Impact of sediment grain-size and biofilm age on epipelic microphytobenthos resuspension

Intertidal zones are dynamic areas, where tidal currents and wind-induced waves are responsible of resuspension of the sediment and associated microphytobenthos (MPB). Sediment composition (mud–sand mixtures) and MPB biofilm age are two major components involved in resuspension of epipelic microphyt...

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Published inJournal of experimental marine biology and ecology Vol. 467; pp. 52 - 64
Main Authors Ubertini, Martin, Lefebvre, Sébastien, Rakotomalala, Christiane, Orvain, Francis
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.06.2015
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Abstract Intertidal zones are dynamic areas, where tidal currents and wind-induced waves are responsible of resuspension of the sediment and associated microphytobenthos (MPB). Sediment composition (mud–sand mixtures) and MPB biofilm age are two major components involved in resuspension of epipelic microphytobenthos in muddy areas. However, their relative role in resuspension phenomenon must be better understood in controlled conditions. In this study, three mud–sand mixtures (Pure mud M1, 75% mud/25% sand M2 and 50% mud/50% sand M3) were tested with an epipelic MPB biofilm of different ages (3, 6 and 9days after inoculum) using an erodimeter flume. The biofilm biomass, physiological state, photosynthetic parameters and Extracellular Polymeric Substances (EPS) were surveyed as well as water content and ammonium concentration in the sediment. Chl a content and Suspended Particular Inorganic Matter (SPiM) erodability differed between treatments, biofilm being able to be eroded before sediment when it is well constituted (especially in pure mud M1). Between day 3 and day 9 of culture, biofilm age did significantly affect critical thresholds for Chl a erosion and sediment resuspension for mud–sand mixtures (M2 and M3). Sediment resuspension seemed to be also driven by physical constraints like differential compaction and vertical sand segregation as a function of mud content. Indeed, grain-size was the main factor involved in MPB resuspension phenomenon, with an optimum reached near a equilibrate ratio between mud and sand (50% mud–50% sand). Proteins of the EPS bound fraction (extracted with dowex resin) appeared to have a critical role in the pioneering stages of biofilm installation, allowing its formation in a less favorable environment caused by sand enrichment (mixtures M2 and M3). This effect of bound EPS must be mediated by an increasing cohesion and lowering sediment permeability. Carbohydrate content of the bound EPS fraction was directly related to the sediment (SPiM) erodability, independently from mixture type or biofilm age. •Three sand–mud mixtures were tested with a presence of an epipelic MPB biofilm.•Biofilm and sediment erodability differed between treatments.•Biofilm development stage did significantly affect critical thresholds.•EPS bound fraction proteins play a critical role in biofilm installation.•Exportation of MPB to the water column decreased as a function of sand enrichment.
AbstractList Intertidal zones are dynamic areas, where tidal currents and wind-induced waves are responsible of resuspension of the sediment and associated microphytobenthos (MPB). Sediment composition (mud–sand mixtures) and MPB biofilm age are two major components involved in resuspension of epipelic microphytobenthos in muddy areas. However, their relative role in resuspension phenomenon must be better understood in controlled conditions. In this study, three mud–sand mixtures (Pure mud M1, 75% mud/25% sand M2 and 50% mud/50% sand M3) were tested with an epipelic MPB biofilm of different ages (3, 6 and 9days after inoculum) using an erodimeter flume. The biofilm biomass, physiological state, photosynthetic parameters and Extracellular Polymeric Substances (EPS) were surveyed as well as water content and ammonium concentration in the sediment. Chl a content and Suspended Particular Inorganic Matter (SPiM) erodability differed between treatments, biofilm being able to be eroded before sediment when it is well constituted (especially in pure mud M1). Between day 3 and day 9 of culture, biofilm age did significantly affect critical thresholds for Chl a erosion and sediment resuspension for mud–sand mixtures (M2 and M3). Sediment resuspension seemed to be also driven by physical constraints like differential compaction and vertical sand segregation as a function of mud content. Indeed, grain-size was the main factor involved in MPB resuspension phenomenon, with an optimum reached near a equilibrate ratio between mud and sand (50% mud–50% sand). Proteins of the EPS bound fraction (extracted with dowex resin) appeared to have a critical role in the pioneering stages of biofilm installation, allowing its formation in a less favorable environment caused by sand enrichment (mixtures M2 and M3). This effect of bound EPS must be mediated by an increasing cohesion and lowering sediment permeability. Carbohydrate content of the bound EPS fraction was directly related to the sediment (SPiM) erodability, independently from mixture type or biofilm age.
Intertidal zones are dynamic areas, where tidal currents and wind-induced waves are responsible of resuspension of the sediment and associated microphytobenthos (MPB). Sediment composition (mud–sand mixtures) and MPB biofilm age are two major components involved in resuspension of epipelic microphytobenthos in muddy areas. However, their relative role in resuspension phenomenon must be better understood in controlled conditions. In this study, three mud–sand mixtures (Pure mud M1, 75% mud/25% sand M2 and 50% mud/50% sand M3) were tested with an epipelic MPB biofilm of different ages (3, 6 and 9days after inoculum) using an erodimeter flume. The biofilm biomass, physiological state, photosynthetic parameters and Extracellular Polymeric Substances (EPS) were surveyed as well as water content and ammonium concentration in the sediment. Chl a content and Suspended Particular Inorganic Matter (SPiM) erodability differed between treatments, biofilm being able to be eroded before sediment when it is well constituted (especially in pure mud M1). Between day 3 and day 9 of culture, biofilm age did significantly affect critical thresholds for Chl a erosion and sediment resuspension for mud–sand mixtures (M2 and M3). Sediment resuspension seemed to be also driven by physical constraints like differential compaction and vertical sand segregation as a function of mud content. Indeed, grain-size was the main factor involved in MPB resuspension phenomenon, with an optimum reached near a equilibrate ratio between mud and sand (50% mud–50% sand). Proteins of the EPS bound fraction (extracted with dowex resin) appeared to have a critical role in the pioneering stages of biofilm installation, allowing its formation in a less favorable environment caused by sand enrichment (mixtures M2 and M3). This effect of bound EPS must be mediated by an increasing cohesion and lowering sediment permeability. Carbohydrate content of the bound EPS fraction was directly related to the sediment (SPiM) erodability, independently from mixture type or biofilm age. •Three sand–mud mixtures were tested with a presence of an epipelic MPB biofilm.•Biofilm and sediment erodability differed between treatments.•Biofilm development stage did significantly affect critical thresholds.•EPS bound fraction proteins play a critical role in biofilm installation.•Exportation of MPB to the water column decreased as a function of sand enrichment.
Author Lefebvre, Sébastien
Rakotomalala, Christiane
Orvain, Francis
Ubertini, Martin
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  fullname: Ubertini, Martin
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  organization: Université de Caen Basse-Normandie, UMR BOREA “Biologie des ORganismes et Ecosystèmes Aquatiques” (MNHN, UPMC, UCBN, CNRS-7208, IRD-207), Caen, France
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  givenname: Sébastien
  surname: Lefebvre
  fullname: Lefebvre, Sébastien
  organization: Université de Lille1, UMR CNRS 8187 LOG “Laboratoire d'Océanologie et Géosciences”, Station Marine de Wimereux, Wimereux, France
– sequence: 3
  givenname: Christiane
  surname: Rakotomalala
  fullname: Rakotomalala, Christiane
  organization: Université de Caen Basse-Normandie, UMR BOREA “Biologie des ORganismes et Ecosystèmes Aquatiques” (MNHN, UPMC, UCBN, CNRS-7208, IRD-207), Caen, France
– sequence: 4
  givenname: Francis
  surname: Orvain
  fullname: Orvain, Francis
  organization: Université de Caen Basse-Normandie, UMR BOREA “Biologie des ORganismes et Ecosystèmes Aquatiques” (MNHN, UPMC, UCBN, CNRS-7208, IRD-207), Caen, France
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Keywords Erodimeter
Substances
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Biofilm
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Microphytobenthos
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SSID ssj0001526
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Snippet Intertidal zones are dynamic areas, where tidal currents and wind-induced waves are responsible of resuspension of the sediment and associated...
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StartPage 52
SubjectTerms Biofilm
biomass
carbohydrate content
chlorophyll
cohesion
Erodimeter
Extracellular polymeric
inoculum
littoral zone
Marine
Microphytobenthos
permeability
photosynthesis
physiological state
proteins
Resuspension
sand
Sediment
Substances
tides
water content
Title Impact of sediment grain-size and biofilm age on epipelic microphytobenthos resuspension
URI https://dx.doi.org/10.1016/j.jembe.2015.02.007
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https://www.proquest.com/docview/2000256379
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