Distribution of dinoflagellate cysts in the Canadian Arctic marine region

Abstract The Canadian Arctic is a major gateway for transport of freshwater from the Arctic Ocean to the North Atlantic. This region comprises the Beaufort Sea, the Canadian Arctic Archipelago (CAA) and northern sections of Baffin and Hudson bays. Subregional differences include major freshwater run...

Full description

Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Mudie, Peta J., Rochon, André
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2001
Subjects:
Online Access:http://dx.doi.org/10.1002/jqs.658
http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.658
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.658
Description
Summary:Abstract The Canadian Arctic is a major gateway for transport of freshwater from the Arctic Ocean to the North Atlantic. This region comprises the Beaufort Sea, the Canadian Arctic Archipelago (CAA) and northern sections of Baffin and Hudson bays. Subregional differences include major freshwater runoff to the Beaufort Sea and Hudson Bay, presence of Pacific and Atlantic Intermediate water in the west, and Atlantic Water in Baffin and Hudson bays. Principal component analysis of 50 core‐top samples shows four subregional dinoflagellate cyst assemblages. Outer Beaufort Shelf Assemblage I is co‐dominated by Operculodinium centrocarpum s.l. and Brigantedinium spp., with minor cysts of Pentapharsodinium dalei , Algidasphaeridium ? minutum s.l. and cysts of Polykrikos spp. Assemblage II in the Canadian Arctic Archipelago is co‐dominated by Brigantedinium spp., A. ? minutum s.l. and cysts of Polykrikos spp., including two Arctic morphotypes. Assemblage III in the North Water polynya exclusively comprises A. ? minutum s.l. and Brigantedinium spp. Assemblage IV in Baffin Bay is dominated by O. centrocarpum s.l. and Spiniferites spp., with Brigantedinium spp. on the shelves. The ratio of gonyaulacoid to protoperidinioid cysts (G : P) generally decreases with increased sea‐ice cover, but it may also decrease in river plumes and in polynyas. Copyright © 2001 John Wiley & Sons, Ltd.