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@ARTICLE{Moschen:3791,
author = {Moschen, R. and Lücke, A. and Parplies, J. and Schleser,
G. H.},
title = {{C}ontrols on the seasonal and interannual dynamics of
organic matter carbon isotopes in mesotrophic {L}ake
{H}olzmaar, {G}ermany},
journal = {Limnology and oceanography / Methods},
volume = {54},
issn = {1541-5856},
address = {Waco, Tex.},
publisher = {ASLO},
reportid = {PreJuSER-3791},
pages = {194 - 209},
year = {2009},
note = {This work was supported by a postdoctoral fellowship to
Robert Moschen and a Ph. D. grant to Jorn Parplies from
Forschungszentrum Julich. Additional financial support was
provided by the Federal Ministry of Education and Research
through the German Climate Research Program (DEKLIM, grant
01LD0001) and the project "Climate in Historical Times
KIHZ."},
abstract = {We investigated the particulate organic matter (POM) flux
and its stable carbon isotope composition in response to
changes in phytoplankton primary production and abiotic
environmental affects in mesotrophic Lake Holzmaar. POM
fluxes were determined by sediment traps emptied biweekly
from 1995 to 2004. Water chemical measurements and
meteorological observations were done concurrently. POM
fluxes within and directly below the lake's epilimnion were
relatively low during winter (<0.5 g m(-2) d(-1)) and
increased to 1.0-1.5 g m(-2) d(-1) during summer months
because of enlarged phytoplankton production. In contrast,
in the lake's hypolimnion a much higher POM flux was
observed during winter as result of resuspension of
particulate material from the lake's bottom. C:N (weight,
total organic carbon : total nitrogen) ratios of settling
organic matter vary around 8 at all three depths, indicating
a predominant phytoplankton origin of POM. The annual
epilimnic POM flux correlates with the epilimnic phosphate
concentration early in the seasonal cycle, indicating that
the supply of phosphate is the major control on the amount
of algal biomass. A recurrent annual oscillation of the
stable carbon isotope composition of POM with low delta C-13
values during winter and more positive values during summer
is interpreted as the result of phytoplankton primary
production. A close delta C-13(POM)-POM flux relationship
was observed, testifying to the primary dependence of delta
C-13(POM) on lacustrine primary production. Contrary to POM
flux, the epilimnic delta C-13(POM) signal is transferred to
the lakes bottom notwithstanding sediment resuspension and
microbial alteration. Our results demonstrate that
sedimentary stable carbon isotopes are a valuable proxy for
lacustrine paleo-productivity in Lake Holzmaar.},
keywords = {J (WoSType)},
cin = {ICG-4},
ddc = {550},
cid = {I:(DE-Juel1)VDB793},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Limnology / Oceanography},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000265168800016},
doi = {10.4319/lo.2009.54.1.0194},
url = {https://juser.fz-juelich.de/record/3791},
}