We developed vector plasmids for the transformation of Halobacterium halobium, using the replicon region from the halobacterial phage OH or from' the plasmid pHHl together with a DNA fragment conferring resistance to mevinolin. H. halobium P03, a strain lacking pHHI as well as the restriction endonuclease activity found in wild-type H.halobium, was used as the recipient strain. AlR H. halobium fragments tested for autonomous replication as well as the Haloferax volcanii vector pWL102 enabled stable plasmid maintenance in this strain. A frequent loss of all vectors (including pWL102) was observed inHf. vokanfi, where >90% of the mevinolin-resistant colonies obtained after transformation had lost the vector, presumably because of restriction endonuclease activity and concomitant recombination of the mevinolin resistance marker with the chromosome. The expression of gas vesicle-encoding genes (vac) was analyzed by using a 4.5-kilobase-pair (kbp) (8), and the second replicon is derived from the endogenous 150-kbp plasmid pHH1 of H. halobium. A common region of4.3-kbp DNA was determined for all pHH1-type plasmids during the analysis of various deletion derivatives (9). One of the two smallest derivatives, pHH9 (5.7 kbp), is found as a major plasmid, whereas the other one, pHH8 (6.3 kbp), is always present at a 1:1 ratio together with the parental plasmid pHH4 (10).In this paper, we describe the transformation of various H. halobium strains as well as Hf. volcanii with plasmid constructs containing the Hf. volcanii mevinolin-resistance gene combined with these putative H. halobium replicons. As the first application, the smallest H. halobium vector, pUBP2, and the Hf. volcanii vector pWL102 were used to study gas vesicle synthesis. MATERIALS AND METHODS Materials

Investigation of the plasmid pHH4 in single colonies of Halobacterium halobium PHH4 indicated transposition of insertion elements in 20% of the colonies. Seven ISH27 insertions were observed as well as one ISH23 insertion. The various copies of ISH27 were compared to the two ISH27 elements already present in pHH4, and to the ISH27 element that was identified in the bacteriopsin (bop) gene of a Bop mutant. These ten copies of ISH27 constitute three types on the basis of DNA sequence identity: ISH27-1 (1398 bp), ISH27-2, and ISH27-3 (1389 bp each). The DNA sequence comparison between the three types indicates a region of 1200 bp where the identity between ISH27-1 and ISH27-2 or ISH27-3 is 82-83%. ISH27-2 and ISH27-3 are 95% identical in this region. The remaining region exhibits a lower DNA similarity (64-74% identity) between the different copies. An open reading frame of 1167 nucleotides spans the more conserved region, and a corresponding transcript could be detected in H. halobium PHH4, but not in H. halobium wild-type. ISH27-1 is 91% identical to members of the insertion sequence-like elements ISH51 of Haloferax volcanii, whereas the other two ISH27 element types are 82-83% identical to ISH51. The transposition 'burst' of ISH27 was only seen after storage of the cells for more than two years at 4 degrees C. Upon continuous cultivation at 37 degrees C no transposition event could be observed, suggesting that stress factor(s) might have caused the high transposition rate.

Deletion events occurring in the major 150-kilobase-pair (kb)

Deletion events that occur spontaneously in 36-kilobase-pair (kbp) plasmid pHH4 from the archaebacterium Halobacterium halobium were investigated. Four different deletion derivatives with sizes ranging from 5.7 to 17 kbp were isolated. Three of these deletion variants derived from pHH4 (pHH6 [17 kbp], pHH7 [16 kbpJ, and pHH8 [6.3 kbpJ), whereas the 5.7-kbp plasmid pHH9 derived from pHH6. Strains containing pHH6, pHH7, or pHH9 each lacked the parental plasmid pHH4, while pHH8 occurred at a 1:1 ratio together with p4H4. Common to all of these plasmids was the 5.7-kbp region of pHH9 DNA. The regions containing the fusion site in the deletion derivatives were investigated and compared with the corresponding area of the parental plasmid. Each deletion occurred exactly at the terminus of an insertion element. In pHH6 and pHH7, a halobacterial insertion element (ISH2) was located at the deletion site. The DNA fused to ISH2 displayed a 7-base-pair (bp) (pHH7) or 10-bp (pHH6) sequence homology to the inverted repeat of ISH2. In the two smaller plasmids, pHH8 and pHH9, an ISH27 element was located at the deletion site. Most likely, all of these smaller plasmids resulted from an intramolecular transposition event. The ISH27 insertion sequence contains a 16-bp terminal inverted repeat and duplicates 5 bp of target DNA during the transposition with the specificity 5'ANNNT3'. Four ISH27 copies were analyzed, and two ISH27 element types were identified that have approximately 85% sequence similarity. The ISH27 insertion elements constitute a family which is related to the ISH51 family characterized for H. volcanii, another halophilic archaebacterium.

Halobacterium halobium contains two gas vacuole protein genes that are located in plasmid pHH1 (p-vac) and in the chromosomal DNA (c-vac). The mutation frequency for these genes is different: the constitutively expressed p-vac gene is mutated with a frequency of 10(-2), while the chromosomal gene expressed in the stationary phase of growth is mutated with a frequency of 10(-5). The difference in the mutation susceptibility is due to the dynamics of plasmid pHH1. p-vac gene mutations are caused (i) by the integration of an insertion element or (ii) by a deletion event encompassing the p-vac gene region. In contrast, c-vac mutants analyzed to date incurred neither insertion elements nor deletions. Deletion events within pHH1 occur at high frequencies during the development of a H. halobium culture. The investigation of the fusion regions resulting from deletion events indicates that insertion elements are involved. The analysis of pHH1 deletion variants led to a 4 kilobase pair DNA region containing the origin of replication of the pHH1 plasmid.