Related Content
Search Google Scholar for:
More Information
Related Jobs from ScienceCareers
|
|
Science 11 September 1998: Vol. 281. no. 5383, pp. 1635 - 1640 DOI: 10.1126/science.281.5383.1635
|
|
Research Articles
History of Atmospheric Lead Deposition Since 12,370 14C yr BP from a Peat Bog, Jura Mountains, Switzerland
W. Shotyk,
*
D. Weiss,
P. G. Appleby,
A. K. Cheburkin,
R. Frei,
M. Gloor,
J. D. Kramers,
S. Reese,
W. O. Van Der Knaap
A continuous record of atmospheric lead since 12,370 carbon-14
years before the present (14C yr BP) is preserved in a
Swiss peat bog. Enhanced fluxes caused by climate changes reached their
maxima 10,590 14C yr BP (Younger Dryas) and 8230 14C yr BP. Soil erosion caused by forest clearing and
agricultural tillage increased lead deposition after 5320 14C yr BP. Increasing lead/scandium and decreasing
lead-206/lead-207 beginning 3000 14C yr BP indicate the
beginning of lead pollution from mining and smelting, and anthropogenic
sources have dominated lead emissions ever since. The greatest lead
flux (15.7 milligrams per square meter per year in A.D. 1979) was 1570 times the natural, background value (0.01 milligram per square meter
per year from 8030 to 5320 14C yr BP).
W. Shotyk and D. Weiss are at the Geological Institute, University
of Berne, Baltzerstrasse 1, CH-3012 Berne, Switzerland. P. G. Appleby is in the Environmental Radiometric Research Centre, Department
of Mathematical Sciences, University of Liverpool, Post Office Box 147, Liverpool, L69 3BX, UK. A. K. Cheburkin is at the Geological
Institute, Ukrainian Academy of Sciences, Gonhkar Street 55b, Kiev 54, 252054, Ukraine. R. Frei is at the Geologisk Institut, Kobenhavns
Universitet, Oster Voldgade 10, DK-1350 Copenhagen, Denmark. M. Gloor
is with the Swiss Federal Research Institute for Forestry, Snow, and
Landscape Research, Zürcherstrasse 111, CH-8903 Birmensdorf,
Switzerland. J. D. Kramers is in the Isotope Geology Group,
Mineralogical-Petrographical Institute, University of Berne,
Erlachstrasse 9a, CH-3012 Berne, Switzerland. S. Reese is at the
Radiocarbon Laboratory, Physics Institute, University of Berne,
Sidlerstrasse 5, CH-3012 Berne, Switzerland. W. O. Van Der Knaap
is at the Institute of Geobotany, University of Berne, Altenbergrain
21, CH-3013 Berne, Switzerland.
*
To whom correspondence should be addressed. E-mail:
shotyk{at}geo.unibe.ch
Present address: EMMA Analytical, Elmvale, Ontario L0L 1P0,
Canada.
Read the Full Text
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
- Multiproxy evidence of `Little Ice Age' palaeoenvironmental changes in a peat bog from northern Poland.
- F. De Vleeschouwer, N. Piotrowska, J. Sikorski, J. Pawlyta, A. Cheburkin, G. Le Roux, M. Lamentowicz, N. Fagel, and D. Mauquoy (2009)
The Holocene
19, 625-637
| Abstract »
| PDF »
- Investigations on buried soils and colluvial layers around Bronze Age burial mounds at Bornhoved (northern Germany): an approach to test the hypothesis of `landscape openness' by the incidence of colluviation.
- S. Dreibrodt, O. Nelle, I. Lutjens, A. Mitusov, I. Clausen, and H.-R. Bork (2009)
The Holocene
19, 487-497
| Abstract »
| PDF »
- A record of anthropogenic Pb deposition in a Mediterranean karst catchment (Lake Vrana, Cres Island, Croatia).
- S. Miko, S. Mesic, M. S. Miko, and O. Hasan (2008)
Mineralogical Magazine
72, 455-460
| Abstract »
| Full Text »
| PDF »
- Influence of lead smelter emissions on the distribution of metals in marine sediments from Chaleur Bay, eastern Canada.
- M. B. Parsons and R. E. Cranston (2006)
Geochemistry: Exploration, Environment, Analysis
6, 259-275
| Abstract »
| Full Text »
| PDF »
- Postnatal Inorganic Lead Exposure Reduces Midbrain Dopaminergic Impulse Flow and Decreases Dopamine D1 Receptor Sensitivity in Nucleus Accumbens Neurons.
- M. Tavakoli-Nezhad and D. K. Pitts (2005)
J. Pharmacol. Exp. Ther.
312, 1280-1288
| Abstract »
| Full Text »
| PDF »
- Holocene environmental change: contributions from the peatland archive.
- F. M. Chambers, F. M. Chambers, and D. J. Charman (2004)
The Holocene
14, 1-6
| Abstract »
| PDF »
- The late-Holocene history of Gormire Lake (NE England) and its catchment: a multiproxy reconstruction of past human impact.
- F. Oldfield, R. Wake, J. Boyle, R. Jones, S. Nolan, Z. Gibbs, P. Appleby, E. Fisher, and G. Wolff (2003)
The Holocene
13, 677-690
| Abstract »
| PDF »
- Book Review: Tracers in geomorphology.
- R. A. Sutherland (2001)
Progress in Physical Geography
25, 574-577
| PDF »
- The palaeoecological history of the Praz-Rodet bog (Swiss Jura) based on pollen, plant macrofossils and testate amoebae (Protozoa).
- E. A. D. Mitchell, E. A.D. Mitchell, W. O. van der Knaap, J. F.N. van Leeuwen, A. Buttler, B. G. Warner, and J.-M. Gobat (2001)
The Holocene
11, 65-80
| Abstract »
| PDF »
- New isotopic evidence for chronic lead contamination in the San Francisco Bay estuary system: Implications for the persistence of past industrial lead emissions in the biosphere.
- D. J. Steding, C. E. Dunlap, and A. R. Flegal (2000)
PNAS
| Abstract »
| Full Text »
- Mineral surfaces and bioavailability of heavy metals: A molecular-scale perspective.
- G. E. Brown Jr., A. L. Foster, and J. D. Ostergren (1999)
PNAS
96, 3388-3395
| Abstract »
| Full Text »
| PDF »
- From the Cover: New isotopic evidence for chronic lead contamination in the San Francisco Bay estuary system: Implications for the persistence of past industrial lead emissions in the biosphere.
- D. J. Steding, C. E. Dunlap, and A. R. Flegal (2000)
PNAS
97, 11181-11186
| Abstract »
| Full Text »
| PDF »
|
|