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During the warm middle Eocene (ca 45 Ma), the Napartulik area (also called ‘the Geodetic Hills’), Axel Heiberg Island, northern Canada (Nunavut), was vegetated with mixed broad-leaved deciduous angiosperm and evergreen conifer forests over extensive floodplain and forested wetland habitats. Massive organic rich sedimentary successions and encapsulated  in-situ  tree trunks suggest these forests were drowned by frequent flooding events. The sedimentary layers contain sub-fossil amber that was produced by representatives of the Pinaceae such as  Pseudolarix . The amber offered an opportunity to investigate aerial plankton and thus the chance to discover microfossils, which could provide evidence of biotic interactions associated with, or the cause of, the forest die-offs. Fifty-four amber samples were subjected to a solvent treatment for microfossil extraction followed by light microscopy, resulting in the discovery of several hundred microfossils. Unexpectedly, one-quarter of the microfossils were diatoms, which may predominantly have lived on the tree bark. Fungal spores were rare, and the pollen grains found corroborated earlier findings in litter or coal. The records of fungal spores and arthropod remains were insignificant and could, therefore, not substantially have been contributing to the forest die-offs. More resin analyses from the complete sedimentary profile would be needed to get a clearer picture of putative forest pests and prevailing environmental conditions

Microfossils in resin from the middle Eocene Buchanan Lake Formation, Napartulik, Axel Heiberg Island, Nunavut, Canada