The Vertical Migratory Rhythm of Intertidal Microphytobenthos in Sediment Depends on the Light Photoperiod, Intensity, and Spectrum: Evidence for a Positive Effect of Blue Wavelengths
Abstract:Barnett et al. Intertidal Microphytobenthos Light-Dependent Rhythmic Migration MPB surface accumulation, as compared to other wavelengths (white, green, and red) in patterns that were intensity-dependent and species-dependent. In particular, we found two species, Navicula spartinetensis and Gyrosigma fasciola, which strongly migrate up under blue light and could potentially be used as model species for further studying the light-responses of intertidal MPB.
“…Instead, in our conditions, MPB abundance at the surface of sediment indicated by Ft went on varying at the function of photoperiod (and probably of the tidal cycle), with striking increase of Ft before day starts (Fig. 1) as previously reported before (Consalvey et al 2004;Barnett et al 2020). It was consistent with the observation of Staats et al (2000) that in situ patterns of diuron-treated-MPB vertical migration in the dark did not differ from those exposed to light during 24 h field experiment on mudflat surface.…”
Section: Indirect Effect Of Diuron On Mpb Photosynthesis Inhibitionsupporting
confidence: 59%
“…Physiological photoprotection mainly depends on distinct xanthophyll pigments, diadinoxanthin and diatoxanthin, which support the dissipation of excessive light energy (the so-called non-photochemical quenching process) and protect PSII reaction centres (Barnett et al, 2015;Cartaxana et al, 2016;Frankenbach et al, 2018;Pniewski and Piasecka-Jędrzejak, 2020). Behavioural photoprotection is realized through the vertical migration of MPB within the uppermost layers of sediment, by which motile diatoms position themselves at suitable depth for optimal light conditions (Consalvey et al 2004;Barnett et al, 2020).…”
Section: Mpb Shows High Photosynthetic Capacity and Efficient Protection Against Photoinhibitionmentioning
The effects of herbicide diuron on photosynthesis and vertical migration of intertidal microphytobenthos (MPB) assemblages were investigated using chlorophyll fluorometry. The results shown diuron ≤ 60 μgꞏL -1 had no obvious effect on MPB vertical migration during 24 h indicated by consistent rhythm. Low concentration of 10 μgꞏL -1 diuron had no significant influence on MPB photosynthesis throughout, however, high concentrations of 40, 50, and 60 μgꞏL -1 had significant impacts exhibited by decreased parameters of maximum relative electron transport rate (rETRmax), maximal PS II quantum yield (Fv/Fm) and non-photochemical quenching (NPQ). For middle concentrations of 20 and 30 μgꞏL -1 , above decreased 3 parameters recovered sooner or later after 2 h or 16.5 h. Comparatively, rETRmax, Fv/Fm and NPQ are concentration dependent and more sensitive than other parameters in assessing diuron toxicity. This study revealed the potential of using MPB assemblages and chlorophyll fluorometry for rapid assessing diuron toxicity in coastal sediments.
“…Instead, in our conditions, MPB abundance at the surface of sediment indicated by Ft went on varying at the function of photoperiod (and probably of the tidal cycle), with striking increase of Ft before day starts (Fig. 1) as previously reported before (Consalvey et al 2004;Barnett et al 2020). It was consistent with the observation of Staats et al (2000) that in situ patterns of diuron-treated-MPB vertical migration in the dark did not differ from those exposed to light during 24 h field experiment on mudflat surface.…”
Section: Indirect Effect Of Diuron On Mpb Photosynthesis Inhibitionsupporting
confidence: 59%
“…Physiological photoprotection mainly depends on distinct xanthophyll pigments, diadinoxanthin and diatoxanthin, which support the dissipation of excessive light energy (the so-called non-photochemical quenching process) and protect PSII reaction centres (Barnett et al, 2015;Cartaxana et al, 2016;Frankenbach et al, 2018;Pniewski and Piasecka-Jędrzejak, 2020). Behavioural photoprotection is realized through the vertical migration of MPB within the uppermost layers of sediment, by which motile diatoms position themselves at suitable depth for optimal light conditions (Consalvey et al 2004;Barnett et al, 2020).…”
Section: Mpb Shows High Photosynthetic Capacity and Efficient Protection Against Photoinhibitionmentioning
The effects of herbicide diuron on photosynthesis and vertical migration of intertidal microphytobenthos (MPB) assemblages were investigated using chlorophyll fluorometry. The results shown diuron ≤ 60 μgꞏL -1 had no obvious effect on MPB vertical migration during 24 h indicated by consistent rhythm. Low concentration of 10 μgꞏL -1 diuron had no significant influence on MPB photosynthesis throughout, however, high concentrations of 40, 50, and 60 μgꞏL -1 had significant impacts exhibited by decreased parameters of maximum relative electron transport rate (rETRmax), maximal PS II quantum yield (Fv/Fm) and non-photochemical quenching (NPQ). For middle concentrations of 20 and 30 μgꞏL -1 , above decreased 3 parameters recovered sooner or later after 2 h or 16.5 h. Comparatively, rETRmax, Fv/Fm and NPQ are concentration dependent and more sensitive than other parameters in assessing diuron toxicity. This study revealed the potential of using MPB assemblages and chlorophyll fluorometry for rapid assessing diuron toxicity in coastal sediments.
“…Such a migration scheme in the GPP algorithm was set according to the observation of the progressive superficial sediment covering by MPB during emersion at our study site (Herlory et al, 2004). However, the migration speed can be faster [a few minutes; see Méléder et al (2003b)] or slower [one hour; see Paterson et al (1998)], and it is mainly controlled by the tidal cycle and the light climate and spectral quality (Pinckney and Zingmark, 1991;Spilmont et al, 2007;Coelho et al, 2011;Barnett et al, 2020;Prins et al, 2020), but also by temperature (Cohn et al, 2003), nutrient availability in the sub-surface of sediment (Kingston, 2002), and desiccation (Coelho et al, 2009). Currently, the GPP-algorithm does not include the short-term variations of MPB photosynthetically active biomass at the sediment surface (i.e., "micro-migrations"), as it has been also observed some days/timings during our field campaigns.…”
Section: Ability Of the Gpp Algorithm To Map The Current Productive Smentioning
The gross primary production (GPP) of intertidal mudflat microphytobenthos supports important ecosystem services such as shoreline stabilization and food production, and it contributes to blue carbon. However, monitoring microphytobenthos GPP over a longterm and large spatial scale is rendered difficult by its high temporal and spatial variability. To overcome this issue, we developed an algorithm to map microphytobenthos GPP in which the following are coupled: (i) NDVI maps derived from high spatial resolution satellite images (SPOT6 or Pléiades), estimating the horizontal distribution of the microphytobenthos biomass; (ii) emersion time, photosynthetically active radiation (PAR), and mud surface temperature simulated from the physical model MARS-3D; (iii) photophysiological parameters retrieved from Production-irradiance (P-E) curves, obtained under controlled conditions of PAR and temperature, using benthic chambers, and expressing the production rate into mg C h −1 m −2 ndvi −1. The productivity was directly calibrated to NDVI to be consistent with remote-sensing measurements of microphytobenthos biomass and was spatially upscaled using satellite-derived NDVI maps acquired at different seasons. The remotely sensed microphytobenthos GPP reasonably compared with in situ GPP measurements. It was highest in March with a daily production reaching 50.2 mg C m −2 d −1 , and lowest in July with a daily production of 22.3 mg C m −2 d −1. Our remote sensing algorithm is a new step in the perspective of mapping microphytobenthos GPP over large mudflats to estimate its actual contribution to ecosystem functions, including blue carbon, from local and global scales.
“…In arid and semi-arid estuaries (Ridd and Stieglitz, 2002) or humid tropical supratidal zones with less fluvial contribution (Soares et al, 2017), HTF ecosystems cover an area that exceeds mangrove forests and occupy a substantial proportion of tropical intertidal zones. HTFs occupy the area just below the highest astronomical tides and are thus only flooded for short periods of the year (Ridd and Stieglitz, 2002;Bento et al, 2017). Evaporation, the flat topography and pronounced hydraulic deficit results in hypersaline conditions with salinity as high as 5 times that of seawater (Ridd and Stieglitz, 2002;Shen et al, 2018).…”
Section: Introductionmentioning
confidence: 99%
“…However, information on OC, nitrogen and phosphorus burial, and sediment CO 2 fluxes from these ecosystems remains scarce (e.g. Bento et al, 2017;Schile et al, 2017). Determining if HTFs are a source or sink of carbon is critical to understanding their importance and value in regards to climate change and coastal carbon sequestration (Lovelock and Duarte, 2019).…”
Abstract. Hypersaline tidal flats (HTFs) are coastal ecosystems with freshwater deficits often occurring in arid or semi-arid regions near mangrove supratidal zones with no major fluvial contributions. Here, we estimate that organic carbon (OC), total nitrogen (TN) and total phosphorus (TP) were buried at rates averaging 21 (±6), 1.7 (±0.3) and 1.4 (±0.3) gm-2yr-1, respectively, during the previous century in three contrasting HTF systems, one in Brazil (eutrophic) and two in Australia (oligotrophic). Although these rates are lower than those from nearby mangrove, saltmarsh and seagrass systems, the importance of HTFs as sinks for OC, TN and TP may be significant given their extensive coverage. Despite the measured short-term variability between net air–saltpan CO2 influx and emission estimates found during the dry and wet season in the Brazilian HTF, the only site with seasonal CO2 flux measurements, the OC sedimentary profiles over several decades suggest efficient OC burial at all sites. Indeed, the stable isotopes of OC and TN (δ13C and δ15N) along with C:N ratios show that microphytobenthos are the major source of the buried OC in these HTFs. Our findings highlight a previously unquantified carbon as well as a nutrient sink and suggest that coastal HTF ecosystems could be included in the emerging blue carbon framework.
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