Postglacial vegetation and climate dynamics in the Seymour-Belize Inlet Complex, central coastal British Columbia, Canada:Palynological evidence from Tiny Lake

• Published in: Journal of Quaternary Science
• Main Authors: Galloway, Jennifer M., Doherty, Christine T., Patterson, R. Timothy, Roe, Helen M.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2009
• Subjects: Palaeoclimatology; Palaeoecology; Palynology; aleutian low
• Online Access: https://pure.au.dk/portal/da/publications/postglacial-vegetation-and-climate-dynamics-in-the-seymourbelize-inlet-complex-central-coastal-british-columbia-canada(b20084ca-9abc-4844-a5c1-9ba4e3eff726).html; https://doi.org/10.1002/jqs.1232; http://www.scopus.com/inward/record.url?scp=66249087650&partnerID=8YFLogxK

A pollen-based study from Tiny Lake in the Seymour-Belize Inlet Complex of central coastal British Columbia, Canada, permits an evaluation of the dynamic response of coastal temperate rainforests to postglacial climate change. Open Pinus parklands grew at the site during the early Lateglacial when the climate was cool and dry, but more humid conditions in the later phases of the Lateglacial permitted mesophytic conifers to colonise the region. Early Holocene conditions were warmer than present and a successional mosaic of Tsuga heterophylla and Alnus occurred at Tiny Lake. Climate cooling and moistening at 8740±70 14C a BP initiated the development of closed, late successional T. heterophylla-Cupressaceae forests, which achieved modern character after 6860±50 14 C a BP, when a temperate and very wet climate became established. The onset of early Holocene climate cooling and moistening at Tiny Lake may have preceded change at more southern locations, including within the Seymour-Belize Inlet Complex, on a meso- to synoptic scale. This would suggest that an early Holocene intensification of the Aleutian Low pressure system was an important influence on forest dynamics in the Seymour-Belize Inlet Complex and that the study region was located near the southern extent of immediate influence of this semi-permanent air mass.