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Cyanobacterial community changes in sulfide biotopes of shallow coastal waters of the Baltic Sea

Identifieur interne : 000058 ( PascalFrancis/Curation ); précédent : 000057; suivant : 000059

Cyanobacterial community changes in sulfide biotopes of shallow coastal waters of the Baltic Sea

Auteurs : U. Fischer [Allemagne] ; J. Rethmeier [Allemagne] ; A. Rabenstein [Allemagne] ; A. Potthoff [Allemagne]

Source :

RBID : Pascal:00-0053703

Descripteurs français

English descriptors

Abstract

Two stations, Hiddensee (station I) and Boiensdorf (station II), of Baltic Sea shallow coastal waters which differ in sulfide concentration and salinity were examined with regard to changes in cyanobacterial community under the influence of sulfide between 1992 and 1994. High abundances of both heterocyst containing filamentous cyanobacteria (e.g. Nodularia) as well as unicellular forms (e.g. Merismopedia) were found at station I in the absence of sulfide in the water column. These groups of cyanobacteria decreased significantly with increasing sulfide concentration up to 4 mM during summer time. Simultaneously, a mass development of 4 gliding, filamentous cyanobacteria (Microcoleus chthonoplastes, Lyngbya aestuarii, Oscillatoria margaritifera and Oscillatoria sp.) occurred. These cyanobacteria exhibit a large tolerance for high sulfide concentrations and form mats of a few cm thickness. The ability to adapt to changing sulfide concentrations is species dependent. No sulfide was detected in the water of station II, where a large abundance of different cyanobacteria species was observed in summer without a mass development of a distinct species. A comparable development of the cyanobacterial coenosis and the occurrence of the same species were observed at both stations during fall and winter. Most of the isolated cyanobacteria oxidize sulfide phototrophically and stoichiometrically to thiosulfate with an intermediate formation of sulfite. Depending on environmental conditions, shifts in the physicochemical gradients (redox potential, oxygen, sulfide) occurrred in the sediments of both stations in the course of a year.
pA  
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A08 01  1  ENG  @1 Cyanobacterial community changes in sulfide biotopes of shallow coastal waters of the Baltic Sea
A09 01  1  ENG  @1 Marine Cyanobacteria
A11 01  1    @1 FISCHER (U.)
A11 02  1    @1 RETHMEIER (J.)
A11 03  1    @1 RABENSTEIN (A.)
A11 04  1    @1 POTTHOFF (A.)
A12 01  1    @1 CHARPY (Loïc) @9 ed.
A12 02  1    @1 LARKUM (A. W. D.) @9 ed.
A14 01      @1 Universität Bremen, Fachbereich 2 und Zentrum für Umweltforschung und Umwelttechnologie (UFT), Abt. Marine Mikrobiologie, Leobener Str. @2 28359 Bremen @3 DEU @Z 1 aut. @Z 2 aut. @Z 3 aut. @Z 4 aut.
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A15 02      @1 School of Biological Sciences, University of Sydney @2 Sydney, NSW 2006 @3 AUS @Z 2 aut.
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C01 01    ENG  @0 Two stations, Hiddensee (station I) and Boiensdorf (station II), of Baltic Sea shallow coastal waters which differ in sulfide concentration and salinity were examined with regard to changes in cyanobacterial community under the influence of sulfide between 1992 and 1994. High abundances of both heterocyst containing filamentous cyanobacteria (e.g. Nodularia) as well as unicellular forms (e.g. Merismopedia) were found at station I in the absence of sulfide in the water column. These groups of cyanobacteria decreased significantly with increasing sulfide concentration up to 4 mM during summer time. Simultaneously, a mass development of 4 gliding, filamentous cyanobacteria (Microcoleus chthonoplastes, Lyngbya aestuarii, Oscillatoria margaritifera and Oscillatoria sp.) occurred. These cyanobacteria exhibit a large tolerance for high sulfide concentrations and form mats of a few cm thickness. The ability to adapt to changing sulfide concentrations is species dependent. No sulfide was detected in the water of station II, where a large abundance of different cyanobacteria species was observed in summer without a mass development of a distinct species. A comparable development of the cyanobacterial coenosis and the occurrence of the same species were observed at both stations during fall and winter. Most of the isolated cyanobacteria oxidize sulfide phototrophically and stoichiometrically to thiosulfate with an intermediate formation of sulfite. Depending on environmental conditions, shifts in the physicochemical gradients (redox potential, oxygen, sulfide) occurrred in the sediments of both stations in the course of a year.
C02 01  X    @0 002A14C02
C03 01  X  FRE  @0 Cyanobacteria @2 NS @5 01
C03 01  X  ENG  @0 Cyanobacteria @2 NS @5 01
C03 01  X  SPA  @0 Cyanobacteria @2 NS @5 01
C03 02  X  FRE  @0 Communauté microbienne @5 02
C03 02  X  ENG  @0 Microbial community @5 02
C03 02  X  SPA  @0 Comunidad microbiana @5 02
C03 03  X  FRE  @0 Structure population @5 03
C03 03  X  ENG  @0 Population structure @5 03
C03 03  X  SPA  @0 Estructura población @5 03
C03 04  X  FRE  @0 Densité population @5 04
C03 04  X  ENG  @0 Population density @5 04
C03 04  X  SPA  @0 Densidad población @5 04
C03 05  X  FRE  @0 Variation saisonnière @5 05
C03 05  X  ENG  @0 Seasonal variation @5 05
C03 05  X  SPA  @0 Variación estacional @5 05
C03 06  X  FRE  @0 Adaptation @5 06
C03 06  X  ENG  @0 Adaptation @5 06
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C03 07  X  FRE  @0 Facteur milieu @5 09
C03 07  X  ENG  @0 Environmental factor @5 09
C03 07  X  SPA  @0 Factor medio @5 09
C03 08  X  FRE  @0 Sulfure @2 NA @5 10
C03 08  X  ENG  @0 Sulfides @2 NA @5 10
C03 08  X  SPA  @0 Sulfuro @2 NA @5 10
C03 09  X  FRE  @0 Sédiment marin @5 12
C03 09  X  ENG  @0 Marine sediments @5 12
C03 09  X  SPA  @0 Sedimento marino @5 12
C03 10  X  FRE  @0 Zone côtière @5 14
C03 10  X  ENG  @0 Coastal zone @5 14
C03 10  X  SPA  @0 Zona costera @5 14
C03 11  X  FRE  @0 Eau peu profonde @5 15
C03 11  X  ENG  @0 Shallow water @5 15
C03 11  X  SPA  @0 Agua poco profunda @5 15
C03 12  X  FRE  @0 Mer Baltique @2 NG @5 67
C03 12  X  ENG  @0 Baltic Sea @2 NG @5 67
C03 12  X  SPA  @0 Mar Báltico @2 NG @5 67
C07 01  X  FRE  @0 Bactérie
C07 01  X  ENG  @0 Bacteria
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C07 02  X  SPA  @0 Medio marino @5 43
N21       @1 038

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Pascal:00-0053703

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<div type="abstract" xml:lang="en">Two stations, Hiddensee (station I) and Boiensdorf (station II), of Baltic Sea shallow coastal waters which differ in sulfide concentration and salinity were examined with regard to changes in cyanobacterial community under the influence of sulfide between 1992 and 1994. High abundances of both heterocyst containing filamentous cyanobacteria (e.g. Nodularia) as well as unicellular forms (e.g. Merismopedia) were found at station I in the absence of sulfide in the water column. These groups of cyanobacteria decreased significantly with increasing sulfide concentration up to 4 mM during summer time. Simultaneously, a mass development of 4 gliding, filamentous cyanobacteria (Microcoleus chthonoplastes, Lyngbya aestuarii, Oscillatoria margaritifera and Oscillatoria sp.) occurred. These cyanobacteria exhibit a large tolerance for high sulfide concentrations and form mats of a few cm thickness. The ability to adapt to changing sulfide concentrations is species dependent. No sulfide was detected in the water of station II, where a large abundance of different cyanobacteria species was observed in summer without a mass development of a distinct species. A comparable development of the cyanobacterial coenosis and the occurrence of the same species were observed at both stations during fall and winter. Most of the isolated cyanobacteria oxidize sulfide phototrophically and stoichiometrically to thiosulfate with an intermediate formation of sulfite. Depending on environmental conditions, shifts in the physicochemical gradients (redox potential, oxygen, sulfide) occurrred in the sediments of both stations in the course of a year.</div>
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<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA">
<s0>Variación estacional</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE">
<s0>Adaptation</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG">
<s0>Adaptation</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA">
<s0>Adaptación</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE">
<s0>Facteur milieu</s0>
<s5>09</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG">
<s0>Environmental factor</s0>
<s5>09</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA">
<s0>Factor medio</s0>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE">
<s0>Sulfure</s0>
<s2>NA</s2>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG">
<s0>Sulfides</s0>
<s2>NA</s2>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA">
<s0>Sulfuro</s0>
<s2>NA</s2>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE">
<s0>Sédiment marin</s0>
<s5>12</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG">
<s0>Marine sediments</s0>
<s5>12</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA">
<s0>Sedimento marino</s0>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE">
<s0>Zone côtière</s0>
<s5>14</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG">
<s0>Coastal zone</s0>
<s5>14</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA">
<s0>Zona costera</s0>
<s5>14</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE">
<s0>Eau peu profonde</s0>
<s5>15</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG">
<s0>Shallow water</s0>
<s5>15</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA">
<s0>Agua poco profunda</s0>
<s5>15</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE">
<s0>Mer Baltique</s0>
<s2>NG</s2>
<s5>67</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG">
<s0>Baltic Sea</s0>
<s2>NG</s2>
<s5>67</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA">
<s0>Mar Báltico</s0>
<s2>NG</s2>
<s5>67</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE">
<s0>Bactérie</s0>
</fC07>
<fC07 i1="01" i2="X" l="ENG">
<s0>Bacteria</s0>
</fC07>
<fC07 i1="01" i2="X" l="SPA">
<s0>Bacteria</s0>
</fC07>
<fC07 i1="02" i2="X" l="FRE">
<s0>Milieu marin</s0>
<s5>43</s5>
</fC07>
<fC07 i1="02" i2="X" l="ENG">
<s0>Marine environment</s0>
<s5>43</s5>
</fC07>
<fC07 i1="02" i2="X" l="SPA">
<s0>Medio marino</s0>
<s5>43</s5>
</fC07>
<fN21>
<s1>038</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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