Timing of the last Deglaciation in the Sierra Nevada of the Mérida Andes, Venezuela
Timing of the last Deglaciation in the Sierra Nevada of the Mérida Andes, Venezuela
复制标题
委内瑞拉梅里达安第斯山脉内华达山脉最后一次冰消期的时间
DOI:
10.1016/j.yqres.2013.08.001
复制
发表时间:
2013
影响因子:
2.3
通讯作者:
C. Beck
中科院分区:
文献类型:
--
作者:
J. Carcaillet;I. Ángel;E. Carrillo;F. Audemard;C. Beck
In the tropical Mérida Andes (northwestern Venezuela), glacial landforms were found at altitudes between 2600 and 5000 m, corresponding to 600 km2 of ice cover during the maximum glacial extension. However, the lack of sufficient absolute age data prevents detailed reconstruction of the timing of the last deglaciation. On the northwestern flank of the Mucuñuque Massif, successive moraines and striated eroded basement surfaces were sampled for cosmogenic 10Be investigation. Their compilation with published data allows the establishment of a detailed chronology of the post-LGM glacier history. The oldest moraines (18.1 and 16.8 ka) correspond to the Oldest Dryas. Successive moraine ridges indicate stops in the overall retreat between the LGM and the Younger Dryas. The cold and short Older Dryas stadial has been identified. Results indicate that most of the ice withdrew during the Pleistocene. The dataset supports an intensification of the vertical retreat rate from ~ 25 m/ka during the late Pleistocene to ~ 310 m/ka during the Pleistocene/Holocene. Afterwards, the glacier was confined and located in the higher altitude zones. The altitude difference of the Younger Dryas moraines in the Mucubají, La Victoria and Los Zerpa valleys indicates a strong effect of valley orientation on the altitude of moraine development.
影响因子:
5.3
作者:
Kaplan, Michael R.;Strelin, Jorge A.;Travis, Scott G.
通讯作者:
Travis, Scott G.
影响因子:
2.7
作者:
Putnam, A. E.;Schaefer, J. M.;Kelley, S. E.
通讯作者:
Kelley, S. E.