Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Wüthrich, Lorenz; Brändli, Claudio; Braucher, Régis; Veit, Heinz; Haghipour, Negar; Terrizzano, Carla; Christl, Marcus; Gnägi, Christian; Zech, Roland (2017): Beryllium 10 (10Be) concentrations from till in the western Swiss lowlands [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.884060, Supplement to: Wüthrich, L et al. (2017): 10Be depth profiles in glacial sediments on the Swiss Plateau: deposition age, denudation and (pseudo-) inheritance. E&G - Eiszeitalter und Gegenwart - Quaternary Science Journal, 66(2), 57-68, https://doi.org/10.5194/egqsj-66-57-2017

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
During the Pleistocene, glaciers advanced repeatedly from the Alps onto the Swiss Plateau. Numeric age control for the last glaciation is good and thus the area is well suited to test a method which has so far not been applied to till in Switzerland. In this study, we apply in situ produced cosmogenic 10Be depth profile dating to several till deposits. Three sites lie inside the assumed Last Glacial Maximum (LGM) extent of the Rhône and Aare glaciers (Bern, Deisswil, Steinhof) and two lie outside (Niederbuchsiten, St. Urban). All sites are strongly affected by denudation, and all sites have reached steady state, i.e., the 10Be production is in equilibrium with radioactive decay and denudational losses. Deposition ages can therefore not be well constrained. Assuming constant denudation rates of 5 cm/kyr, total denudation on the order of 100 cm for sites within the extent of the LGM and up to tens of meters for older moraines are calculated. Denudation events, for example related to periglacial conditions during the LGM, mitigate the need to invoke such massive denudation and could help to explain high 10Be concentrations at great depths, which we here dub "pseudo-inheritance". This term should be used to distinguish conceptionally from "true inheritance", i.e., high concentrations derived from the catchment.
Coverage:
Median Latitude: 47.121400 * Median Longitude: 7.645000 * South-bound Latitude: 46.922000 * West-bound Longitude: 7.453000 * North-bound Latitude: 47.286000 * East-bound Longitude: 7.855000
Minimum DEPTH, sediment/rock: 0.100 m * Maximum DEPTH, sediment/rock: 3.800 m
Event(s):
Deisswil * Latitude: 47.034000 * Longitude: 7.465000 * Elevation: 574.0 m * Location: Switzerland * Method/Device: Rock sample (ROCK)
Gurten * Latitude: 46.922000 * Longitude: 7.453000 * Elevation: 654.0 m * Location: Switzerland * Method/Device: Rock sample (ROCK)
Niederbuchsiten * Latitude: 47.286000 * Longitude: 7.770000 * Elevation: 483.0 m * Location: Switzerland * Method/Device: Rock sample (ROCK)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventWüthrich, Lorenz
2Latitude of eventLatitudeWüthrich, Lorenz
3Longitude of eventLongitudeWüthrich, Lorenz
4Elevation of eventElevationmWüthrich, Lorenz
5Sample code/labelSample labelWüthrich, Lorenz
6Beryllium-10, production rate per year10Be prodatoms/g/aWüthrich, Lorenz
7DEPTH, sediment/rockDepth sedmWüthrich, LorenzGeocode
8Mass per areaMassg/cm2Wüthrich, Lorenzdensity is 2.2 g/cm**3
9Quartz, dissolvedQz dissgWüthrich, Lorenz
10CarrierCarrierWüthrich, Lorenz9Be carrier added [mg]
11Beryllium-10/Beryllium-910Be/9Be10-9 atoms/atomsWüthrich, Lorenz
12Beryllium-10/Beryllium-9, standard deviation10Be/9Be std dev±Wüthrich, Lorenz
13Beryllium-1010Be109 atoms/gWüthrich, Lorenz
14Beryllium-10, standard deviation10Be std dev±Wüthrich, Lorenz
Size:
181 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML