Effects of shoreline permafrost thaw on nutrient dynamics and diatom ecology in a subarctic tundra pond

Author:

Morison M. Q.ORCID,Volik O.,Hall R. I.,Wiklund J. A.,Macrae M. L.,Petrone R. M.

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Aquatic Science

Reference72 articles.

1. Anderson NJ, Curtis CJ, Whiteford EJ, Jones VJ, McGowan S, Simpson GL, Kaiser J (2018) Regional variability in the atmospheric nitrogen deposition signal and its transfer to the sediment record in Greenland lakes. Limnol Oceanogr 63:2250–2265

2. Appleby PG (2001) Chronostratigraphic techniques in recent sediments. In: Last WM, Smol JP (eds) Tracking environmental change using lake sediments: vol. 1: basin analysis, coring, and chronological techniques. Kluwer Academic Publishers, Dordrecht, pp 171–203

3. Appleby PG, Oldfield F (1978) The calculation of lead-210 dates assuming a constant rate of supply of unsupported 210Pb to the sediment. CATENA 5:1–8

4. Battarbee RW, Jones VJ, Flower RJ, Cameron NG, Bennion H, Carvalho L, Juggins S (2001) Diatoms. In: Smol JP, Birks HJB, Last W (eds) Tracking environmental change using lake sediments. Vol. 3: terrestrial, algal, and siliceous indicators. Springer, Dordrecht, pp 155–202

5. Bergström AK (2010) The use of TN: TP and DIN: TP ratios as indicators for phytoplankton nutrient limitation in oligotrophic lakes affected by N deposition. Aquat Sci 72:277–281

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