Domain Eukaryota Order Phaeocystales Rank Genus | Family Phaeocystaceae | |
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Similar Prymnesiales, Prymnesiophyceae, Haptophyte, Phaeocystis pouchetii, Chrysochromulina | ||
Phaeocystis
Phaeocystis is a genus of algae belonging to the Prymnesiophyte class and to the larger division of Haptophyta. It is a widespread marine phytoplankton and can function at a wide range of temperatures (eurythermal) and salinities (euryhaline). Members of this genus live in the open ocean, as well as in sea ice. It has a polymorphic life cycle, ranging from free-living cells to large colonies.
Contents
The ability to form a floating colony is one of the unique attributes of Phaeocystis – hundreds of cells are embedded in a polysaccharide gel matrix, which can increase massively in size during blooms. The largest Phaeocystis blooms form in the polar seas: P. pouchetii in the north and P. antarctica in the south. This intense Phaeocystis productivity generally persists for about a three-month period, spanning most of the summer in the Southern Hemisphere. Phaeocystis-abundant ecosystems are generally associated with commercially important stocks of crustaceans, molluscs, fish and mammals. Phaeocystis may have negative effects on higher trophic levels in the marine ecosystem, and consequent impacts on human activities (such as fish farming and coastal tourism), by forming odorous foams on beaches during the wane of a bloom.
The ability to form large blooms and its ubiquity make Phaeocystis an important contributor to the ocean carbon cycle. In addition, Phaeocystis produces dimethyl sulfide (DMS), a key player in the sulfur cycle.
Phaeocystis globosa
Distribution and life cycle
Free-living forms of Phaeocystis are globally distributed and occur in a variety of marine habitats, including coastal oceans, open oceans, polar seas and sea ice. Six species are currently assigned to the genus: P. antarctica, P. jahnii, P. globosa, P. pouchetti, P. scrobiculata and P. cordata. Three species (P. globosa, P. pouchetii, and P. antarctica) are associated with bloom formation in nutrient-rich areas, which can occur either naturally (e.g. in the Ross Sea, Greenland Sea or the Barents Sea) or due to anthropogenic inputs (e.g. in the Southern Bight of the North Sea or the Persian Gulf). Generally, P. globosa blooms in temperate and tropical waters, whereas P. pouchetii and P. antarctica are better adjusted to the cold temperatures prevailing in Arctic and Antarctic waters, respectively. However, P. pouchetii also tolerates warmer temperatures and has been seen in temperate waters.
Genome comparison has shown that the RUBISCO spacer region (located in the plastid DNA, between two subunits of the enzyme 1,5 -isphosphate carboxylase) is highly conserved among closely related colonial Phaeocystis species and identical in P. antarctica, P. pouchetii and two warm-temperate strains of P. globosa, with a single base substitution in two cold-temperate strains of P. globosa.
Phaeocystis can exist as either free-living cells or colonies. Free-living cells can show a variety of morphologies, depending on the species. All species can exist as scaly flagellates, and this is the only form that has been observed for P. scrobiculata and P. cordata. Three species have been observed as colonies (P. globosa, P. pouchetii and P. antarctica) and these can also exist as a flagellate devoid of scales and filaments. In colonies of Phaeocystis, the colony skin may provide protection against smaller zooplankton grazers and viruses.
While suspected in other species (P. pouchetii and P. antarctica), a haploid-diploid life cycle has only been observed in P. globosa. In this cycle, sexual reproduction is dominant in colony bloom formation/termination, and two types of vegetative reproduction exist.
Impacts on global ocean
The Phaeocystis genus is a major producer of 3-dimethylsulphoniopropionate (DMSP), the precursor of dimethyl sulfide (DMS). Biogenic DMS contributes approximately 1.5×1013 g sulfur to the atmosphere annually and plays a major part in the global sulfur cycle, which can affect cloud formation and, potentially, climate regulation.