Guido Wiesenberg
www.geo.uzh.ch
0000-0003-2738-5775
Universitat Zurich
47 papers found
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Erratum to “Carbonate rhizoliths in loess and their implications for paleoenvironmental reconstruction revealed by isotopic composition: δ13C, 14C” [Chemical Geology 283 (2011) 251–260]
Branched tetraether membrane lipids associated with rhizoliths in loess: Rhizomicrobial overprinting of initial biomarker record
Cold hardiness of Pinus nigra Arnold as influenced by geographic origin, warming, and extreme summer drought
Carbonate rhizoliths in loess and their implications for paleoenvironmental reconstruction revealed by isotopic composition: δ13C, 14C
C and N in soil organic matter density fractions under elevated atmospheric CO2: Turnover vs. stabilization
Differentiation of plant derived organic matter in soil, loess and rhizoliths based on n-alkane molecular proxies
Comparison of free lipid compositions between roots and leaves of plants in the Dajiuhu Peatland, central China
Rhizoliths in loess – evidence for post-sedimentary incorporation of root-derived organic matter in terrestrial sediments as assessed from molecular proxies
Fast incorporation of root-derived lipids and fatty acids into soil – Evidence from a short term multiple pulse labelling experiment
Reconstructing Quaternary vegetation history in the Carpathian Basin, SE-Europe, using n-alkane biomarkers as molecular fossils
Is there a possibility to correct fossil n-alkane data for postsedimentary alteration effects?
Carbon isotopic composition of branched tetraether membrane lipids in soils suggest a rapid turnover and a heterotrophic life style of their source organism(s)
Source determination of lipids in bulk soil and soil density fractions after four years of wheat cropping
Optimization of 14C liquid scintillation counting of plant and soil lipids to trace short term formation, translocation and degradation of lipids
Short-chain n-alkanes (C16–20) in ancient soil are useful molecular markers for prehistoric biomass burning
Thermal degradation of rye and maize straw: Lipid pattern changes as a function of temperature
Plant and soil lipid modifications under elevated atmospheric CO2 conditions: I. Lipid distribution patterns
Storage and stability of organic matter and fossil carbon in a Luvisol and Phaeozem with continuous maize cropping: A synthesis
Plant and soil lipid modification under elevated atmospheric CO2 conditions: II. Stable carbon isotopic values (δ13C) and turnover
How relevant is recalcitrance for the stabilization of organic matter in soils?
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