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Use of exogenous glycine betaine and its precursor choline as osmoprotectants in Antarctic sea‐ice diatoms 1
Author(s) -
Torstensson Anders,
Young Jodi N.,
Carlson Laura T.,
Ingalls Anitra E.,
Deming Jody W.
Publication year - 2019
Publication title -
journal of phycology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.85
H-Index - 127
eISSN - 1529-8817
pISSN - 0022-3646
DOI - 10.1111/jpy.12839
Subject(s) - osmoprotectant , betaine , osmolyte , biology , salinity , seawater , dimethylsulfoniopropionate , oceanography , environmental chemistry , botany , biochemistry , ecology , chemistry , phytoplankton , proline , nutrient , amino acid , geology
Wide salinity ranges experienced during the seasonal freeze and melt of sea ice likely constrain many biological processes. Microorganisms generally protect against fluctuating salinities through the uptake, production, and release of compatible solutes. Little is known, however, about the use or fate of glycine betaine ( GBT hereafter), one of the most common compatible solutes, in sea‐ice diatoms confronted with shifts in salinity. We quantified intracellular concentrations and used [ 14 C]‐labeled compounds to track the uptake and fate of the nitrogen‐containing osmolyte GBT and its precursor choline in three Antarctic sea‐ice diatoms Nitzschia lecointei , Navicula cf. perminuta, and Fragilariopsis cylindrus at −1°C. Experiments show that these diatoms have effective transporters for GBT , but take up lesser amounts of choline. Neither compound was respired. Uptake of GBT protected cells against hyperosmotic shock and corresponded with reduced production of extracellular polysaccharides in N. lecointei cells, which released 85% of the retained GBT following hypoosmotic shock. The ability of sea‐ice diatoms to rapidly scavenge and release compatible solutes is likely an important strategy for survival during steep fluctuations in salinity. The release and recycling of compatible solutes may play an important role in algal–bacterial interactions and nitrogen cycling within the semi‐enclosed brines of sea ice.