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    Pfeiffer et al. (2012) Nature doi:10.1038/nature11586

    !"#$%&'($! #$ %&$' (&)( *+,)-./($0% 1)2(.3+) 2)/ (3)/%4$3( .,.2(3$/%$5.3 2./(+-.(.3 6+%()/2.%7

    )$&*+,- +($/('$0! 8+23$.,.2(3$6.%9 8$,.20,)3 (.2&/+:0.%9 ;($-+2

    ;

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    Bacterial Nanowires

    A+,,+ ,+D. %(302(03.% *$3 .,.2(3$/ (3)/%4$3(7

    E)5. 1../ $1%.35.6 +/ -)/= -.(), 3.602+/B 1)2(.3+)7 F./.3),,= %=/(&.(+G.6 +/ 2$/6+(+$/% $* )22.4($3 ,+-+()(+$/7

    @H)-4,.%! #$%&'()$* +,,-. /0$1'2$33' %2$45$2+4+ >),%$ +/

    2=)/$1)2(.3+) )/6 *.3-./(+/B 1)2(.3+)?

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    Gorby et al., (2006) PNAS 103(30): 1135811363

    Shewanella oneidensis under oxygen limitingconditions (electron acceptor)

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    Gorby et al., (2006) PNAS 103(30): 1135811363

    Shewanella oneidensis

    O2limitation No O2limitation

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    Gorby et al., (2006) PNAS 103(30): 1135811363

    Shewanella oneidensis in the presenceof ferrihydrite (reduced to magnetite)

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    Gorby et al., (2006) PNAS 103(30): 1135811363

    Synechocystis PCC 6803

    Methanothermobacterthermoautotrophicus

    Pelotomaculumthermopropionicum

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    7&+3'% 8+/%$ )'%/+-%+49 :78);

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    Pfeiffer et al. (2012) Nature doi:10.1038/nature11586

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    10

    Study Area

    Pfeiffer et al. (2012) Nature doi:10.1038/nature11586

    Marine sediment in Aarhus bay (Denmark)

    Laboratory experiments

    Background: Incubated sediment samples in which no match was found

    between electrochemical data and physicochemical gradients andzonation of

    potential metabolisms.

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    H2S

    Reduction of

    oxygen at the

    surface of the

    sediment

    Oxidation of H2S at

    deep layers in a

    completely anoxic

    environment

    Pic de pH(consum

    Filaments density:

    117 m cm3

    Cell length: 3 m

    Filament: 4x107

    cel/cm3

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    8$,.20,)3 I6./(+*+2)(+$/ $* (&. $1%.35.6 *+,)-./(%

    Deltaproteobacteria

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    O2

    H2S

    #&. %.6+-./( +% 20( +/($ ('$ 4+.2.%

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    O2

    H2S

    8+B3)(+$/ $* *+,)-./(% +/ (&. 5.3(+2), )H+% +% ,+-+(.6

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    Glass, non-conducting

    microspheres

    J&)( +* .,.2(3+2 2$/602(+5+(= +% 13$D./K

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    8+23$%2$4= $1%.35)(+$/% $* *+,)-./(%

    =

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    L)2(.3+), 3'%/+2)1,.% $4./M04 /.' :0.%(+$/% ($ 1. )/%'.3.6!

    E$' +% ./.3B= 2$/%.35.6 )/6 ),,$2)(.6 )-$/B 2.,,%K

    J&)( +% (&.+3 6+5.3%+(= >B./.(+2 )/6 -.()1$,+2?K

    J&)( +% (&. -$,.20,)3 1)%+% *$3 .,.2(3$/ (3)/%4$3(K

    ;3. (&.= '+6.%43.)6K

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    Pfeiffer et al. (2012) Nature doi:10.1038/nature11586