This paper reports a first estimate of the Holocene lake sediment carbon po
ol in Alberta, Canada. The organic matter content of lake sediment does not
appear to depend strongly on lake size or other limnological parameters, a
llowing a simple first estimate in which we assume all Alberta lake sedimen
t to have the same organic matter content. Alberta lake sediments sequester
about 15 g C m(-2) yr(-1), for a provincial total of 0.23 Tg C yr(-1), or
2.3 Pg C over the Holocene. Alberta lakes may represent as much as 1/1700 o
f total global, annual permanent carbon sequestration.