Square Haloarchaea of Walsby (SHOW)
(also known as "Square Bacteria"
and "Haloquadratum walsbyi")

The SHOW team - Peter Janssen, David Burns, Mike Dyall-Smith, and Helen Camakaris
First described by Anthony Walsby in 1980, this organism managed to
elude
cultivation for 25 years until it was cultivated as part of my doctoral
research. The first (mixed) culture was detected in the MDS
lab in October 2002, with pure cultures being isolated by the following
year. My work has been published in FEMS Microbiology letters - abstract.
This paper was the second
most
downloaded FEMS Micro. Letters paper in the last quarter of 2004,
and the most downloaded original research paper for that quarter!
My FEMS
paper on the cultivation of the "square bacteria" is recommended by the Faculty of 1000
- you may see the evaluation here (you
must have a subscription to the Faculty of 1000 - if you click the
link from a university you should be able to go directly to the
article).
Interest in this event was widespread, particularly internationally,
with Nature.com carrying a
news story (unfortunately now only available to Nature subscribers).
Local interest included the Australian
ABC (internet article only), while my institution, The University
of
Melbourne, carried an
in-house story which may be seen here.
A second lab independently confirmed cultivation of the organism was possible, using quite different techniques, and published later in 2004 (Bolhuis et al, 2004). At present, work is being undertaken with that research group (Henk Bolhuis and others) to characterise this organism, tentatively named "Haloquadratum walsbyi", after its shape and initial discoverer.
Further information may also be found on Mike Dyall-Smith's website.Haloarchaea - Why research them in Australia (and
worldwide)?
Natural hypersaline environments are a significant part of Australia’s landscape and ecology, while artificial hypersaline lakes are being created to alleviate the country’s salinity problems and also for economic reasons, such as salt harvesting. The distinctive pink colouration of these lakes indicates that, far from being devoid of life, they in fact harbour large and active populations of microorganisms. Saline lakes are widely recognized as highly productive aquatic habitats, harbouring specialised assemblages of species and often supporting large populations of both migrating and breeding birds (Rodriguez-Valera, 1988). It is important to have an understanding of the microbial ecology of these environments, given the increasing importance of these environments in Australia, and also internationally - salt lakes make up about the same volume of the world’s bodies of water as freshwater systems. Of Australia’s largest five lakes, four are salt lakes - Lake Eyre (9500 km2 when full), and the next two largest salt lakes in Australia, Lake Torrens and Lake Gardiner are 5745 and 4351 km2 respectively (Geoscience, 2002).
The oceans are about 3.5% (w/v) salt, mainly NaCl, and contain the
majority of halophilic microorganisms, including a wide variety of
Bacteria and Eukarya (eg. protists and algae), and some Archaea.
Extremely halophilic microrganisms grow between 15% salt up to
saturation (around 37%), and previous studies have found that the
dominant microorganisms in lakes with salinities approaching saturation
are haloarchaea from the Family Halobacteriaceae (Benlloch et al.,
2002), (Oren 2002). High salinity represents an extreme environment
that relatively few organisms have been able to adapt to and occupy.
While the diversity is low in these environments, the productivity and
cell densities can be quite high. Even in lakes with saturated salt
concentrations - when not dried out to salt pans, or after recent
rains, salt lakes are usually near saturation, with a thick layer of
crystalline salt as the lake bed - microbial cell densities can reach
up to 107 to 108 cells per ml. These populations reflect a lack of
predation and often quite high nutrient levels (Oren 2002).
The low total diversity in the lakes makes hypersaline lakes an ideal
candidate system for ecological studies. Investigation into the
nutrient cycling and population dynamics is a more manageable task than
in a high diversity environment such as soil, which can contain as many
as 12-18,000 species per gram (Torsvik et al., 1996). In particular,
multi-pond solar salterns represent ideal candidate model systems due
to their managed nature, in which salt concentrations are kept
relatively constant over time, in contrast to natural systems which are
more susceptible to climatic variation. Additionally, salterns exist
around the world, albeit under somewhat different conditions. This
provides a greater degree of international comparability than compared
to natural systems.
Archaea are now widely considered the third Domain of life alongside
Bacteria and Eukaryotes. Exhibiting features of both of the other
Domains, Archaea represent a remarkable opportunity to study
evolutionary relationships and the development of life. Archaea are
also, in their own right, a diverse and significant part of the
biosphere, particularly in “extreme” environments, although their
distribution is otherwise as broad as Bacteria.
Haloarchaea, and particularly, the family Halobacteriaceae are members
of the Domain Archaea, and comprise the majority of the prokaryotic
population in hypersaline environments (Oren 2002). There are currently
15 recognised genera in the family (Gutierrez et al., 2002). The domain
Bacteria can comprise up to 25% of the prokaryotic community, but is
more commonly a much lower percentage of the overall population (Anton
et al., 2000). At times, the alga Dunaliella salina can also
proliferate in this environment (Casamayor et al., 2002).
Members of several genera within the Halobacteriaceae have been
isolated from saltern crystalliser ponds, including Haloferax,
Halogeometricum, Halococcus, Haloterrigena, Halorubrum, Haloarcula and
Halobacterium families (Oren 2002). However, the viable counts in these
studies have been small when compared to total counts, and the
numerical significance of these isolates has been unclear. Only
recently has it become possible to determine the identities and
relative abundances of organisms in natural populations, typically
using PCR-based strategies that target 16S small subunit ribosomal
ribonucleic acid (16S rRNA) genes. While comparatively few studies of
this type have been performed, results from these suggest that some of
the most readily isolated and studied genera may not in fact be
significant in the in-situ community. This is seen in cases such as the
genus Haloarcula, which is estimated to make up less than 0.1% of the
in situ community (Anton et al., 1999) but commonly appears in
isolation studies.
Isolation of representative populations of the target environment
offers significant potential both for the understanding of the
ecological system and also for research into one of the most easily
accessed Archaea, the Haloarchaea, but is limited by the lack of
cultured representatives of the dominant species present in the
environment as identified by Fluorescent In-Situ Hybridisation (Anton
et al., 1999), clone library and microscopic analysis. At present many
currently isolated representatives are thought to be only minor
components of the total community (Anton et al., 1999).
However, isolation of pure strains is nevertheless an essential
requirement to properly study organisms as it allows characterisation
of their metabolic capabilities and hence an insight into their role in
the natural environment. In addition, pure cultures allow
investigations into the interaction of specific strains and/or other
organisms in the home ecology.
As an example, pure strains are required for viral isolation to be
undertaken. Viral populations are believed responsible for the majority
of nutrient cycling and population turnover in hypersaline lakes
through the lysis of infected cells. Bacterivory is absent in ponds
above about 20% salinity, while viruses begin to be detectable at
salinities above 15% (Pedros-Alio et al., 2000). Viral lysis is
estimated to affect 7% of the total population per day, significant
given the low doubling time of about 2 days for the in-situ prokaryotic
population.
Viruses present a possible problem with isolation in liquid media due
to the fact that viral loads are estimated at up to 10 times that of
the prokaryotic population. Hence, an extinction culture containing
only one cell may contain 10 times as many phage, some of which may
have the potential to lyse the cell. This possibility is increased when
the fact that the dominant organisms (and hence most likely to be at
the end-point of the dilution series) are most likely to be the hosts
for the largest phage populations.
The dominant organism, presumably responsible for a
significant part of the nutrient cycling in the environment, is a
square, flat and gas-vacuolated, bacteriorhodopsin containing archaeon
first described by Walsby in 1980 (Walsby, 1980). After 25 years of
attempts, it has recently been cultured as part of my doctorate (Burns
et al, 2004; Bolhuis et al, 2004).
By combining molecular analytical methods with newer cultivation
techniques, it may be possible to gain insight into the community
structure and culture a greater percentage of the population such that
most major groups are represented, as described by Burns et al, (2004b).
In particular, it is imperative that
the dominant microbial species present in a sample environment be
isolated and characterised if any meaningful analysis of the natural
ecology is to be made.
Cultivation of Haloarchaea
Please see here for an abstract of the paper describing this recent work. (pdf download available at the linked site)
Briefly, this work has demonstrated for the first time that it is
possible to cultivate all numerically-significant organisms from a real
environment - not just the ones that grow well in a laboratory. This
has major implications for microbial ecology, as for the first time we
can study both all of the organisms separately, as well as the
interactions these organisms have with each other.
As the dominance of each organism in the lakes is known, this opens up
the possibility of meaningful studies into the lake ecology to be
undertaken using these organisms, rather than guessing at lake ecology
using isolates which are not actually significant in the isolating
environment – an extremely common situation in microbial ecology at
present.
Haloarchaeal viruses - [this
subsection courtesy Kate Porter, Dyall-Smith laboratory, The University
of Melbourne]
[Further background information may also be found at my supervisor, Mike Dyall-Smith's, website here]
Viruses, which are dependant on their host cells for replication, must carefully regulate gene expression over the infection cycle. As a result, viruses are frequently utilised to study fundamental aspects of gene expression and regulation. In particular, the viruses of Archaea and Bacteria (bacteriophages) have proven to be extremely useful in the study of host genetics. The first archaeal virus was discovered in 1974 (Torsvik and Dundas, 1974) and since this, around 39 archaeal viruses and virus-like particles (VLPs) have been reported (http://www.ncbi.nlm.nih.gov/ICTV/; Dyall-Smith et al., 2003; Häring et al., 2004), a miniscule number compared with over 5,100 bacteriophages (Ackermann, 2001; Ackermann, 2003).
Archaeal viruses are known to infect two of the four phylogenetic
kingdoms (reviewed in Zillig et al., 1996; Ackermann, 2001; Ackermann,
2003). The viruses of Crenarchaeota are morphologically diverse,
belonging to at least five families: Fuselloviridae, “Globuloviridae”,
“Guttaviridae”, Lipothrixviridae and Rudiviridae
(http://www.ncbi.nlm.nih.gov/ICTV/; Arnold et al., 2000; Häring et al.,
2004). The viruses of Euryarchaeota are morphologically less
diverse, with the majority belonging to the families Myoviridae and
Siphoviridae, although one lemon-shaped virus and two lemon-shaped VLPs
are known (http://www.ncbi.nlm.nih.gov/ICTV/; Bath and Dyall-Smith,
1998; Geslin et al., 2003a). In addition, numerous VLPs of
Crenarchaeota and Euryarchaeota, displaying diverse morphologies, have
been observed in hot springs, hypersaline waters and deep-sea
hydrothermal vents (Oren et al., 1997; Dyall-Smith et al., 2003; Geslin
et al., 2003b; Prangishvili, 2003). Although archaeal virus
characterisation is still in its early stages, 19 genomes of archaeal
viruses and VLPs have been completely sequenced: 13 species
infecting Crenarchaeota and six infecting Euryarchaeota
(http://www.ncbi.nlm.nih.gov/genomes/VIRUSES/viruses.html; Bath,
2004).
The first haloarchaeal virus (halovirus) was observed in a preparation of crudely purified Hbt. salinarum flagella (Torsvik and Dundas, 1974). Since this, 15 haloviruses have been isolated from numerous other sources (reviewed in Zillig et al., 1986; Zillig et al., 1988; Dyall-Smith et al., 2003). Hypersaline waters are an especially good source of haloviruses and VLPs, as they contain high VLP concentrations. In these environments, VLPs may outnumber cells by up to a factor of 9.5 (Oren et al., 1997). The VLPs observed in such environments are of a variety of morphologies, including lemon-shaped, polyhedral and head-and-tail (Oren et al., 1997; Geslin et al., 2003b). As hypersaline environments are, in general, devoid of protists that graze on prokaryotes, it seems probable that viruses are a major regulating factor of haloarchaeal populations. They may also play a significant role in mediating genetic transfer between cells.
Of the 15 halovirus isolates, most have head-and-tail morphologies and
are monovalent, infecting Halobacterium species, although the more
recent isolates infect members of the genera Haloarcula, Haloferax,
Halorubrum and Natrialba. All known haloviruses possess genomes
of linear, double-stranded (ds) DNA and are capable of lytic
multiplication within their hosts, although many haloviruses are able
to enter lysogenic state or form persistent infection. Halovirus
particles are generally sensitive to low salt concentrations, although
His1 and Hh1 can tolerate low salt media (Pauling, 1982; Bath and
Dyall-Smith, 1998) and fN retains infectivity even in distilled water
(Vogelsang-Wenke and Oesterhelt, 1988). It appears that haloviral
eclipse and latent periods and burst size may be regulated by the
external salt concentration of the medium, a phenomenon that has been
proposed to be significant for virus replication during changing
salinity conditions in the environment (Daniels and Wais, 1990).
Relatively few haloviruses have been studied in detail at the molecular
level. The most thoroughly studied are fH, which has had
extensive molecular characterisation (reviewed in Zillig et al., 1986;
Zillig et al., 1988), and HF1, HF2, fCh1 and His1, whose complete
genome sequences have been determined
(http://www.ncbi.nlm.nih.gov/genomes/VIRUSES/viruses.html; Bath,
2004). These five viruses have contributed greatly to archaeal
genetics and have been utilised in transfection (Cline and Doolittle,
1987; Bath, 2004), gene cloning and expression (Blaseio and Pfeifer,
1990) and identification of restriction-modification systems (Pauling,
1982; Daniels and Wais, 1984; Patterson and Pauling, 1985). The
genome sequences have revealed interesting relationships among
haloviruses and have demonstrated some links between archaeal viruses
and bacteriophages. fH and fCh1 display significant sequence
similarity, surprising as the viruses are from considerably different
environments and host ranges (Klein et al., 2002), whilst the HF1 and
HF2 genome sequences are remarkably similar to one another, suggesting
that the viruses only recently diverged and that the divergence was a
single, major recombination event (Dyall-Smith et al., 2003; Tang et
al., 2004). The halovirus sequences also show varying degrees of
resemblance to bacteriophages in genome organisation and replication
strategy and in some cases there is significant gene sequence
similarity. This suggests that there has been horizontal transfer
between the prokaryotic viruses, or that there was a common ancestor of
viruses prior to the split between Archaea and Bacteria (Tang et al.,
2002; Klein et al., 2002; Tang et al., 2004; Bath, 2004).
In addition to the haloviruses identified in the literature, this
laboratory has isolated nine novel haloviruses from Australian
hypersaline waters (Bath, 1995; Walker, 1999; Dyall-Smith et al.,
2003). Eight of these haloviruses were isolated in 1998 by
plating hypersaline water samples directly on lawns of Haloarcula
hispanica, Halorubrum coriense and Haloferax volcanii (Walker,
1999). In initial studies, two of the viruses infecting Har.
hispanica (designated PH1 and SH1) were revealed to possess a spherical
morphology, which had previously been unobserved in euryarchaeal
viruses (Walker, 1999; Seah, 2000; Porter, 2003).
Preliminary studies suggested that these two spherical viruses could be related to one another and possess an internal lipid membrane (Walker, 1999; Seah, 2000; Porter, 2003). This virion architecture has been observed in many other viruses, including bacteriophages, such as PRD1 (Abrescia et al., 2004; Cockburn et al., 2004), eukaryotic viruses, such as adenovirus, and, recently, the archaeal virus STIV (Rice et al., 2004), suggesting a structural relationship between viruses from all three domains of life (Benson et al., 2004). Several of these viruses also share a common replication system, which has only recently been observed in archaeal viruses (Bath, 2004).
References - General
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Burns, D.G., Camakaris, H.M., Janssen, P.H. and Dyall-Smith, M. (2004b) Combined use of cultivation-dependent and cultivation-independent methods indicates that members of most haloarchaeal groups in an Australian crystalliser pond are cultivable. Appl. Environ. Microbiol. 70(9): 5258-5265.
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