<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>27</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hall, R.I.</style></author><author><style face="normal" font="default" size="100%">Wolfe, B. B.</style></author><author><style face="normal" font="default" size="100%">Edwards, T. W. D.</style></author><author><style face="normal" font="default" size="100%">Johnston, R. N.</style></author><author><style face="normal" font="default" size="100%">Sinnatamby, T. L.</style></author><author><style face="normal" font="default" size="100%">Sokal, M.</style></author><author><style face="normal" font="default" size="100%">Asada, T.</style></author><author><style face="normal" font="default" size="100%">Clogg-Wright, K.</style></author><author><style face="normal" font="default" size="100%">Yi, Y.</style></author><author><style face="normal" font="default" size="100%">Last, W. M.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Lake Athabasca and the Little Ice Age : sustained high-water stand driven by snowmelt-enhanced Athabasca River discharge?, Canadian Quaternary Association Conference, Winnipeg, MB, June 5-8, 2005</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">en</style></language><custom1><style face="normal" font="default" size="100%">Geography</style></custom1><custom4><style face="normal" font="default" size="100%">Science</style></custom4></record></records></xml>