Bacteria Genomes - SYNECHOCOCCUS ELONGATUS
Synechococcus elongatus
is a model for photosynthetic and circadian rhythm studies
Synechococcus elongatus
is a freshwater unicelluar oligotrophic cyanobacterium , Synechococcus is among the most important
photosynthetic bacteria in the marine environment, estimated to
account for about 25 percent of the primary production that occurs
in typical marine habitats. Unlike other photosynthetic prokaryotes,
it use chlorophyllA (as do plants)
and water as the source of electrons to reduce CO 2 to carbohydrate.
Formerly named Anacystis nidulans it has a 2.7-Mb chromosome.
The factors
that control their growth directly impact oceanic processes, such
as the marine carbon and nitrogen cycles. Cyanobacteria, including
species of Synechococcus, Prochlorococcus , Trichodesmium , and Crocosphaera , are prominent
constituents of the marine biosphere that account for a significant
percentage of oceanic primary productivity.
Iron
is an essential trace element for all bacteria. Despite their environmental
importance and the belief that Fe (ferric iron) limits their growth
in many regimens we know very little about how open-ocean cyanobacteria
acquire Fe. Recent work has indicated that primary production in
the equatorial Pacific Ocean is limited by Fe bioavailability, thereby
implying that Fe may be an important limiting factor for open-ocean
cyanobacterial growth in other regions of the ocean. Determining
how these microorganisms respond to Fe stress and how they acquire
Fe from the environment will provide insights into the factors that
limit their growth and greatly increase our understanding of how
marine Fe cycling impacts oceanic processes.
The comparison
between the genomes of two Prochlorococcus ecotypes and Synechococcus may help elucidate the key factors that regulate species diversity,
and the resulting biogeochemical cycles, in today’s oceans.
Biological
rhythmicity and the clock mechanisms that drive biological rhythms
are fundamental properties of all groups of cellular life, ranging
from prokaryotes to humans. These biological clocks time specific
molecular, physiological, and behavioural events to optimise their
phase relationships relative to the time of day (circadian) and
time of year (circannual). The identities of individual clock components
or genes suggest that clock mechanisms may have evolved multiple
times in the history of life on Earth. Analysis of the cyanobacterial
clock in Synechococcus appears to show that all of transcription
is rhythmic and that regulation by the clock loci kai (which bear no relationship to per , frq or
any of the genes isolated in eukaryotes) occurs at several levels
to determine circadian period and phase.
References:
http://genome.jgi-psf.org/draft_microbes/synel/synel.home.html
http://www.tamu.edu/clocks/
Planta. 205(1):73-81 (1998)
Biochim. Biophys. Acta 1264, 289-293 (1995).
Plant Cell Physiol. 41: 1085-1095 (2000)
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