Palaeoenvironmental reconstuction of Holocene climate change in the Trans-Mexican Volcanic Belt : a multi-disciplinary approach
Late Quaternary (c. 11,400 [sup]14 C years BP) palaeoclimates were reconstructed from the sediments of closed lake basins in the western (Laguna de Cuitzéo) and eastern (Laguna de Zempöala) trans-Mexican volcanic belt (TMVB). Climate was separated out as a distinct agent of environmental change from...
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Kingston University
2004
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.412596 |