Algal bloom in a melt pond on Canada Basin pack ice

ABSTRACT Melt ponds are common on the surface of ice floes in the Arctic Ocean during spring and summer. Few studies on melt pond algae communities have been accomplished. These studies have shown that these melt ponds were ultra-oligotrophic, and contribute little to overall productivity. However,...

Full description

Bibliographic Details
Published in:Polar Record
Main Authors: Lin, Ling, He, Jianfeng, Zhang, Fang, Cao, Shunan, Zhang, Can
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2015
Subjects:
Online Access:http://dx.doi.org/10.1017/s0032247415000510
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247415000510
Description
Summary:ABSTRACT Melt ponds are common on the surface of ice floes in the Arctic Ocean during spring and summer. Few studies on melt pond algae communities have been accomplished. These studies have shown that these melt ponds were ultra-oligotrophic, and contribute little to overall productivity. However, during the 6th Chinese Arctic Cruise in the Arctic Ocean in summer 2014, a closed coloured melt pond with a chlorophyll a concentration of 15.32 μg/L was observed on Arctic pack ice in the Canada Basin. The bloom was caused by the chlorophyte Carteria lunzensis at an abundance of 15.49×10 6 cells/L and biomass of 5.07 mg C/L. Primary production within surface melt ponds may need more attention along with Arctic warming.