The biosphere: A homogeniser of Pb-isotope signals

Author(s)
Clemens Reimann, Belinda Flem, Arnold Arnoldussen, Peter Englmaier, Tor Erik Finne, Friedrich Koller, Friedrich Koller, Øystein Nordgulen
Abstract

Rock, soil, and plant (terrestrial moss, European mountain ash leaves, mountain birch leaves, bark and wood, and spruce needles and wood) samples, collected at 3 km intervals along a 120 km long transect (40 sites) cutting the city of Oslo, Norway, were analysed for their Pb concentration and Pb-isotope ratios. A general decrease in 206Pb/207Pb, 208Pb/207Pb and 206Pb/208Pb ratios, with a characteristic low variability in all plant materials and the plant-derived O-horizon of soil profiles, compared to rocks and mineral soils, is observed along the transect. It is demonstrated that minerogenic and biogenic sample materials belong to two different spheres, the lithosphere and biosphere, and that geochemical processes determining their chemical and isotopic compositions differ widely. Background variation for both sample materials needs to be established and documented at the continental and global scale before the anthropogenic influence on the geochemistry of the earth's surface can be reliably estimated

Organisation(s)
Department of Lithospheric Research
External organisation(s)
Geological Survey of Norway, Norwegian Forest and Landscape Institute
Journal
Applied Geochemistry
Volume
23
Pages
705-722
No. of pages
18
ISSN
0883-2927
Publication date
2008
Peer reviewed
Yes
Austrian Fields of Science 2012
1060 Biology, 105105 Geochemistry
Sustainable Development Goals
SDG 15 - Life on Land
Portal url
https://ucrisportal.univie.ac.at/en/publications/34855d9f-a8a5-4b42-8789-c5d092c52719