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The Annual Oceanographic Cycle at Igloolik in the Canadian Arctic: II. The Phytoplankton

1961/04/01 by Adam S. Bursa · 3 citations
Agricultural and Biological Sciences · Earth and Planetary Sciences · Environmental Science · #Annual cycle #Arctic #Biology #Biomass (ecology) #Botany #Ecological succession #Ecology #Environmental science #Fauna #Flagellate #Food Industry and Aquatic Biology #Geological Studies and Exploration #Geology #Hydrography #Methane Hydrates and Related Phenomena #Nutrient #Oceanography #Phytoplankton

paper · doi:10.1139/f61-046

openalex publication_date 1961/04/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/05/21

Abstract

Phytoplankton populations near Igloolik, northern Foxe Basin, began to increase in late April, and reached their climax in mid-August. The rapid late-August decline of the phytoplankton populations coincided with diminishing light. Diatoms were the main biomass producers in Igloolik and the principal food for the marine fauna. The succession of spring Pennatae and summer Centriceae apparently was caused by light and ice conditions. Taxonomic composition of the Igloolik phytoplankton was influenced by the fast ice and by the shallowness and hydrographic uniformity of the adjacent areas. Descriptions are given of two new species of dinoflagellates, Gyrodinium arcticum and Gymnodinium intercalaris, and the new coccolithine flagellate Pontospkaera ditrematolitha.

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