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1000 Titel
  • Potential impacts of cable bacteria activity on hard-shelled benthic foraminifera: implications for their interpretation as bioindicators or paleoproxies
1000 Autor/in
  1. Daviray, Maxime |
  2. Geslin, Emmanuelle |
  3. Risgaard-Petersen, Nils |
  4. Scholz, Vincent V. |
  5. Fouet, Marie |
  6. Metzger, Edouard |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-02-20
1000 Erschienen in
1000 Quellenangabe
  • 21(4):911-928
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/bg-21-911-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Hard-shelled foraminifera are protists able to build a calcareous or agglutinated shell (called a “test”). Here we study the impact of sediment acidification on calcareous test preservation. For this study, sediment cores were sampled in the macrotidal Auray estuary located on the French Atlantic coast. Living and dead foraminifera were quantified until 5 cm depth and discriminated using the Cell-Tracker™ Green vital marker. The pH and oxygen profiles combined with quantitative polymerase chain reaction (qPCR) suggested that cable bacteria were most likely to cause the acidifying process. Cable bacteria (CB) are filamentous bacteria coupling sulfide oxidation to oxygen reduction over centimetre distances, generating a strong pH gradient within the first few centimetres of the sediment that could affect the microhabitats occupied by benthic foraminifera. On two different intertidal mudflats, volumetric filament densities have been estimated. They were comparable to those observed in the literature for coastal environments, with 7.4 ± 0.4 and 74.4 ± 5.0 m cm−3 per bulk sediment, respectively. Highly contrasting sediment acidification (from low to very intense) was described from 1.0 to 2.4 ΔpH. This seems to lead to various dissolution stages of the foraminiferal calcareous test from intact to fully dissolved tests revealing the organic lining. The dissolution scale is based on observations of living Ammonia spp. and Haynesina germanica specimens under a scanning electronic microscope. Furthermore, dead foraminiferal assemblages showed a strong calcareous test loss and an organic lining accumulation throughout depth under low pH, hampering the test preservation in deep sediment. These changes in both living and dead foraminiferal assemblages suggest that cable bacteria must be considered in ecological monitoring and historical studies using foraminifera as bioindicators and paleoenvironmental proxies. </jats:p>
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/RGF2aXJheSwgTWF4aW1l|https://frl.publisso.de/adhoc/uri/R2VzbGluLCBFbW1hbnVlbGxl|https://frl.publisso.de/adhoc/uri/UmlzZ2FhcmQtUGV0ZXJzZW4sIE5pbHM=|https://frl.publisso.de/adhoc/uri/U2Nob2x6LCBWaW5jZW50wqBWLg==|https://frl.publisso.de/adhoc/uri/Rm91ZXQsIE1hcmll|https://frl.publisso.de/adhoc/uri/TWV0emdlciwgRWRvdWFyZA==
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  • DeepGreen-ID: b8940dd5d66e48cf9a4f2787986c2ab2 ; metadata provieded by: DeepGreen (https://www.oa-deepgreen.de/api/v1/), LIVIVO search scope life sciences (http://z3950.zbmed.de:6210/livivo), Crossref Unified Resource API (https://api.crossref.org/swagger-ui/index.html), to.science.api (https://frl.publisso.de/), ZDB JSON-API (beta) (https://zeitschriftendatenbank.de/api/), lobid - Dateninfrastruktur für Bibliotheken (https://lobid.org/resources/search)
1000 Label
1000 Förderer
  1. Centre National de la Recherche Scientifique |
  2. Office Français de la Biodiversité |
1000 Fördernummer
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1000 Förderprogramm
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1000 Dateien
1000 Förderung
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    1000 Förderer Centre National de la Recherche Scientifique |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer Office Français de la Biodiversité |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 @id frl:6482241.rdf
1000 Erstellt am 2024-05-24T03:53:05.964+0200
1000 Erstellt von 322
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1000 Zuletzt bearbeitet 2024-05-27T11:03:42.326+0200
1000 Objekt bearb. Mon May 27 11:03:42 CEST 2024
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