Landscape heterogeneity and response of lake ecosystems to changes in climate and peatland expansion over the past 7500 years at the tundra-forest border of northern Manitoba, Canada

• Published in: Holocene (Sevenoaks) 2024-09, Vol.34 (9), p.1252-1265
• Main Authors: Umbanhowar, Charles E, Camill, Philip, Edlund, Mark, Hobbs, Will O, Geiss, Christoph, Stefanova, Vania, Lynch, Jason A
• Format: Article
• Language: English
• Subjects: Annual precipitation; Aquatic ecosystems; Climate change; Climate models; Cores; Heterogeneity; Holocene; Hydrology; Lakes; Landscape; Organic matter; Peat; Peatlands; Pollen; Precipitation; Sediment; Sediments; Silica; Sphagnum; Spores; Tundra
• ISSN: 0959-6836; 1477-0911
• DOI: 10.1177/09596836241254479

Responses of Arctic lakes to climate change are complex and heterogeneous at regional to local scales, but there are few studies comparing multiple sites within the same landscape. We studied sediment cores recovered from seven lake sites located within the forest-tundra biome of northern Manitoba, Canada. We first used sediment core pollen from the seven sites to reconstruct July temperatures and total annual precipitation for the past 7500 years based on the modern analog technique. Lake responses and peatland expansion were analyzed based on changes in the concentration and quality of organic matter, biogenic silica (bSi), Sphagnum spores, and published peat core basal dates. Changes in sediment organic matter and bSi were concentrated prior to 4500 cal. Yr BP. From 7500 to 3100 cal. Yr BP, July temperatures rose by ~3°C, and total annual precipitation fell by 200 mm; there was little change in temperature or precipitation after 3100 cal. Yr BP. Sphagnum spore concentrations exceeded 0.5% at all of the sites at 7500 cal. Yr BP indicating the early presence of peatlands. Spores increased markedly after 4500 cal. Yr BP in agreement with timing of peat basal dates, but the magnitude and timing of changes varied widely among sites likely reflecting local differences in hydrology or topography. The use of hierarchical generalized additive models provided a unified regional pattern of Holocene climate for northern Manitoba, even though lake responses to climate and peatland expansion differed greatly.