The influence of water-table depth and pH on the spatial distribution of diatom species in peatlands of the Boreal Shield and Hudson Plains, Canada

Author:

Hargan Kathryn E.1,Rühland Kathleen M.1,Paterson Andrew M.2,Finkelstein Sarah A.3,Holmquist James R.4,MacDonald Glen M.4,Keller Wendel5,Smol John P.1

Affiliation:

1. Paleoecological Environmental Assessment and Research Laboratory (PEARL), Department of Biology, 116 Barrie Street, Queen’s University, Kingston, ON K7L 3N6, Canada.

2. Ontario Ministry of the Environment and Climate Change, Dorset Environmental Science Centre, 1026 Bellwood Acres Road, Dorset, ON P0A 1E0, Canada.

3. Department of Earth Sciences, University of Toronto, 22 Russell Street, Toronto, ON M5S 3B1, Canada.

4. Department of Geography, University of California, Los Angeles, 1255 Bunche Hall, Box 951524, Los Angeles, CA 90095, USA.

5. Cooperative Freshwater Ecology Unit, Living with Lakes Centre, Laurentian University, 935 Ramsey Lake Road, Sudbury, ON P3E 2C6, Canada.

Abstract

Diatoms collected from 113 surface peat samples from the Boreal Shield and Hudson Plains show taxonomic distributions that are associated with macro-vegetation type, pH, and position relative to the water table, the main environmental variables measured in this study. The overall goal of our research was to determine the ecological distribution and response of diatoms to microhabitat conditions, and to assess the potential for diatoms to be applied as indicators of long-term environmental change in northern peatlands. Our results indicate that diatom assemblage composition was determined by both the broader peatland type (i.e., bog, rich and poor fens) and microhabitats within peatland formations (e.g., hummock, hollow). The diatom assemblages were primarily influenced by pH with the sites divided at a critical pH of 5.5, and secondarily by the depth to the water table. Acidic bog hollow and hummock microhabitats were species-poor and dominated almost exclusively by Eunotia paludosa A.Grunow and (or) Eunotia mucophila (H.Lange-Bertalot, M.Nörpel-Schempp & E.Alles) H.Lange-Bertalot. These acidophilic and aerophilic diatom species were associated with the narrow pH optima of the dominant Sphagnum L. species (e.g., Sphagnum fuscum (Schimp.) Klinggr., Sphagnum angustifolium (C.E.O.Jensen ex Russow) C.E.O.Jensen) found in these bog habitats. Rich and poor fen samples, which were less acidic, supported a more diverse diatom assemblage (>30 species) with greater variability in both diatom and bryophyte pH tolerances. The diatom assemblages recorded in the bogs and fens of our study are similar to those found in peatlands around the world, demonstrating that diatom species are very specialized to exist in these often harsh semi-aquatic environments. Diatoms from peatlands have great potential as biomonitors of environmental change in these important ecosystems.

Publisher

Canadian Science Publishing

Subject

Plant Science,Ecology,Ecology, Evolution, Behavior and Systematics

Reference92 articles.

1. Antoniades, D., Hamilton, P.B., Douglas, M.S.V., and Smol, J.P. 2008. Diatoms of North America: the freshwater floras of Prince Patrick, Ellef Ringnes, and Northern Ellesmere Islands from the Canadian Arctic Archipelago. Iconographia Diatomologica, Vol. 17.

2. Battarbee, R.W., Charles, D.F., Bigler, C., Cumming, B.F., and Renberg, I. 2010. Diatoms as indicators of surface-water acidity. In The diatoms: applications for the environmental and earth sciences. Edited by J.P. Smol and E.F. Stoermer. Cambridge University Press, New York. pp. 98–121.

3. Environmental and biotic controls on bryophyte productivity along forest to peatland ecotones

4. Fate of silicate minerals in a peat bog

5. On the subboreal climate of the Belgian campine as deduced from diatom and testate amoebae analyses

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