TY - JOUR
T1 - A high-resolution 10Be profile from deep sea sediment covering the last 70 Ka
T2 - Indication for globally synchronized environmental events
AU - Aldahan, A.
AU - Possnert, G.
N1 - Funding Information:
The sediment samples were kindly provided by the ODP repository stuff at La Jolla. We thank professor S. Johnsen for providing the δ 18 O data of the Summit ice core. Financial support for this work was provided by the Swedish Natural Science Research Council (NFR), Knut and Alice Wallenberg Foundation and the Tandem Laboratory (AMS group).
PY - 1998/11
Y1 - 1998/11
N2 - 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, particularly the Vostok core from Antarctica. This high-resolution profile revealed occurrences of enhanced 10Be concentrations at about 23-24, 37-39 and 60-65 ka. The excellent match between these peaks appearing in a georeservoir profile other than in polar ice, strengthens the implications that can be inferred from 10Be and provide global markers for chronological correlation of climatic events. The position at low latitude of the studied sediment section is, unlike the case with the high latitude polar regions, excellent for exposing causes of modulation in 10Be production. We interpret the source of the pattern and enhancements, particularly the 37-39 ka peak, of 10Be to be global and do not strictly relate to climatic conditions and/or production rates specific to the polar regions.
AB - 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, particularly the Vostok core from Antarctica. This high-resolution profile revealed occurrences of enhanced 10Be concentrations at about 23-24, 37-39 and 60-65 ka. The excellent match between these peaks appearing in a georeservoir profile other than in polar ice, strengthens the implications that can be inferred from 10Be and provide global markers for chronological correlation of climatic events. The position at low latitude of the studied sediment section is, unlike the case with the high latitude polar regions, excellent for exposing causes of modulation in 10Be production. We interpret the source of the pattern and enhancements, particularly the 37-39 ka peak, of 10Be to be global and do not strictly relate to climatic conditions and/or production rates specific to the polar regions.
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U2 - 10.1016/S0277-3791(97)00089-9
DO - 10.1016/S0277-3791(97)00089-9
M3 - Article
AN - SCOPUS:0031791888
SN - 0277-3791
VL - 17
SP - 1023
EP - 1032
JO - Quaternary Science Reviews
JF - Quaternary Science Reviews
IS - 11
ER -