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1000 Titel
  • Diazotrophic Cyanobacteria are Associated With a Low Nitrate Resupply to Surface Waters in Lake Tanganyika
1000 Autor/in
  1. Ehrenfels, Benedikt |
  2. Bartosiewicz, Maciej |
  3. Mbonde, Athanasio Stephano |
  4. Baumann, Kathrin B.L. |
  5. Dinkel, Christian |
  6. Junker, Julian |
  7. Kamulali, Tumaini M. |
  8. Kimirei, Ismael A. |
  9. Niederdorfer, Robert |
  10. Odermatt, Daniel |
  11. Pomati, Francesco |
  12. Sweke, Emmanuel A. |
  13. Wehrli, Bernhard |
1000 Erscheinungsjahr 2021
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2021-07-23
1000 Erschienen in
1000 Quellenangabe
  • 9
1000 Copyrightjahr
  • 2021
1000 Embargo
  • 2022-01-25
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.3389/fenvs.2021.716765 |
1000 Publikationsstatus
1000 Abstract/Summary
  • <jats:p>In Lake Tanganyika, blooms of nitrogen-fixing (diazotrophic) cyanobacteria emerge, when the upper water column re-stratifies after a period of upwelling and convective mixing. During this seasonal transition, diazotrophic cyanobacteria exploit the abundant phosphate and fix nitrogen after other phytoplankton taxa have consumed the available nitrate. However, it remains less clear, which mechanisms favour diazotrophic cyanobacteria under more heavily stratified conditions with lower levels of excess phosphate and persistent nitrate-depletion. Here, we collected profiles of physicochemical parameters, nutrients and photo-pigments, as well as the medium- to large-sized phytoplankton community during two lake-wide cruises to elucidate to what extent the abundance of diazotrophic cyanobacteria in Lake Tanganyika may be controlled by the nitrate resupply through the thermocline into the euphotic zone. At stations where nitrate was depleted, but phosphate remained available near the surface, high densities of diazotrophic cyanobacteria were associated with a low nitrate supply to surface waters. Our data provide first support for two conceptual scenarios, where the relative position of the thermocline and the euphotic depth may create a functional niche for diazotrophic cyanobacteria: when the upward transport of nitrate into the euphotic zone is reduced by a subjacent thermocline, diazotrophic cyanobacteria, comprising <jats:italic>Dolichospermum</jats:italic> and <jats:italic>Anabaenopsis</jats:italic>, are key players in the medium-to large-sized phytoplankton community. By contrast, a thermocline located within the euphotic zone allows for a rapid vertical transport of nitrate for a thriving nitrate-assimilating phytoplankton community that evidently outcompetes diazotrophic cyanobacteria. This study highlights that, under nitrogen-depleted conditions, diazotrophic cyanobacteria can also grow in response to a reduced nutrient resupply to the productive surface waters.</jats:p>
1000 Sacherschließung
lokal phycoerythrin
lokal cyanobacterial blooms
lokal dolichospermum
lokal phycocyanin
lokal oligotrophic
lokal Environmental Science
lokal diazotrophs
lokal stratification
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/RWhyZW5mZWxzLCBCZW5lZGlrdA==|https://frl.publisso.de/adhoc/uri/QmFydG9zaWV3aWN6LCBNYWNpZWo=|https://frl.publisso.de/adhoc/uri/TWJvbmRlLCBBdGhhbmFzaW8gU3RlcGhhbm8=|https://frl.publisso.de/adhoc/uri/QmF1bWFubiwgS2F0aHJpbiBCLkwu|https://frl.publisso.de/adhoc/uri/RGlua2VsLCBDaHJpc3RpYW4=|https://frl.publisso.de/adhoc/uri/SnVua2VyLCBKdWxpYW4=|https://frl.publisso.de/adhoc/uri/S2FtdWxhbGksIFR1bWFpbmkgTS4=|https://frl.publisso.de/adhoc/uri/S2ltaXJlaSwgSXNtYWVsIEEu|https://frl.publisso.de/adhoc/uri/TmllZGVyZG9yZmVyLCBSb2JlcnQ=|https://frl.publisso.de/adhoc/uri/T2Rlcm1hdHQsIERhbmllbA==|https://frl.publisso.de/adhoc/uri/UG9tYXRpLCBGcmFuY2VzY28=|https://frl.publisso.de/adhoc/uri/U3dla2UsIEVtbWFudWVsIEEu|https://frl.publisso.de/adhoc/uri/V2VocmxpLCBCZXJuaGFyZA==
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  1. Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung |
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1000 Dateien
1000 Förderung
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    1000 Förderer Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung |
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1000 Objektart article
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1000 Erstellt am 2024-04-11T12:15:29.257+0200
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1000 Zuletzt bearbeitet 2024-05-07T13:29:18.342+0200
1000 Objekt bearb. Tue May 07 13:29:18 CEST 2024
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