<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Wieder, R. Kelman</style></author><author><style face="normal" font="default" size="100%">Scott, Kimberli D.</style></author><author><style face="normal" font="default" size="100%">Kamminga, Katherine</style></author><author><style face="normal" font="default" size="100%">Vile, Melanie A.</style></author><author><style face="normal" font="default" size="100%">Vitt, Dale H.</style></author><author><style face="normal" font="default" size="100%">Bone, Tiffany</style></author><author><style face="normal" font="default" size="100%">Xu, Bin</style></author><author><style face="normal" font="default" size="100%">Benscoter, Brian W.</style></author><author><style face="normal" font="default" size="100%">Bhatti, Jagtar S.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Postfire carbon balance in boreal bogs of Alberta, Canada</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://cfs.nrcan.gc.ca/bookstore_pdfs/29160.pdf</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">Global Change Biology</style></publisher><volume><style face="normal" font="default" size="100%">15</style></volume><pages><style face="normal" font="default" size="100%">63-81</style></pages><language><style face="normal" font="default" size="100%">en</style></language><abstract><style face="normal" font="default" size="100%">Boreal peatland ecosystems occupy about 3.5 million km2 of the earth’s land surface and store between 250 and 455 Pg of carbon (C) as peat. While northern hemisphere boreal peatlands have functioned as net sinks for atmospheric C since the most recent deglaciation, natural and anthropogenic disturbances, and most importantly wildfire, may compromise peatland C sinks. To examine the effects of fire on local and regional C sink strength, we focused on a 12 000 km2 region near Wabasca, AB, Canada, where ombrotrophic Sphagnum-dominated bogs cover 2280km2 that burn with a fire return interval of 123 </style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue><custom1><style face="normal" font="default" size="100%">Biology</style></custom1><custom2><style face="normal" font="default" size="100%">Pelican Lake</style></custom2><custom3><style face="normal" font="default" size="100%">http://www.worldcat.org/oclc/438955365</style></custom3><custom4><style face="normal" font="default" size="100%">Science</style></custom4></record></records></xml>