Pollen transport and representation in the Coast Mountains of British Columbia. I. Flowering phenology and aerial deposition
- 1 October 1984
- journal article
- research article
- Published by Canadian Science Publishing in Canadian Journal of Botany
- Vol. 62 (10), 2154-2164
- https://doi.org/10.1139/b84-295
Abstract
Two years of aerial pollen trapping at two lakes surrounded by coniferous forest are summarized. Most of the annual pollen and spore deposition occurs between February and May (86%), followed by 10% during the summer, and 4% during the fall – winter nonflowering period. Annual aerial influx is very similar at both Marion and Surprise lakes, ca. 5000 grains∙cm−2∙year−1. The annual frequency spectra are also equivalent, with a predominance of Cupressaceae (32%) and Alnus (35%), followed by Tsuga heterophylla (8 – 11%), grasses (8 – 10%), and pine (2 – 3%). Regional, rather than local or extralocal pollen, is estimated to account for about 90% of the annual aerial deposition at both lakes. The data also suggest that pollen transport is predominantly upslope in this mountainous area.This publication has 6 references indexed in Scilit:
- The Selection of Sites for Paleovegetational StudiesQuaternary Research, 1981
- A 12 000 year palynological record of temperature and precipitation trends in southwestern British ColumbiaCanadian Journal of Botany, 1981
- The Modern and Late Quaternary Vegetation of the Campbell‐Dolomite Uplands, near Inuvik, N.W.T., CanadaEcological Monographs, 1977
- Temporal and Spatial Differences in Phytoplankton Productivity in Marion Lake, British ColumbiaJournal of the Fisheries Research Board of Canada, 1967
- A METHOD OF ABSOLUTE POLLEN COUNTINGNew Phytologist, 1967
- Recent Pollen Spectra from the Deciduous and Coniferous‐Deciduous Forests of Northeastern Minnesota: A Study in Pollen DispersalEcology, 1966