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10Be concentrations from lake Meerfelder Maar during the earliest part of the...
The samples were measured by AMS at Uppsala University.The sample for 11,201 years BP broke in the centrifuge resulting in no measurement. -
Beryllium 10 (10Be) concentrations from till in the western Swiss lowlands
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... -
Intercomparison of 10Be measurements by decay and Accelerator mass spectromet...
Cosmogenic beryllium-10 activities have been measured in marine accumulations of up to about 6 m.y age by conventional beta counting technique and by accelerator mass... -
Al and Be isotope composition of two ferromanganese crusts from the Pacific O...
The technique of accelerator mass spectrometry (A.H.S.) has opened up a number of new potential geochronological applications of long lived cosmogenic nuclei- However the... -
High-resolution 10Be concentrations in the EDC96 ice core
A new, decadally resolved record of the 10Be peak at 41 kyr from the EPICA Dome C ice core (Antarctica) is used to match it with the same peak in the GRIP ice core (Greenland).... -
10Be measured on Akademii Nauk ice core, Russian Arctic, for the period 1590-...
Global variations of the radionuclide 10Be that are almost simultaneous provide a powerful tool to synchronize 10Be records from different locations. We compared the 10Be record... -
Beryllium-10 concentration in the EPICA Dome C core between 2384.36 and 2626....
Ice cores are exceptional archives which allow us to reconstruct a wealth of climatic parameters as well as past atmospheric composition over the last 800 kyr in Antarctica.... -
(Table 1, page 418) 10Be measurements inside a ferromanganese crust of the At...
The growth rate of a manganese nodule from the South Atlantic Ocean (Rio Grande Ridge) has been determined using a 10Be profile as measured with a Tandem Van de Graaff... -
(Table 1, page 119) 10Be and 9Be concentrations in manganese nodules of the P...
The usefulness of cosmogenic beryllium-10 (half life = 2.5 Ma) for studying the rates of accumulation of ferromanganese nodules is reported based on its measured depth... -
(Table 1) Soil density and concentration of 10Beryllium and 26Aluminium in sa...
The McMurdo Dry Valleys, Antarctica (MDV) are among the oldest landscapes on Earth, and some landforms there present an intriguing apparent contradiction such that millions of... -
(Table 1) 10 Beryllium and CaCO3 at DSDP Holes 86-576B, 86-576, and 86-578
Extension of the 10Be geochronology for deep-sea sediments beyond the limit of late Pliocene age found in published works has been attempted. The results obtained on sediments... -
Beryllium-10, mineralogy and grain size distribution of DSDP Hole 68-502B (Ta...
We present a high-resolution 10Be profile from deep sea sediments (sampled from Hole 502B in the Caribbean sea) that strongly resembles the 10Be record in ice core profiles,... -
(Table 1) The 10Be and 9Be isotope record of IODP EXP202 composite Site
The upper 200 m of the sediments recovered during IODP Leg 302, the Arctic Coring Expedition (ACEX), to the Lomonosov Ridge in the central Arctic Ocean consist almost... -
10Be and barium concentrations of sediment core GeoB1008-3
Particle reactive elements are scavenged to a higher degree at ocean margins than in the open ocean due to higher fluxes of biogenic and terrigenous particles. In order to... -
10Be and 9Be concentrations and ratios of hydroxylamine leachable and residua...
Profiles of both10Be and9Be concentrations have been measured in sediments from the DSDP, Leg 64, Site 477 core. Established in the deep Guaymas Basin, in an area of high heat... -
(Table 1) Chemical compositions of beryllium in sediments and pore waters of ...
Studies of Be distributions in subduction zone sediments will help to understand questions regarding the enrichments of cosmogenic Be-10 in arc volcanic rocks. Analyses of Be-10... -
Radionuclides of sediment core NBP98-02-07-13
negative numbers refer to water or fluff layer above the sediment-water interface -
Radionuclides of sediment core NBP98-02-06-5
negative numbers refer to water or fluff layer above the sediment-water interface -
Radionuclides of sediment core NBP98-02-05-2
negative numbers refer to water or fluff layer above the sediment-water interface -
Radionuclides of sediment core NBP98-02-04-1
negative numbers refer to water or fluff layer above the sediment-water interface