% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{Dutta:6219,
author = {Dutta, S. and Hartkopf-Fröder, C. and Mann, U. and Wilkes,
H. and Brocke, R. and Bertram, N.},
title = {{M}acromolecular composition of {P}alaeozoic scolecodonts:
insights into the molecular taphonomy of zoomorphs},
journal = {Lethaia},
volume = {43},
issn = {0024-1164},
address = {Oxford [u.a.]},
publisher = {Wiley-Blackwell},
reportid = {PreJuSER-6219},
pages = {334 - 343},
year = {2010},
note = {We would like to thank Forschungszentrum Julich for
financial support. SD is grateful to IIT Bombay for
providing infrastructural facilities. Mrs K. Witte (Aachen
University of Applied Sciences, Germany) is acknowledged for
providing access to the micro-FTIR instrument. The authors
are grateful to Mats Eriksson and an anonymous reviewer for
valuable comments. We gratefully acknowledge Richard M.
Fuchs (Harrison, OH, USA), Axel Munnecke (GeoZentrum
Nordbayern, Germany) and Jan Bohaty (University of Cologne,
Germany) for providing the samples from the Upper Ordovician
of Ohio, the Silurian of Gotland and from the Devonian of
the Eifel Mountains respectively.},
abstract = {Biogeochemistry and molecular taphonomy of biopolymers of
marine zoomorphs are poorly known. In order to obtain
insights into this issue we report on the
biogeomacromolecular composition of hand-picked,
well-preserved scolecodonts of Ordovician, Silurian and
Devonian age using micro-Fourier transform infrared
(micro-FTIR) spectroscopy, Curie point pyrolysis-gas
chromatography-mass spectrometry (Cupy-GC-MS) and
tetramethylammonium hydroxide (TMAH)-assisted
thermochemolysis-GC-MS. The present study reveals that
scolecodonts are composed of both aliphatic and aromatic
moieties. The micro-FTIR spectra of scolecodonts are
characterized by aliphatic CHx (3000–2800 and
1460–1450/cm) and CH3 (1375/cm) absorptions and aromatic
C=C (1560–1610/cm) and CH (3050/cm and 700–900/cm)
absorptions. The major pyrolysis products from the
scolecodonts include aromatic hydrocarbons such as
alkylbenzenes, alkylnaphthalenes and alkylphenols. Aliphatic
hydrocarbons are represented by a homologous series of
n-alkenes and n-alkanes. The compounds released upon
thermochemolysis with TMAH are saturated and unsaturated
fatty acids (as their methyl esters), n-alkenes/alkanes and
aromatic acids (as their methyl esters). No protein/amino
acid-derived compounds have been recognized in the
pyrolysates or in the thermochemolysates, and it is
concluded that protein/amino acid-related compounds, which
are commonly found in the jaws of extant polychaetes, were
destroyed due to diagenetic processes. Obviously, excellent
morphological preservation and low thermal alteration are
not paralleled by a similar degree of chemical preservation.
□Biogeomacromolecules, micro-FTIR, pyrolysis-GC-MS,
scolecodonts, thermochemolysis-GC-MS.},
cin = {ICG-4},
ddc = {550},
cid = {I:(DE-Juel1)VDB793},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Paleontology},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000281200500005},
doi = {10.1111/j.1502-3931.2009.00193.x},
url = {https://juser.fz-juelich.de/record/6219},
}