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- W2247193458 abstract "Recent palynological studies of late-glacial sites in Nova Scotia and New Brunswick have indicated a cold event between 11,000 and 10,000 years B.P. equivalent to the younger Dryas recognized in Europe. Some sites investigated for pollen content are organic-rich peats and sands suitable for paleoentomological analysis. Preliminary studies at two Nova Scotia sites, Lismore ( 11,900 10,500 years B.P.) and Collins Pond (12,700 11,800 years B.P.) have yielded fossil Coleoptera (beetle) fragments. Bottom samples from Lismore contain a small beetle fauna. Bottom samples from Collins Pond are almost devoid of beetle fragments, likely resulting from poor preservation. Both sites, along with several yet to be sampled, span the period of the younger Dryas equivalent recognized in pollen profiles. Beetle faunas from Lismore suggest that shortly after 12,000 years ago conditions were similar to that in the present boreal forest. Species like Acidota cf. quadrata, Olophrum consimile, 0. rotundicolle, Tachinus cf. tachyporoides, and Eocnecosum are transcontinental, boreal insects. There presence suggests climatic conditions cooler than present, probably more similar to the southern to middle boreal forest. Little work has been done on fossil beetles from Atlantic Canada and further research may provide interesting comparisons with more extensive work carried out in the mid-continent over the past two decades." @default.
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- W2247193458 date "1989-01-01" @default.
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- W2247193458 title "Abstract: Fossil Coleoptera studies of Late-Glacial sites in Nova Scotia" @default.
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