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@ARTICLE{Heyng:21990,
author = {Heyng, A.M. and Mayr, C. and Lücke, A. and Striewski, B.
and Wastegard, S. and Wissel, H.},
title = {{E}nvironmental changes in northern {N}ew {Z}ealand since
the {M}iddle {H}olocene inferred from stable isotope records
(d15{N}, d13{C}) of {L}ake {P}upuke},
journal = {Journal of paleolimnology},
volume = {48},
issn = {0921-2728},
address = {Dordrecht [u.a.]},
publisher = {Springer Science + Business Media B.V},
reportid = {PreJuSER-21990},
pages = {351 - 366},
year = {2012},
note = {We thank Gillian Turner and Jim Neale for coring, Markus
Oehlerich and Laurentius Sauer for assistance in the isotope
lab, Alexander Altenbach for discussions. Thomas Stephens,
an anonymous reviewer and the editors Thomas Whitmore and
Steffen Mischke provided useful comments on an earlier
version of this manuscript. Funding to AL and CM by the
German Research Foundation (grant nos. MA 4235/1-1 and LU
786/5-1) is gratefully acknowledged.},
abstract = {Maar lakes in the Auckland Volcanic Field are important
high-resolution archives of Holocene environmental change in
the Southern Hemisphere mid-latitudes. Stable carbon and
nitrogen isotope analyses were applied on bulk organic
matter and the green alga Botryococcus from a sediment core
from Lake Pupuke (Auckland, North Island, New Zealand)
spanning the period since 7,165 cal. year BP. The origin of
organic matter was established using
total-organic-carbon-to-nitrogen ratios (TOC/TN) as well as
organic carbon (delta C-13(OM)) and nitrogen (delta N-15)
isotope composition of potential modern sources. This
approach demonstrated that the contribution of allochthonous
organic matter to the lake sediment was negligible for most
of the record. The sedimentary TOC/TN ratios that are higher
than Redfield ratio (i.e. > 7) are attributed to N-limiting
conditions throughout the record. Variations of nitrogen and
carbon isotopes during the last 7,165 years are interpreted
as changes in the dominant processes in the lake. While
epilimnetic primary productivity controlled isotope
composition before 6,600 cal. year BP, microbial processes,
especially denitrification and methane oxidation, caused
overall shifts of the delta N-15 and delta C-13 values since
the Mid-Holocene. Comparisons with climate reconstructions
from the Northern Island suggest that changes in the
wind-induced lake overturn and a shift to more pronounced
seasonality were the most likely causes for lake-internal
changes since 6,600 cal. year BP.},
keywords = {J (WoSType)},
cin = {IBG-3},
ddc = {930},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Environmental Sciences / Geosciences, Multidisciplinary /
Limnology},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000305959000006},
doi = {10.1007/s10933-012-9606-5},
url = {https://juser.fz-juelich.de/record/21990},
}