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UGA-Marine Sciences    Gordon and Betty Moore Foundation   National Science Foundation
 

Sulfitobacter sp. EE-36

©Dennis Kunkel Microscopy, Inc.

Ecology and Physiology

Isolate Sulfitobacter sp. EE-36 was isolated from the salt marsh on the coast of Georgia, US. Phylogenetically it belongs to the Sulfitobacter genus, which has been isolated from numerous places. Originally Sulfitobacter was isolated from the Black Sea, although it proved to be abundant in other environments, such as coastal and open ocean environments, an Antarctic lake and in symbiosis with sea animals. Sulfitobacter is particularly abundant in environments with a constant source of inorganic sulphur, like the Black Sea sediment or seafloor. Sulfitobacter sp. EE-36 stands out for its high inorganic sulphur oxidation activity. It is able to oxidize sulfite and thiosulfate, possibly to conserve energy for growth. It also grows on DMSP and glycine betaine as sole carbon sources.

For NCBI Genome Page, click here.

Moore Foundation

 
General features of the Sulfitobacter sp. EE-36
Feature
Total number of coding sequiences 3,474
G + C content (%) 60.0
Est. Genome size (bp) 3,547,243
% Coding 90.0
Sequence status Draft

Roseobacter Genomes

Dinoroseobacter shibae DFL 12 Roseobacter sp. AzwK-3b Roseovarius nubinhibens ISM
Jannaschia sp. CCS1 Roseobacter denitrificans OCh 114 Roseovarius TM1035
Loktanella vestfoldensis SKA53 Roseobacter sp. CCS2 Sagittula stellata E-37
Oceanicola batsensis HTCC2597 Roseobacter sp. MED193 Silicibacter pomeroyi DSS-3
Oceanicola granulosus HTCC2516 Roseobacter RCA clade HTCC2150 Silicibacter sp. TM1040
Rhodobacterales bacterium HTCC2255 Roseobacter SK209-2-6 Sulfitobacter sp. EE-36
Rhodobacterales bacterium HTCC2654 Roseovarius sp. 217 Sulfitobacter NAS-14.1
  Roseovarius sp. HTCC2601  
 

Shulei Sun
Scientific Computing Professional Associate  [shulei@uga.edu]

Dr. Mary Ann Moran
Research Professor Department of Marine Sciences  [mmoran@uga.edu]

University of Georgia
Department of Marine Sciences
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This material is based upon work supported by the National Science Foundation under Grant No. 0315200.

Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s)
and do not necessarily reflect the views of the National Science Foundation.