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will have to be performed on Oval Lake, as a single surface water measurement is not sufficient to understand the complex chemistry of its circulating mixolimnion. Ice Cover (thickness & Salinity Tempera Nitrate Nitrite Ammoniu SRP DOC Chi a Lake percentage) (p t ture °C m (pg L"' (pg L (m g LL-1) (pg L' Pendant , Lake 1.5m, 100% 12 0.5 0 3.44 5.9 17.96 3.045 0.243 Ace Lake 1.2m, 100% 14 Oval Lake Nr, 85% 34 -0.9 0 3.84 1.39 52.5 1.079 0.74 -1.9 0 5.41 0.89 52.45 10.607 0.95 Triple Lake 0% 136 3.4 0 7.22 6.69 12.17 38.676 1.68 Table 3.3 - Comparison of the major recorded physico-chemical factors for the lakes from which AFP active bacteria were isolated. All measurements are from Om during the summer. This allows comparison between the lakes because Oval Lake was only sampled at Om.. \"r - not recorded 3.4 - Conclusions Only four of the lakes were shown to contain AFP active bacteria within their biota - Pendant Lake, Ace Lake, Oval Lake and Triple Lake (refer to Chapter 4). Table 3.2 outlines the differences between these four lakes. However, apart from the two meromictic lakes (Ace Lake and Oval Lake), there were very few similarities between them; they have different salinities, stratification types and inorganic / organic chemical concentrations. Ace Lake is a meromictic, saline lake. Its meromixis induces a very interesting water chemistry profile. The bacterial populations within the lake were zoned due to the permanent stratification. The mixolimnion appears to have lower concentrations of ammonium and DOC and a higher SRP concentration than Pendant Lake or Triple Lake, possibly due to meromixis. Oval Lake is also a meromictic, saline lake. Only a surface water sample was collected from the lake during the summer, so there was a lack of information regarding the physico-chemical characteristics of the water column. However, Oval Lake had a moderately high salinity and low ammonium concentrations, with high DOC and chlorophyll a concentrations. As observed in Ace Lake, SRP was also relatively abundant compared to Pendant Lake and Triple Lake. 112
Pendant Lake is an unstratified, saline lake. It had a similar salinity to Ace Lake but generally had higher primary production, and hence a more abundant biota. It had a small anoxic sump at the bottom of the lake. Triple Lake is a shallow hypersaline holomictic lake. It had moderately high bacterial and flagellate abundance due to high nutrient concentrations which were higher than Ace Lake or Pendant Lake, probably due to low levels of biotic degradation and therefore accumulation. Deep Lake and Club Lake were not shown to have AFP active bacteria in their bacterial populations, but were part of the detailed study and so are still summarised here. They had similar surface water environments; they were both extremely hypersaline and had high nutrient concentrations, which suggests that nutrient levels did not inhibit biological activity within the lakes. Biological activity during the summer period indicated that some organisms were capable of surviving the high salinity. However, for about 9 months of the year the surface water temperature reached approximately -14°C - this is thought to be the main inhibitory factor to life in the lakes. 113
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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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compiled using Seqman and any erron
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ecorded and related to the level of
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information regarding the cold adap
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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 and 126: a Bacterial abundance (x 106 1.1) 0
Page 127 and 128: 8 ö a N Ö oý L _> Q O O 4 0 rn O
Page 129 and 130: undoubtedly true of Club Lake. The
Page 131: suggested that input of bacteria an
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
Page 177 and 178: et al., 1994) and the Antarctic SIM
Page 179 and 180: Chapter 6: BACTERIAL COMMUNITY ANAL
Page 181 and 182: 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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