot
Climatic significance of tree-ring width and δ13C in a Spanish pine forest network
inferred← citeshttps://doi.org/10.1111/j.2153-3490.1980.tb00954.xopenalex-snapshot
Past atmospheric CO 2 levels and the 13 C/ 12 C ratios in tree rings
inferred← citeshttps://doi.org/10.1111/j.2153-3490.1982.tb01838.xopenalex-snapshot
Carbon isotope records in Wisconsin trees
inferred← citeshttps://doi.org/10.1111/nph.12587openalex-snapshot
UV ‐laser‐based microscopic dissection of tree rings – a novel sampling tool for δ 13 C and δ 18 O studies
inferred← citeshttps://doi.org/10.1111/nph.12741openalex-snapshot
Seasonal transfer of oxygen isotopes from precipitation and soil to the tree ring: source water versus needle water enrichment
inferred← citeshttps://doi.org/10.1111/nph.17094openalex-snapshot
Linking canopy‐scale mesophyll conductance and phloem sugar δ13C using empirical and modelling approaches
inferred← citeshttps://doi.org/10.1111/nph.20170openalex-snapshot
Reconciling water‐use efficiency estimates from carbon isotope discrimination of leaf biomass and tree rings: nonphotosynthetic fractionation matters
inferred← citeshttps://doi.org/10.1111/pce.12196openalex-snapshot
Drivers of radial growth and carbon isotope discrimination of bur oak ( Q uercus macrocarpa M ichx.) across continental gradients in precipitation, vapour pressure deficit and irradiance
inferred← citeshttps://doi.org/10.1111/pce.12383openalex-snapshot
Carbon isotope compositions (δ 13 C) of leaf, wood and holocellulose differ among genotypes of poplar and between previous land uses in a short‐rotation biomass plantation
inferred← citeshttps://doi.org/10.1126/science.199.4326.253openalex-snapshot
Atmospheric Carbon Dioxide and Carbon Reservoir Changes
inferred← citeshttps://doi.org/10.1126/science.206.4417.409openalex-snapshot
Fate of Fossil Fuel Carbon Dioxide and the Global Carbon Budget
inferred← citeshttps://doi.org/10.1130/0091-7613(2002)030<0403:aiserc>2.0.co;2openalex-snapshot
Are industrial SO2 emissions reducing CO2 uptake by the boreal forest?
inferred← citeshttps://doi.org/10.1139/b01-001openalex-snapshot
Population differences in stable carbon isotope ratio of Pinus contorta Dougl. ex Loud.: relationship to environment, climate of origin, and growth potential
inferred← citeshttps://doi.org/10.1139/x09-091openalex-snapshot
Chemical pretreatment of Thuja occidentalis tree rings: implications for dendroisotopic studies
inferred← citeshttps://doi.org/10.1144/jgs2013-127openalex-snapshot
Leaf habit of Late PermianGlossopteristrees from high-palaeolatitude forests
inferred← citeshttps://doi.org/10.1163/22941932-90001619openalex-snapshot
Variations of Wood Anatomy and δ13C Within-Tree Rings of Coastal Pinus Pinaster Showing Intra-Annual Density Fluctuations
inferred← citeshttps://doi.org/10.1177/0144598720950479openalex-snapshot
Effect of peat mire evolution on pore structure characteristics in thick coal seam: Examples from Xishanyao Formation (Middle Jurassic), Yili Basin, China
inferred← citeshttps://doi.org/10.1177/0959683608100569openalex-snapshot
Rainfall control of the δ 13 C ratios of Mimusops caffra from KwaZulu-Natal, South Africa
inferred← citeshttps://doi.org/10.1177/0959683609350389openalex-snapshot
Sphagnum δ13C values as indicators of palaeohydrological changes in a peat bog
inferred← citeshttps://doi.org/10.1177/0959683614561888openalex-snapshot
Mid- to late-Holocene East Asian summer monsoon variability recorded in lacustrine sediments from Jingpo Lake, Northeastern China
inferred← citeshttps://doi.org/10.1177/095968369500500408openalex-snapshot
High-resolution stable isotope analysis of tree rings: implications of 'microdendroclimatology' for palaeoenvironmental research
inferred← citeshttps://doi.org/10.1186/s13595-024-01247-6openalex-snapshot
Do leaf lignin content or leaf mass-to-area bias the estimation of intrinsic water use efficiency from leaf bulk δ13C? A test with seedlings from five oak species
inferred← citeshttps://doi.org/10.1191/095968301680223477openalex-snapshot
Stable carbon isotope ratios of Pinus sylvestris from northern Finland and the potential for extracting a climate signal from long Fennoscandian chronologies
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