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3.3.2.4 - Deep Lake and Club Lake Both Deep Lake and Club Lake are hyper-saline (246ppt & 231 ppt respectively (Fig 3.3a & b)). Only exceptionally halotolerant bacterial species can survive in these lakes (Hand, 1980; Ferris & Burton, 1988; McMeekin & Franzmann, 1988), therefore most propagules brought into the lakes by wind, melt streams or animal deposits will die immediately. Several desiccated penguin carcasses are to be found on the western most beach of Deep Lake, therefore penguins do travel to the lake, albeit infrequently. The majority of Deep Lake is too cold and too saline to support life (- -15°C below 15m throughout the year (Kerry et al., 1977)), however, the top lm of the lake has suitable temperatures during the summer to support bacterial growth (--+3°C) (McMeekin & Franzmann, 1988). Therefore, the surface water was ideal for bacterial isolation. Fourteen bacterial isolates were cultured from Deep Lake throughout the sampling season (Chapter 4). Eleven of the 14 isolates cultured from Deep Lake were from summer samples when the surface water was relatively warm (Fig 3.3a). One bacterium was isolated during July, none during September and then three during November when surface water began to warm again. Fifteen bacteria were isolated from Club Lake (Chapter 4). Eleven of these isolates were cultured from summer samples as with Deep Lake. This suggests that low temperature, not high salinity is the main inhibitory factor for bacterial growth in the hypersaline lakes (Ferris & Burton, 1988). However, attempts to culture bacteria from Deep and Club Lake water samples on solid media at the same salinity as the lake water itself were not effective. Subsequent attempts to culture bacteria in liquid enriched media (nutrient broth) using Deep Lake water at varying concentrations (100%, 50% and 25% of original 246ppt sterilized and GF/F filtered lake water) proved negative. Hand (1980) also showed that bacteria could not be cultured in vitro from Deep Lake if the salinity of the media was more than half of the lake itself. Of course the numbers of bacterial isolates found from direct culturing may not represent the entire bacterial assemblage. As has been suggested previously (Muy'zer et al., 1993, Amann et al., 1995; Hugenholtz & Pace, 1996. Hugenholtz et al.. 1998), it is estimated that >99% of bacteria in the environment are not cultivatable using traditional techniques. Attempts were made to address this problem by looking at community' profiles for 16s rDNA DGGE-PCR (Chapter 6). 106
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COLD ADAPTATION STRATEGIES AND DIVE
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, 71 "If you march your Winter Jour
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1.6.3. Molecular typing techniques
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3.2.1.2.3. DOC and chlorophyll a ..
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5.3.2.5. The Sphingomonas group, is
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LIST OF FIGURES Figure I. I. Diagra
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Figure 3.17a Mean bacterial abundan
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LIST OF TABLES Table 1.1. Types of
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List of Abbreviations AFP AFGP AFLP
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ACKNOWLEDGEMENTS This study was fun
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Chapter 1: INTRODUCTION 1.1 - Tempe
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1999 ; Hand & Burton, 1981) or iden
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Cold adaptation is dependant on the
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not at 25°C is a function of the a
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The most prolific literature on col
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process known as thermal hysteresis
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dominant, role in the ice-growth in
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explanation for this diversity is t
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1.5.3.5 - Membrane bound solute tra
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een well established (Russell & Nic
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& Bowman, 2001; Labrenz & Hirsch, 2
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The reaction mix contains both deox
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gene mixtures and hence can be used
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displaying a high number of common
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AACGTCGAAA AACCTCGAAA (Organism A)
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particular set of environmental par
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Lake Maximum Depth (m) Approximate
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Larsemann Hills __ rp3rtrnent of th
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Sampling trips took two days during
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Sigma, Sigma-Aldrich Company Ltd.,
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oxidized and the sample then conver
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sample. An appropriate volume was l
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min to ensure complete extension of
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Figure 2.3 - Lane delineation image
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Figure 2.6b - Molecular weights are
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RNA 41F (5'-GCT CAG ATT GAA CGC TGG
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I min. The spin column was removed
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Page 79 and 80: information regarding the cold adap
Page 81 and 82: 50ppt to 186ppt. Thirteen were sali
Page 83 and 84: M N N 't M M \p \p 00 kf) M kf) bA
Page 85 and 86: as would normally be expected, as b
Page 87 and 88: 1444 6ý L CC vý O Q O O NO u 'c z
Page 89 and 90: 5 - 250 3 245 240 G (, -3 235 a 0-
Page 91 and 92: 3.2.2.2.5 - Dissolved organic carbo
Page 93 and 94: d 14 12 10 14 12 7 10 8 6 4 2 0 00/
Page 95 and 96: SRP ('g L- 05 10 15 20 2 3 Depth4 5
Page 97 and 98: 3.2.2.3 - Biological characteristic
Page 99 and 100: a 0 Bacterial Abundance (x 106 ml-1
Page 101 and 102: 3.3 - Discussion 3.3.1 - Summer sam
Page 103 and 104: to high surface water temperatures
Page 105 and 106: chemocline (Rankin et al., 1999). M
Page 107 and 108: a 250 200 150 100 50 70 60 50 40 ý
Page 109 and 110: The temperature (Fig 3.2a) through
Page 111 and 112: et al., 1999). No melt out was obse
Page 113 and 114: increase in ammonium is probably du
Page 115 and 116: 10 7 9 6 8 E ö 7 5 Co u c m c 40 w
Page 117 and 118: main pigments were chlorophylls a a
Page 119 and 120: Inorganic nitrogen (NO2, NO3 and NH
Page 121 and 122: 744 -- 7 644 6 19 ü SE 400-- 4 2s
Page 123 and 124: salinity decreased from July to Sep
Page 125: a Bacterial abundance (x 106 1.1) 0
Page 129 and 130: undoubtedly true of Club Lake. The
Page 131 and 132: suggested that input of bacteria an
Page 133 and 134: Pendant Lake is an unstratified, sa
Page 135 and 136: non-AFP active peptides from inhibi
Page 137 and 138: . ter rý :. 'ý Figure 4.2 -Fryka
Page 139 and 140: -ý- ---- ,. r. __-_-. ___. r. ýý
Page 141 and 142: 4.2 - Results 4.2.1 - Sampling and
Page 143 and 144: SPLAT score. It has been shown that
Page 145 and 146: 3'E t ý _d M! .PJ r rn 15 3.5 4 3
Page 147 and 148: 4.3 - Discussion Of the 866 bacteri
Page 149 and 150: arisen in very few species due to c
Page 151 and 152: Chapter 5: BACTERIAL MOLECULAR TYPI
Page 153 and 154: Fig 5.1 - Photographs of ARDRA gel
Page 155 and 156: Coefficient: Dice Algorithm: lPGMAA
Page 157 and 158: The closest published relative for
Page 159 and 160: identification was made based on 15
Page 161 and 162: Isolate number Closest phylogenetic
Page 163 and 164: e included due to its small sequenc
Page 165 and 166: 5.3.2 - Identification of the AFP a
Page 167 and 168: explains the fluctuation in related
Page 169 and 170: contamination was lower as the PCR
Page 171 and 172: seen to a certain extent in the ARD
Page 173 and 174: American Type Culture Collection (A
Page 175 and 176: Phylogenetic cluster alignment of t
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et al., 1994) and the Antarctic SIM
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Chapter 6: BACTERIAL COMMUNITY ANAL
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6.2.1 - Detection of AFP active iso
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using the same PCR protocol as orig
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Figure 6.1 - Denaturing gradient ge
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6.2.2 - Temporal and spatial variat
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Figure 6.4c - Gel I image showing b
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Coefficient: Dice Algorithm: UPGMA
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etween Om and 2m was obviously the
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All PCR-based rRNA molecular techni
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6.3.2.3 - Cellular lysis and DNA pu
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hybrids should be equal. However, S
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contain contaminants. If the profil
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(Section 6.3.2.4.3 ) could not be r
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most dominant species in the commun
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study was characterised as M protea
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11 species) showed AFP activity. Th
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that AFP activity could have evolve
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7.2 - Future Work The 19 AFP active
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REFERENCES ABYZOV, S. S. (1993). Mi
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BELL, E. M. and LAYBOURN-PARRY, J.
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Symposium on Environmental Biogeoch
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Research. 5,477-493. CLESCERI, L. S
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DRICKAMER, K. (1999). C-type lectin
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antifreeze proteins from Atlantic s
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FRANZMANN, P. D. and DOBSON, S. J.
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GRIFFITH, M., ALA, P., YANG. D. S.
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IVANOVA, E. P., KIPRIANOVA, E. A.,
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Antarctic Ecosystems. G. A. Llano (
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Howard-Williams and I. Hawes). Balk
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W. (1998). Rep-PCR-mediated genomic
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putida strains from Antarctica. Mic
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NICHOLS, D., BOWMAN, J., SANDERSON,
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PEARCE, D. A. and BUTLER, H. G. (20
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(1999). Palaeohydrological modellin
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tracers of biogeochemical processes
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R. G. Landes Company, Austin, Texas
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partial 16S rDNA sequencing. Applie
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YABUUCHI, E., WANG, L., ARAKAWA, M.
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APPENDICES Al. Media Tryptic Soya A
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"D C 'O I. .. r .. r 6 rr E , 4mo .
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. + + + I I I I I I + I + + I I I I
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Ö ON N M 1 O - N 'zt "o l'" 00 C N
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1 T 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1
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1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1
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1 1 1 1 I 1 + I I 1 I 1 1 I 1 1 1 I
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1 1 1 1 1 1 1 I I 1 I 1 I 1 1 I T I
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Cl M 'tt tn '. p t- 00 O\ N M O - (
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d' O - (N M 'nt V) \O N. 00 O> N M
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1 1 T 1 1 1 T 1 1 1 1 1 1 1 1 1 1 1
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+ + i i i i i i " i " . + + + + " +
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e O --ý N M t Vn 1,0 [-- 00 O> N M
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FT ce + I I r. to \, O t- 00 O\ N M
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kn 110 r- 00 Oý N M O - N M Itt vn
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, It N M "t N M Iýt N M M M M Oý
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gj a - - - - - - - - - - - - - - -
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