“…There are indications that bog development and associated permafrost formation began earlier in the north and gradually spread southward. Within 1170±150 6510±150 5070±60 6160±90 2800±100 4250±100 6070±100 6280±80 1320±60 7590±80 6940±110 9820±220 2080±60 4750±60 2920±130 6770±140 8260±110 10100±130 1890±60 4810±60 3150±90 6020±100 2200±80 4030±100 2130±80 3850±400 920±80 3890±160 2300±100 Lowdon et ai, 1967Lowdon era/., 1967Tarnocai & Zoltai, 1988Tamocai & Zoltai, 1988Tarnocai & Zoltai, 1988Tarnocai & Zoltai, 1988 This paper This paper Blake, 1987Blake, 1987Dyck & Fyles, 1963Dyck & Fyles, 1963Blake, 1988Blake, 1988Lowdon & Blake, 1981Lowdon & Blake, 1981 This paper This paper Tarnocai & Zoltai, 1988Tarnocai & Zoltai, 1988Tarnocai & Zoltai, 1988Tarnocai & Zoltai, 1988Zoltai et al, 1992Zoltai et al, 1992 This paper This paper This paper This paper This paper This paper Alberta, bog development occurred earlier in the north (about 5 ka) than farther south in the present LPZ (about 2.2 ka, Zoltai and Vitt, 1990). …”