Archive

  • Visit JGI.DOE.GOV
Our Projects
Home › CSP Plans › Why Sequence Phaeocystis antarctica?

Approved Proposals FY08

Why Sequence Phaeocystis antarctica?

Phaeocystis is a group of important unicellular, photosynthetic, eukaryotic algae distributed throughout the world’s oceans. Representatives of this genus live in the open ocean as well as in sea ice. A unique attribute of Phaeocystis is its ability to form a floating colony with hundreds of cells embedded in a polysaccharide gel matrix that can multiply massively during blooms.

Diffraction interference contrast micrograph of P. antarctica colony with five cells embedded in a carbohydrate matrix. Photo courtesy Oliver Killian and Gry Mine Berg.

Diffraction interference contrast micrograph of P. antarctica colony with five cells embedded in a carbohydrate matrix. Photo courtesy Oliver Killian and Gry Mine Berg.

The polar algae Phaeocystis antarctica is a key member of the phytoplankton community in the Southern Ocean where it plays a major role in global carbon and sulfur cycles. It sequesters CO2 efficiently over large geographical areas and is a major emitter of 3-dimethylsulphoniopropionate (DMSP), the precursor of dimethyl sulfide (DMS). Biogenic DMS is a highly volatile gas that contributes about 1.5×1013 grams of sulfur to the atmosphere annually. As such, P. Antarctica may be a source of sulfate aerosols that play an important part in cloud formation and potentially in climate regulation.

Although P. Antarctica has been investigated intensively for decades in cultures and in the field, important questions with respect to its life cycle and growth regime remain unanswered. Sequencing of the P. antarctica genome will provide long-awaited insights into processes that enable it to transition from solitary to colonial stages, to form massive blooms, and to transition from the water column to sea ice. Ultimately, a better understanding of the metabolic pathways present in this enigmatic organism may aid in forecasting its future distribution as global warming continues and ice cover diminishes in the Southern Ocean ecosystem.

Principal Investigators: Gry Mine Berg and Kevin R. Arrigo (Stanford Univ.) and Arthur R. Grossman (The Carnegie Inst.)

Share this:

  • Click to share on Facebook (Opens in new window)
  • Click to share on LinkedIn (Opens in new window)
  • Click to share on Pinterest (Opens in new window)
  • Click to share on Twitter (Opens in new window)
  • Click to print (Opens in new window)

More from the JGI archives:

  • Software Tools
  • Science Highlights
  • News Releases
  • Blog
  • User Proposals
  • 2018-24 Strategic Plan
  • Progress Reports
  • Historical Primers
  • Legacy Projects
  • Past Events
  • JGI.DOE.GOV
  • Disclaimer
  • Accessibility / Section 508
Lawrence Berkeley National Lab Biosciences Area
A project of the US Department of Energy, Office of Science

JGI is a DOE Office of Science User Facility managed by Lawrence Berkeley National Laboratory

© 1997-2025 The Regents of the University of California