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@ARTICLE{Schleser:189597,
author = {Schleser, Gerhard, Hans and Anhuf, D. and Helle, G. and
Vos, Heinz},
title = {{A} remarkable relationship of the stable carbon isotopic
compositions of wood and cellulose in tree-rings of the
ropical speices {C}ariniana micrantha ({D}ucke) from
{B}razil},
journal = {Chemical geology / Isotope geoscience section},
volume = {401},
issn = {0168-9622},
address = {Amsterdam [u.a.]},
publisher = {Elsevier},
reportid = {FZJ-2015-02735},
pages = {59-66},
year = {2015},
abstract = {The stable isotopes of carbon were analysed in total wood
and cellulose from the tree-rings of the tropical wood
species Cariniana micrantha (Ducke). The aim was to examine
the isotopic relationship between total wood and its
cellulose over the last two and a half centuries. Although
the correlation for the whole time period is very high (r =
0.96) it is remarkable that different sub-periods deviate
strongly from this close relationship. Consequently, a good
correlation from the subset of a longer isotopic record
cannot necessarily prove its validity for the whole record.
The study indicates that changes of the carbon isotopes of
cellulose and of total wood show sometimes during short
sub-periods different isotope patterns presumably caused by
different environmental effects. Thorough calculations
indicate that strong variations within the isotopic record
especially changes of the isotopic level along a chronology
lead to high correlations between δ13Cwood and δ13Ccel.
Contrary thereto subsections with low isotopic variability
lead to low correlations. The results imply that long term
trends provide similar patterns. Therefore, if long term
trends are of interest such as e.g. in climate
reconstruction then total wood can be analysed in favour of
cellulose, thus saving a tremendous amount of work. However,
if short term aspects from a longer record are of interest,
cellulose and total wood may sometimes provide different
information. In addition it is hypothesized that during
intervals of low isotopic variability the proportions of the
various wood components may change relative to each other,
leading for certain time intervals to different isotope
patterns.},
cin = {IBG-3 / IEK-7},
ddc = {540},
cid = {I:(DE-Juel1)IBG-3-20101118 / I:(DE-Juel1)IEK-7-20101013},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255) / 255 - Terrestrial Systems: From Observation to
Prediction (POF3-255)},
pid = {G:(DE-HGF)POF3-255 / G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000352086900005},
doi = {10.1016/j.chemgeo.2015.02.014},
url = {https://juser.fz-juelich.de/record/189597},
}