75 research outputs found
Net community metabolism of a Posidonia oceanica meadow
We report a 12-yr data-set (August 2006 - October 2018) of nearly-continuous estimates (n=3275) of gross primary production (GPP), community respiration (CR), and net community production (NCP) in a Posidonia oceanica seagrass meadow, computed from O2 measurements on a mooring at 10 m bottom depth in the Bay of Revellata (Corsica). Both NCP and CR were correlated to GPP and followed the leaf biomass seasonal cycle. The meadow was net autotrophic (NCP of 23±8 mol O2 m-2 yr-1, GPP (83±16 mol O2 m-2 yr-1) > -CR (-60±9 mol O2 m-2 yr-1)), in agreement with oxygen over-saturation (104% at annual scale, 101% in winter and 109% in summer). Calcification (CAL) and CaCO3 dissolution (DIS) rates were evaluated from dissolved inorganic carbon measurements in benthic chamber incubations (August 2006-2009). The meadow was found to be a net sink of CaCO3 (DIS>CAL) at an annual rate of 7 mol CaCO3 m-2 yr-1 that matched estimates of CaCO3 deposition on the meadow by sedimentation from the water column. CAL from epiphyte coralline algae was correlated to GPP, but CAL:GPP ratio (0.1) was lower than reported for coralline algae in cultures (0.6) due to the additional contribution of Posidonia to GPP. Both NCP and net DIS contributed to an annual CO2 sink of -30 mol CO2 m-2 yr-1 distinctly stronger than the estimated net air-sea CO2 flux (-1 mol CO2 m-2 yr-1). This suggests that CO2 input by vertical mixing and/or transport by horizontal advection also strongly contribute to the net atmospheric CO2 exchange
Natural patches in Posidonia oceanica meadows: the seasonal biogeochemical pore water characteristics of two edge types
peer reviewedSeagrass meadows can be assimilated to seascape
matrixes encompassing a mosaic of natural and
anthropogenic patches. Natural patches within the Mediterranean
Posidonia oceanica meadows show a structural
particularity which consist in a duality of their edge types.
One edge is eroded by bottom currents, while the adjacent
meadow colonizes the bare sediments. This study aims to
study the dynamics of these two edges through the investigation
of the biogeochemistry (pH, total alkalinity, dissolved
inorganic carbon, CO2,
CH4,
N2O,
H2S,
dissolved
inorganic nitrogen, PO4
3−) within vegetated and unvegetated
sediments. These observations are compared with
the adjacent meadow to have a better understanding of the
colonization processes. Our results reveal that the P. oceanica
matrix shows differences from the vegetated edges of
sand patches, especially with regard to nutrient availability,
which is generally more important at the colonized edge
(dissolved inorganic nitrogen up to 65.39 μM in June). A
clear disparity also occurs between the eroded and colonized
edge with both a seasonal and bathymetrical variation of leaf
biomass with higher disparities at 10 m in June (colonized
edge 1415 gDW m−2; eroded edge 1133 gDW m−2). Themost important contrasts during this study were assessed in
June, suggesting that the warm period of the year is more
suitable for sampling to highlight disparate characteristics in
temperate seagrass meadows. These findings put into light
the potential importance of biogeochemical processes in
the dynamics of natural patch edges. We hypothesize that
they may influence the structural dynamics of P. oceanica
seascapes
Oxygen saturation, water temperature, gross primary production, community respiration, net community production, partial pressure of CO2 over a Posidonia oceanica meadow in the Bay of Revellata (2006-2018)
Table 1 : Oxygen saturation (%O2 in %), water temperature (°C) at 4.5 m, 7.0m and 9.0 m over a Posidonia oceanica meadow (seafloor depth =10 m) in the Bay of Revellata (Corsica) (42.580043°N 8.725148°E) from 06/08/2006 to 16/07/2018
Table 2 : Gross primary production (GPP), community respiration (CR), net community production (NCP) over a Posidonia oceanica meadow (seafloor depth =10 m) in the Bay of Revellata (Corsica) (42.580043°N 8.725148°E) from 06/08/2006 to 16/07/2018. The metabolic rates we derived from the mass balance of O2 (Table 1) based on the method of Odum (1956, Limnology and Oceanography 1: 102-117, https://doi.org/10.4319/lo.1956.1.2.0102)
Table 3: Partial pressure of CO2 (pCO2) in seawater over a Posidonia oceanica meadow (seafloor depth =10 m) in the Bay of Revellata (Corsica) (42.580043°N 8.725148°E) from 09-08-2006 to 20-08-2007.
Detailed methods are given by Champenois W & Borges AV (2021) Net community metabolism of a Posidonia oceanica meadow, Limnology and Oceanography, 66, 2021,2126–2140, https://doi.org/10.1002/lno.1172
First year of results from a mooring over a Posidonia Oceanica seagrass meadow (Corsica, France)
peer reviewe
A 15-month survey of Dimethylsulfoniopropionate and Dimethylsulfoxide content in Posidonia oceanica
Posidonia oceanica is the only reported seagrass to produce significant amount of
dimethylsulfoniopropionate (DMSP). It is also the largest known producer of DMSP
among coastal and inter-tidal higher plants. Here, we studied (i) the weekly to seasonal
variability and the depth variability of DMSP and its related compound dimethylsulfoxide
(DMSO) in P. oceanica leaves of a non-disturbed meadow in Corsica, France, (ii) the
weekly to seasonal variability and the depth variability of DMSP to DMSO concentration
to assess the potential of the DMSP:DMSO ratio as indicator of stress, and (iii)
the relationships between DMSP, DMSO, and the DMSP:DMSO ratio with potential
explanatory variables such as light, temperature, photosynthetic activity (effective
quantum yield of photosystem II), and leaf size. The overall average concentrations of
organosulfured compounds in P. oceanica leaves were 130 ± 39 µmol.g−1
fw for DMSP
and 4.9 ± 2.1 µmol.g−1
fw for DMSO. Concentrations of DMSP and DMSO in P. oceanica
were overall distinctly higher and exhibited a wider range of variations than other marine
primary producers such as Spartina alterniflora, phytoplankton communities, epilithic
Cyanobacteria and macroalgae. Concentrations of both DMSP and DMSO in P. oceanica
leaves decreased from a maximum in autumn to a minimum in summer; they changed
little with depth. Potential explanatory variables except the leaf size, i.e., the leaf age
were little or not related to measured concentrations. To explain the seasonal pattern
of decreasing concentrations with leaf aging, we hypothesized two putative protection
functions of DMSP in young leaves: antioxidant against reactive oxygen species and
predator-deterrent. The similar variation of the two molecule concentrations over time
and with depth suggested that DMSO content in P. oceanica leaves results from oxidation
of DMSP. The DMSP:DMSO ratio remained constant around a mean value of 29.2 ± 9.0
µmol:µmol for the non-disturbed harvested meadow regardless of the time of the
year, the depth or the leaf size. As suggested for the salt march plant S. alterniflora, we hypothesized the DMSP:DMSO ratio could be considered as indicator of stress in
seagrasses exposed to environmental or anthropogenic stressors. More research would
now be needed to confirm the functions of DMSP and DMSO in seagrasses and how
the DMSP:DMSO ratio will vary under various disturbances.FCT: 57/2016, UID/Multi/04326/2019.info:eu-repo/semantics/publishedVersio
Copper toxicity on coral holobiont photosynthetic processes
Copper (Cu), an essential micronutrient to organisms, may become toxic when present at too high environmental concentrations. This metal remains an aquatic contaminant of concern, notably because of its recent re-use as biocide in metal-based antifouling paints. The aim of this study was to monitor the physiological alterations in a zooxanthellate coral species and its endosymbionts (i.e. the coral holobiont) exposed to increasing Cu concentrations. Nubbins of Seriatopora hystrix were exposed for 8 days in 1 L intermittent respirometers to 5 nominal Cu concentrations: 0-2-5-15-50 ppb. Respirometers were maintained at 25.0±0.2°C with successive open/close cycles of 30 min. A 12/12 hours day-night light regime was applied with constant daylight intensity of 200 μmol photons m-2 s-1. Water renewal rate during the 30 min open cycles was 15 mL.min-1. The photosynthetic performances of coral endosymbionts were assessed daily with a fluorescence imaging system (imaging-PAM). At the end of the 8-days experiment, the maximal photochemical quantum yield (FV/FM) of coral nubbins had decreased by 12% and 38%, respectively, in the 15 ppb and 50 ppb treatments. This decrease was even greater for the effective photochemical quantum yield (ɸPSII) with values dropping by 41% and 54%, respectively. Cu exposure also affected the symbiosis between the coral host and its endosymbionts. Nubbins of the 15 ppb treatment slightly lightened from day 6, whilst nubbins exposed to the 50 ppb treatment lightened from day 3, and started to bleach from day 6. The analysis of nubbins' primary productivity did not coincide with the above observations, the oxygen production within each respirometer remaining relatively constant during the overall experiment for all treatments. This unexpected observation may be the sign of a compensation mechanism. In conclusion, Cu affected the photosynthetic processes of S. histrix within 8 days from relevant environmental concentrations of 15 ppb. The exposure of corals to toxic chemicals thus has to be considered as an additional stressor to, e.g., ocean acidification or elevated temperature, which may disturb their ecophysiology and lead to bleaching
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