GEOSCAN Search Results: Fastlink


TitleDiatom ecological response to deposition of the 833-850 CE White River Ash (east lobe) ashfall in a small subarctic Canadian lake
AuthorHutchinson, S J; Hamilton, P B; Patterson, R T; Galloway, J MORCID logo; Nasser, N A; Spence, C; Falck, H
SourcePeerJ 7, 6269, 2019 p. 1-21, Open Access logo Open Access
Alt SeriesNatural Resources Canada, Contribution Series 20180371
Mediapaper; on-line; digital
File formatpdf; html
ProvinceNorthwest Territories
AreaPocket Lake; Yellowknife
Lat/Long WENS-114.3833 -114.3667 62.5167 62.5000
Subjectsenvironmental geology; surficial geology/geomorphology; paleontology; geochronology; stratigraphy; Recent; paleoecology; surface waters; lakes; biota; microfossils; algae; diatoms; fossil assemblages; lake sediment cores; tectonic history; volcanism; volcanic ash; depositional history; depositional environment; lacustrine environments; radiometric dating; radiocarbon dating; fossil distribution, strata; stratigraphic analyses; biostratigraphy; biological communities; ecosystems; environmental impacts; acidity; paleoclimates; White River Ash; Mount Churchill Volcano; lacustrine sediments; Resilience; Environmental adaptation; Phanerozoic; Cenozoic; Quaternary
Illustrationslocation maps; geoscientific sketch maps; tables; models; photographs; profiles; graphs; biostratigraphic charts
ProgramEnvironmental Geoscience Metal Mining: northern baselines
Released2019 01 25
AbstractA <5 mm thick volcanic ashfall layer associated with the White River Ash (east lobe [WRAe]) originating from the eruption of Mount Churchill, Alaska (833-850 CE; 1,117-1,100 cal BP) was observed in two freeze cores obtained from Pocket Lake (62.5090ºN, -114.3719ºW), a small subarctic lake located within the city limits of Yellowknife, Northwest Territories, Canada. Here we analyze changes in diatom assemblages to assess impact of tephra deposition on the aquatic biota of a subarctic lake. In a well-dated core constrained by 8 radiocarbon dates, diatom counts were carried out at 1-mm intervals through an interval spanning 1 cm above and below the tephra layer with each 1 mm sub-sample represented about 2 years of deposition. Non-metric Multidimensional Scaling (NMDS) and Stratigraphically Constrained Incremental Sum of Squares (CONISS) analyses were carried out and three distinct diatom assemblages were identified throughout the interval. The lowermost 'Pre-WRAe Assemblage (Pre-WRAeA)' was indicative of slightly acidic and eutrophic lacustrine conditions. Winter deposition of the tephra layer drove a subsequent diatom flora shift to the 'WRAe Assemblage (WRAeA)' the following spring. The WRAeA contained elevated abundances of taxa associated with oligotrophic, nutrient depleted and slightly more alkaline lake waters. These changes were only apparent in samples within the WRAe containing interval indicating that they were short lived and only sustained for a single year of deposition. Immediately above the WRAe horizon, a third, 'Post-WRAe Assemblage (Post-WRAeA)' was observed. This assemblage was initially similar to that of the Pre-WRAeA but gradually became more distinct upwards, likely due to climatic patterns independent of the WRAe event. These results suggest that lacustrine environments are sensitive to perturbations such as deposition of ash fall, but that ecological communities in subarctic systems can also have high resilience and can recover rapidly. If subsampling of the freeze cores was carried out at a more standard resolution (0.5-1 cm) these subtle diatom ecological responses to perturbation associated with the WRAe depositional event would not have been observed. This research illustrates the importance of high-resolution subsampling when studying the environmental impact of geologically 'near instantaneous' events such as episodic deposition of ashfalls.
Summary(Plain Language Summary, not published)
This study examines the response of lacustrine algae to deposition of an ash layer associated with a volcanic eruption. The study provides new insight to recovery rates of algae to disturbance in a subarctic lake.

Date modified: