Publications
Contact: Holger Lueschen, Institut
für
Chemie und Biologie des Meeres, 26111 Oldenburg, Germany
e-mail:
h.lueschen@icbm.de
- L. Neretin, M.E.
Böttcher, B. B. Jorgensen, I. Volkov, H. Lüschen und
Hilgenfeldt, K. (2004), Pyritization processes and greigite formation
in the advancing sulfidization front in the upper Pleistocene sediments
of the Black Sea, Geochimica Cosmochimica Acta, 68, 2081-2093
- B. B. Jorgensen, M.E. Böttcher, H. Lüschen, L. Neretin,
I. Volkov (2004), Anaerobic methane oxidation and a deep H2S sink
generate isotopically heavy sulfides in Black Sea sediments, Geochimica Cosmochimica Acta, 68, 2095-2118
-
H.Lüschen, B.Schnetger, H.-J.Brumsack,
J.Paul
(2000), Haupt- und Spurenelementsignaturen des paläozoischen
Kupferschiefers
und der Exshaw Formation, Terra Nostra 2000/2, Potsdam, 73-75
Abstract: This paper presents a comparison of
minor-element enrichmentfactors of some ancinet and recent "black shales
see also: Poster
presentation 4. Geochemie Tagung, Potsdam (PDF).
- M.E. Böttcher, B.B. Jorgensen, L.Neretin, H. Lüschen,
K. Däumler, H.-J. Brumsack (2000), Authigene Mineralbildung
in Sedimenten des
Schwarzen Meeres: Ein natürliches Transportexperiment und die
geochemischen
Konsequenzen für den sedimentären Rekord, DMG-Tagungsband
2000,
Heidelberg
- H. Lüschen, B. Schnetger,H.-J. Brumsack, J. Paul
(2000); Trace Element
Distribution in Palaeozoic Black Shales: "Kupferschiefer" (Germany) and
Exshaw Formation (Canada), Journal of Conference Abstracts Volume 5(2),
Goldschmidt 2000, 656 Download
(PDF)
- L. Neretin, M.E. Böttcher, B.B.
Jörgensen,
I.I. Volkov, H. Lüschen (1999), Pyritazation at the Holocene /
Late
Pleistocene transition in the Black Sea sediments: Sulfur species and
their
isotopic composition,
Geochemistry of the Earth´s Surface,
Balkema, Rotterdam, 331-334
Abstract: This paper presents the
high-resolution
data on sulfur compounds distribution and their isotopic composition
for
a gravity core from the western part of the Black Sea. Pyritazation
processes
in the uppper part of lake beds is considered in detail and potential
sources
of hydrogen sulfide are discussed. The pyrite sulfur isotope
composition
is used as an indicator of paleoconditions in the basin during
Late-Quaternary
time.
Download introduction and summary of my diploma
thesis (PDF)
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