Results/Conclusions
Pine Lake has 1-2% hemlock pollen throughout most of the last thousand years and a peak of 3-6% hemlock pollen from 850-650 years ago. One to two percent hemlock pollen is present throughout the last 1000 years in Sawdust Lake, 10 km southwest of Pine Lake. Other cores from nearby sites outside the continuous range of hemlock seldom exceed 1% hemlock pollen and none exceed 2%. Analogs to PLS-age pollen samples of 30 other sites on sandy soils in the region shift from jack-red pine dominated vegetation to red pine-birch vegetation in Pine Lake at about 850 cal yr BP. The peak of hemlock pollen at Pine Lake is well above the regional background level of 0-2% represented in Sawdust and other lakes. We interpret this peak of hemlock pollen at Pine Lake as evidence for the establishment of a disjunct population of hemlock by long-distance seed dispersal. After ~600 cal. yr BP hemlock pollen percentages at Pine Lake decrease to about the level found at Sawdust Lake. This site provides rare documentation of the establishment of a disjunct population 10s of km from the range limit of hemlock at the time.