Posidonia oceanica meadow: a low nutrient high chlorophyll (LNHC) system?
© Gobert et al; licensee BioMed Central Ltd. 2002
Received: 16 May 2002
Accepted: 21 August 2002
Published: 21 August 2002
In spite of very low nutrient concentrations in its vicinity – both column and pore waters-, the Posidonia oceanica of the Revellata Bay displays high biomass and productivity. We measured the nutrient fluxes from the sediment into the water enclosed among the leaf shoots ("canopy water") to determine if it is possible source of nutrients for P. oceanica leaves.
During the summer, the canopy water appears to act as a nutrient reservoir for the plant. During that period, the canopy water layer displays both a temperature 0.5°C cooler than the upper water column, and a much higher nutrient content, as shown in this work using a very simple original technique permitting to sample water with a minimal disturbance of the water column's vertical structure.
Despite low nutrient concentrations in pore water, mean net fluxes were measured from the sediment to the canopy water. These fluxes are sufficient to provide 20% of the mean daily nitrogen and phosphorus requirement of the P. oceanica shoots.
An internal cycling of nutrients from P. oceanica senescent leaves was previously noted as an efficient strategy to help face low nutrient availability. The present study points out a second strategy which consists in holding back, in the canopy, the nutrients released at the water-sediment interface. This process occurs when long leaves, during poor nutrient periods in the water column, providing, to P. oceanica, the possibility to develop, high biomass, high chlorophyll quantities in low nutrient environment (a Low Nutrients High Chlorophyll system).
Porewater nutrient concentrations Pore water nutrients in the sediment beneath meadows of different species (μmol L-1) (1ammonium data, 2nitrate data).
Recently, seagrasses have been shown to profit from mechanisms which diminish their dependence on the nutrient availability. One of these mechanisms appears to be related to the leaf longevity. An extended leaf longevity lowers the frequency of leaf formation and extends the time available to reclaim nutrients from mature leaves, thus reducing nutrient demands . In this regard, the high P. oceanica leaf longevity (345 days) appears to be an advantage compared to other seagrass species (mean leaf longevity: 88 days; range: 4–345 days).  report a nitrogen and phosphorus resorption efficiency of 20.4% and 21.9% in seagrasses. In P. oceanica, these resorption efficiencies have been estimated to 37% and 44% for nitrogen and phosphorus respectively by . In the Revellata Bay, the annual nitrogen requirements of P. oceanica are encountered by the leaves uptake for 25 to 45%, by the roots for 15 to 35% and by an internal recycling for 40% [11, 12]. This, while important, is however not sufficient to explain the high primary production regarding the low nutrient availability.
At variance with the HNLC regions (High-Nitrate, Low-Chlorophyll) encountered in the North and South Equatorial Pacific Ocean and in the Arctic  where standing stocks of phytoplankton remain low in spite of high nitrate and phosphate concentrations, the P. oceanica meadow of the Revellata Bay apparently behaves as a LNHC system (Low-Nutrient, High-Chlorophyll). The question then arises how P. oceanica meadows manage apparent very low nutrient availability to produce high quantities of living matter; for example the P. oceanica seagrass bed of the Revellata Bay displays a net primary production of about 230 gC m-2 year-1[5, 7].
These high biomass and production in spite of very low levels of nutrients (LNHC) in the vicinity of the seagrasses observed in Revelatta Bay correspond to the characteristics encountered in tropical zones [14, 15]. Nutrient fluxes have been estimated in a tropical zone meadow  and represent 0.53–1.56 gN m-2 year-1 and 0.14–0.42 gP m-2 year-1.
In this work, we have examined the nutrient conditions in the vicinity of the P. oceanica meadow of the Revellata Bay (pore water, canopy water and column water) and we have estimated the nutrient fluxes (nitrite+nitrate, ammonium and phosphate) from the sediment into the canopy using a benthic chamber. The results were used to evaluate the potential contribution of this source to meadow production.
The P. oceanica leaves and water canopy
The mean length of the leaves was 64.1 ± 18.8 cm (n = 43) and 18.0 ± 11.1 cm (n = 78) in June and October 1999 respectively. In June, the sediment was not visible through the canopy and the canopy water was 0.5°C cooler (n = 10) than in the upper water column. A typical visible water transition layer of a high temperature gradient was visually observable at this interface. In October, no temperature difference was observed between the canopy and column waters (n = 10) and the sediment was visible among the shoots. At the neighbouring of the study site, the shoot density was 415 ± 156 shoot m-2 (n = 20), measured in October 1999.
Nutrient fluxes Nitrite+nitrate, ammonium and orthophosphate fluxes (μmol m-2 day-1) calculated from results obtained in February, June and October 1997 with a benthic chamber and in June 1999 with a benthic cylinder settled in the P. oceanica meadow of the Revellata Bay at 10 m depth (mean ± standard deviation; number of observation into brackets).
-495 ± 573 (2)
-5700 ± 763 (2)
-1395 ± 1018 (2)
98 ± 81 (8)
-528 ± 547 (8)
-59 ± 243 (10)
-452 ± 423 (2)
133 ± 242 (8)
-862 ± 995 (8)
-77 ± 98 (8)
-60 ± 98 (8)
-2 ± 6 (8)
The P. oceanica leaves and water canopy
The P. oceanica meadow of the Revellata Bay at 10 m depth is to be considered a dense meadow according to . The mean length of the leaves of P. oceanica shoots is in good agreement with data obtained since 1975 at same periods of the year at 10 m depth [5, 6]. The seasonal variation between June and October 1999 corresponds to the annual leaf growth cycle: maximum lengths reached in June or July, decrease from August or September (related to a great appearance of necrosis on the tips) to December or January during heavy storms with a high proportion of leaf fall. From February on, the leaves length regularly increases (i.e.[5, 6]).
The sample collection tube system has permitted to point out the effect of the P. oceanica canopy on the nutrient distribution from the sediment to the column water. During the summer, when the leaves are long, the meadow forms a barrier enclosing the water and its nutrients in the canopy. The canopy water is a specific layer with measurable different chemical (nutrients) and physical (temperature) properties than the column water. During the winter, the leaves are shorter and the "barrier" effect of the canopy is diminished, furthermore higher currents associated with seasonal storms homogenised all the water column to the sediment. It is known that the seagrass canopies have the capacity to modify current velocity and waves [18, 19] causing a decrease in water movement on the sediment water interface and affecting nutrient fluxes from sediment to column water.
Our results about the nutrient fluxes, obtained with the benthic chamber, on the sandy small patches of the P. oceanica meadow in the Revellata Bay are consistent with previous data obtained on flux measurements in seagrass meadow (i.e. 228 to -363 μmol N – ammonium – m-2 d-1 in ), much lower than fluxes estimated till now in estuaries and intertidal zones (i.e. -2191 to -19704 μmol N – ammonium – m-2 d-1 in ).
The ranges of our data were large, such a high variability, already mentioned by other authors, is due to both small scale heterogeneous physical, chemical and biological processes of the sedimentary environments and actual temporal variability of nutrient fluxes . For example,  noted that the benthic fluxes showed a good relationship with bioturbation.
Concerning the seasonal variation, our results are not similar to some literature data which have pointed out a direct relation between the magnitude of the fluxes and the water temperature. Generally, minimum fluxes have been obtained during low temperature periods [24, 25]. In fact, like in other Mediterranean meadows (see ), in the Revellata Bay, registered water temperature were higher in October than in June and than in February.
Relation between fluxes and nutrient concentrations Ammonium and nitrite+nitrate concentrations (μmol L-1) in the column, canopy and pore waters in the P. oceanica meadow of the Revellata Bay at 10 m depth (mean ± standard deviation; number of sample into brackets); correlation coefficient (r2) between the concentration gradient at the water-sediment interface (canopy and pore-water) and the fluxes (from table 2) at this interface.
NH 4 +
0.10 ± 0.10 (3)
≤ 0.05 (21)
3.5 ± 5.0 (22)
0.05 ± 0.03 (5)
0.07 ± 0.04 (16)
3.7 ± 3.5 (51)
0.14 ± 0.09 (7)
0.15 ± 0.12 (14)
2.8 ± 2.1 (10)
0.10 ± 0.06 (15)
0.50 ± 0.50 (16)
1.3 ± 2.6 (10)
NO 2 +NO 3
0.07 ± 0.03 (3)
0.07 ± 0.04 (21)
0.8 ± 2.1 (22)
0.15 ± 0.04 (3)
0.18 ± 0.04 (16)
0.2 ± 0.4 (51)
0.18 ± 0.09 (7)
0.09 ± 0.04 (14)
0.7 ± 0.7 (10)
0.05 ± 0.03 (15)
0.19 ± 0.09 (16)
0.2 ± 0.2 (10)
Our results obtained both with the benthic chamber and the cylinder show that N and P from sediment diffuse into the water column. In spite of the low concentrations encountered in the Revellata Bay, both in pore and column water, the fluxes of nutrients across sediment to the canopy water are a potential important source of nitrogen and phosphate for the P. oceanica canopy.
It is now well known that seagrasses use ammonium, nitrate and phosphate found in both the column and sediment waters (see [8, 28]). Nutrients levels available for seagrass meadows are generally low and the biomass formation is often limited by nutrient availability. Among the seagrasses, P. oceanica have been shown to diminish its dependence on nutrients by an important leaf longevity which allows a better efficiency of nutrients recycling from senescent leaves.
In the Revellata Bay, at 10 metres depth, the nitrogen resorption of P. oceanica leaves has been shown to represent 40% of the annual nutrient budget of the plant [11, 12]. The mean daily nitrogen requirement of the plant covering 1 m2 has been estimated to 1500 μmol [11, 12]. Considering a weight N/P Redfield ratio of 10 for P. oceanica, the similar phosphorus requirement could be estimated to 150 μmol P m-2 d-1. From the present work, the mean annual nutrient fluxes (i.e. -31, -269 and -37 μmol m-2 d-1 for NO2-+NO3-, NH4+ and PO4- respectively) across the sediment could provide 20% of the nitrogen and phosphorus requirement of the plant.
However, it must be taken into account that primary producers (epiphytes, phytoplankton...) occur in the canopy and in its vicinity competes with P. oceanica leaves for these nutrients released by sediments. In this regard, during calm weather events, often occurring during the summer, the appearance of a nutrient rich layer in the canopy is an additional factor which favour P. oceanica vs phytoplankton during a period when the nutrients in the column water are often below the detection limits in the Revellata Bay (as measured by ).
Such a "barrier" effect played by the leaves during the period of high biomass which corresponds with low nutrient concentrations in the column water in the Revellata Bay is therefore to be added to the known meadow strategies which permit a high development of biomass in oligotrophic zone. To conclude, the apparent paradox of P. oceanica meadows growing in very oligotrophic environments can be explained by the addition of two strategies:
the high leaf longevity which allows a significant internal cycling of nutrients from senescent leaves,
the formation by the canopy of a nutrient rich water layer which largely increases the nutrient availability for the meadow during periods when nutrients are virtually absent of the column water.
Materials and Methods
Ten shoots were collected by Scuba diving in June and October 1999, at 10 metres depth to record biometrical data. The shoots were weighed after lyophilisation. The juvenile, intermediate and adult leaves were separated and measured according to . The shoot density (number of shoots per square metre) was estimated by counting the number of shoots within a 30 cm diameter circle according to .
The canopy and column water temperatures were measured with a mercury thermometer (0,1°C) in June and in October 1999.
The nutrient concentration gradients in the canopy water were measured with an original sample collection tube system. The fluxes across the sediment were estimated by the use of a classical benthic chamber. The nutrient concentration gradients in the water column were measured with a benthic cylinder. The three systems are hereafter described.
The sample collection tube system (figure 7a)
The vertical profiles of the column water in the canopy were obtained with a set of tubes fixed at known depths in the water column such as they allow a vertical sampling of undisturbed water. A diver carefully attached a syringe to the lowest tube (5 cm height) and sucked water in, ejecting the first 65 ml of sample (volume of the tube) and sampling the next 45 ml of water. The same procedure was then repeated with 4 other syringes for the 15, 30, 50 and 100 cm heights. Additional water column samplings were made above the seagrass bed at 5 m depth. The water samples were frozen.
Measurements have been performed every 3 hours a day, in June and October, when the height of the canopy is high and low respectively.
The classical benthic chamber (figure 7b)
An opaque cylindrical shape plexiglas chamber was used (diameter 12 cm, height 6 cm). Twenty four hours before starting the experiment, the base of the benthic chamber was carefully pushed in the sand of a small patch (20 cm2) in the sediment of the meadow.
At the beginning of the experiment, the top of the chamber was screwed on, the pump, tubing and flexible plastic bag were settled by a diver. The pump (discharge of 0.5 L min-1) prevents water inside the chamber from stratifying, so that samples obtained are representative of the whole volume of the chamber.
During incubation, sampling was performed periodically (T0, T4, T8, T16, T20 and T32 minutes) to determine the nutrient concentrations. The samples were collected following a simple procedure: seven syringes were filled with column water (syringe 1 to 7). At T0: the pump was switched on, floodgate n°1 closed, floodgate n°2 and n°3 opened; syringe 1 and syringe T0 were plugged in. After 3 minutes (time required for a complete homogenisation of the water inside the system), the floodgate 1 was opened, the 2 and 3 were closed, 40 ml of water was collected with syringe T0 after what the 40 ml of the syringe 1 were injected into the system. The floodgates 2 and 3 were opened again while the floodgate 1 was closed. The samples were frozen directly after collection.
The measurements have been performed in February, June and October in 1997.
The opened benthic cylinder (figure 7c)
The benthic cylinder is a plexiglas chamber (50 cm height, diameter: 12 cm), with a small opening on the top (diameter: 1.5 cm). Once the cylinder carefully settled on the sandy patch sediment of the meadow by a diver, the column water was collected inside owing to a fixed tube system at 5, 10, 20 and 40 cm above the sediment with 4 syringes. This procedure was regularly repeated every 3 hours during a day.
Pore water sampling
Pore water was sampled by Scuba diving with PVC syringes connected a 10 cm long needle entirely pushed in the sediment at 10 cm depth; the water collected was directly filtered through a Whatman GF/C (1.2 μm).
Nitrogen (NH4+ and nitrite+nitrate) and orthophosphate concentrations in the water (pore, canopy and column) were analysed with an autoanalyser (SKALAR) by the classical method  for an automated system  adapted for oligothophic seawater (detection limits: 0.1, 0.02 and 0.05 μM for ammonium, nitrite+nitrate and orthophosphate respectively).
According to the first law of Fick, the flux of matter across a surface (JD, μmol cm2 d-1) can be estimated as follow:
JD = Ds (∂C/∂z)
Ds: the diffusion coefficient (cm2 s-1),
(∂C/∂z): the concentration gradient across the sediment water-interface.
Positive values indicate a nutrient movement from the water column into the sediment.
A diffusion coefficient Ds of 16 10-6 cm2 s-1 was used for NH4+ and (NO2-+NO3-) and of 7 10-6 cm2 s-1 for orthophosphate according to  for marine sediment.
In the benthic chamber, the volume of water remained constant during the incubation and the fluxes were calculated from the slope of the concentration values versus time multiplied by the ratio of chamber volume to the covered surface area. Internal concentrations were previously corrected to take into account the dilution due to subsequent sampling.
The fluxes obtained by benthic chambers incorporate diffusion and bioturbation effects on porewater solute exchange.
In the cylinder, the fluxes were calculated considering that the water movement during the sampling was negligible.
Data are presented as mean ± standard deviation, minimum and maximum.
This work was supported by grants from the Belgian National Fund for Scientific Research (FRFC 2.4570.97) and from the French Community of Belgium (ARC-97/02-212). We acknowledge G. Lacroix for providing critical comments on methodology.
The authors acknowledge R. Biondo for providing technical and diving assistance and also thank C. Beans for correcting grammatical and spelling mistakes.
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