Abstract:Abstract. This paper presents results on the spatial and temporal distribution patterns of mesozooplankton in the naturally fertilized region to the east of the Kerguelen Islands (Southern Ocean) visited at early bloom stage during the KEOPS2 survey (15 October to 20 November 2011). The aim of this study was to compare the zooplankton response in contrasted environments localized over the Kerguelen Plateau in waters of the east shelf and shelf edge and in productive oceanic deep waters characterized by conditi… Show more
“…Values of carbon content in cylindrical fecal pellets found in the literature range over approximately 1 order of magnitude between 0.01 and 0.1 mg C mm −3 (González and Smetacek, 1994;González et al, 1994González et al, , 2000Carroll et al, 1998), leading to potential strong variations in carbon flux estimations if large volumes of fecal pellets are involved, as was the case at E-5. Mesozooplankton communities collected in Bongo nets from 250 m to the surface (day and night haulings, except at R-2 and F-L, where only day haulings were conducted), and analysed with a ZooScan integrated system (Carlotti et al, 2015), generally revealed a large dominance of the size fraction 500-1000 µm with values from 54 to 79 % (considering only the stations where the traps were deployed). Microscopic identifications confirmed a community largely dominated by copepods (Carlotti et al, 2015).…”
Section: Comparison Of Poc Flux Estimationsmentioning
confidence: 99%
“…Mesozooplankton communities collected in Bongo nets from 250 m to the surface (day and night haulings, except at R-2 and F-L, where only day haulings were conducted), and analysed with a ZooScan integrated system (Carlotti et al, 2015), generally revealed a large dominance of the size fraction 500-1000 µm with values from 54 to 79 % (considering only the stations where the traps were deployed). Microscopic identifications confirmed a community largely dominated by copepods (Carlotti et al, 2015). However, most of the fecal pellets collected in gel traps at E-5 were large fragments (Fig.…”
Section: Comparison Of Poc Flux Estimationsmentioning
confidence: 99%
“…(34.6 %: fraction of total live diatom cell counts; see Table 6 for sampling depths; M. Lasbleiz, personal communication, 2014) and Thalassionema nitzschioides (25.6 %), as well as by a limited mesozooplankton biomass represented mainly by middle-sized copepods (Carlotti et al, 2015). The export was mostly mediated through physical aggregation as suggested by the dominance of phytoplankton and fecal aggregates.…”
Section: Toward An Explanation Of the Negative Relationship Between Pmentioning
confidence: 99%
“…The mesozooplankton biomass was up to 3-fold higher at A3-2 than at R-2. Small-and middle-sized copepods dominated, along with euphausiid eggs and appendicularians (Carlotti et al, 2015). Particles exported were mostly phytodetrital aggregates.…”
Section: Toward An Explanation Of the Negative Relationship Between Pmentioning
confidence: 99%
“…In Fig. 9b, mesozooplankton biomass data from KEOPS2 (250 m to surface Bongo net haulings; Carlotti et al, 2015) is shown as a simple index of zooplankton abundance against export efficiency. Considering all POC flux estimation methods, a correlation has been found (n = 15, r 2 = 0.72, p < 0.0005), suggesting that zooplankton may exert an important control on export efficiency.…”
Section: Toward An Explanation Of the Negative Relationship Between Pmentioning
Abstract. The first KErguelen Ocean and Plateau compared Study (KEOPS1), conducted in the naturally iron-fertilised Kerguelen bloom, demonstrated that fecal material was the main pathway for exporting carbon to the deep ocean during summer (January-February 2005), suggesting a limited role of direct export via phytodetrital aggregates. The KEOPS2 project reinvestigated this issue during the spring bloom initiation (October-November 2011), when zooplankton communities may exert limited grazing pressure, and further explored the link between carbon flux, export efficiency and dominant sinking particles depending upon surface plankton community structure. Sinking particles were collected in polyacrylamide gel-filled and standard free-drifting sediment traps (PPS3/3), deployed at six stations between 100 and 400 m, to examine flux composition, particle origin and their size distributions. Results revealed an important contribution of phytodetrital aggregates (49 ± 10 and 45 ± 22 % of the total number and volume of particles respectively, all stations and depths averaged). This high contribution dropped when converted to carbon content (30±16 % of total carbon, all stations and depths averaged), with cylindrical fecal pellets then representing the dominant fraction (56 ± 19 %).At 100 and 200 m depth, iron-and biomass-enriched sites exhibited the highest carbon fluxes (maxima of 180 and 84 ± 27 mg C m −2 d −1 , based on gel and PPS3/3 trap collection respectively), especially where large fecal pellets dominated Published by Copernicus Publications on behalf of the European Geosciences Union. 1008 E. C. Laurenceau-Cornec et al.: The importance of sinking particle types to carbon export over phytodetrital aggregates. Below these depths, carbon fluxes decreased (48±21 % decrease on average between 200 and 400 m), and mixed aggregates composed of phytodetritus and fecal matter dominated, suggesting an important role played by physical aggregation in deep carbon export.Export efficiencies determined from gels, PPS3/3 traps and 234 Th disequilibria (200 m carbon flux/net primary productivity) were negatively correlated to net primary productivity with observed decreases from ∼ 0.2 at low-iron sites to ∼ 0.02 at high-iron sites. Varying phytoplankton communities and grazing pressure appear to explain this negative relationship. Our work emphasises the need to consider detailed plankton communities to accurately identify the controls on carbon export efficiency, which appear to include small spatio-temporal variations in ecosystem structure.
“…Values of carbon content in cylindrical fecal pellets found in the literature range over approximately 1 order of magnitude between 0.01 and 0.1 mg C mm −3 (González and Smetacek, 1994;González et al, 1994González et al, , 2000Carroll et al, 1998), leading to potential strong variations in carbon flux estimations if large volumes of fecal pellets are involved, as was the case at E-5. Mesozooplankton communities collected in Bongo nets from 250 m to the surface (day and night haulings, except at R-2 and F-L, where only day haulings were conducted), and analysed with a ZooScan integrated system (Carlotti et al, 2015), generally revealed a large dominance of the size fraction 500-1000 µm with values from 54 to 79 % (considering only the stations where the traps were deployed). Microscopic identifications confirmed a community largely dominated by copepods (Carlotti et al, 2015).…”
Section: Comparison Of Poc Flux Estimationsmentioning
confidence: 99%
“…Mesozooplankton communities collected in Bongo nets from 250 m to the surface (day and night haulings, except at R-2 and F-L, where only day haulings were conducted), and analysed with a ZooScan integrated system (Carlotti et al, 2015), generally revealed a large dominance of the size fraction 500-1000 µm with values from 54 to 79 % (considering only the stations where the traps were deployed). Microscopic identifications confirmed a community largely dominated by copepods (Carlotti et al, 2015). However, most of the fecal pellets collected in gel traps at E-5 were large fragments (Fig.…”
Section: Comparison Of Poc Flux Estimationsmentioning
confidence: 99%
“…(34.6 %: fraction of total live diatom cell counts; see Table 6 for sampling depths; M. Lasbleiz, personal communication, 2014) and Thalassionema nitzschioides (25.6 %), as well as by a limited mesozooplankton biomass represented mainly by middle-sized copepods (Carlotti et al, 2015). The export was mostly mediated through physical aggregation as suggested by the dominance of phytoplankton and fecal aggregates.…”
Section: Toward An Explanation Of the Negative Relationship Between Pmentioning
confidence: 99%
“…The mesozooplankton biomass was up to 3-fold higher at A3-2 than at R-2. Small-and middle-sized copepods dominated, along with euphausiid eggs and appendicularians (Carlotti et al, 2015). Particles exported were mostly phytodetrital aggregates.…”
Section: Toward An Explanation Of the Negative Relationship Between Pmentioning
confidence: 99%
“…In Fig. 9b, mesozooplankton biomass data from KEOPS2 (250 m to surface Bongo net haulings; Carlotti et al, 2015) is shown as a simple index of zooplankton abundance against export efficiency. Considering all POC flux estimation methods, a correlation has been found (n = 15, r 2 = 0.72, p < 0.0005), suggesting that zooplankton may exert an important control on export efficiency.…”
Section: Toward An Explanation Of the Negative Relationship Between Pmentioning
Abstract. The first KErguelen Ocean and Plateau compared Study (KEOPS1), conducted in the naturally iron-fertilised Kerguelen bloom, demonstrated that fecal material was the main pathway for exporting carbon to the deep ocean during summer (January-February 2005), suggesting a limited role of direct export via phytodetrital aggregates. The KEOPS2 project reinvestigated this issue during the spring bloom initiation (October-November 2011), when zooplankton communities may exert limited grazing pressure, and further explored the link between carbon flux, export efficiency and dominant sinking particles depending upon surface plankton community structure. Sinking particles were collected in polyacrylamide gel-filled and standard free-drifting sediment traps (PPS3/3), deployed at six stations between 100 and 400 m, to examine flux composition, particle origin and their size distributions. Results revealed an important contribution of phytodetrital aggregates (49 ± 10 and 45 ± 22 % of the total number and volume of particles respectively, all stations and depths averaged). This high contribution dropped when converted to carbon content (30±16 % of total carbon, all stations and depths averaged), with cylindrical fecal pellets then representing the dominant fraction (56 ± 19 %).At 100 and 200 m depth, iron-and biomass-enriched sites exhibited the highest carbon fluxes (maxima of 180 and 84 ± 27 mg C m −2 d −1 , based on gel and PPS3/3 trap collection respectively), especially where large fecal pellets dominated Published by Copernicus Publications on behalf of the European Geosciences Union. 1008 E. C. Laurenceau-Cornec et al.: The importance of sinking particle types to carbon export over phytodetrital aggregates. Below these depths, carbon fluxes decreased (48±21 % decrease on average between 200 and 400 m), and mixed aggregates composed of phytodetritus and fecal matter dominated, suggesting an important role played by physical aggregation in deep carbon export.Export efficiencies determined from gels, PPS3/3 traps and 234 Th disequilibria (200 m carbon flux/net primary productivity) were negatively correlated to net primary productivity with observed decreases from ∼ 0.2 at low-iron sites to ∼ 0.02 at high-iron sites. Varying phytoplankton communities and grazing pressure appear to explain this negative relationship. Our work emphasises the need to consider detailed plankton communities to accurately identify the controls on carbon export efficiency, which appear to include small spatio-temporal variations in ecosystem structure.
Spatial and seasonal dynamics of microbial loop fluxes were investigated in contrasting productivity regimes in the Indian sector of the Southern Ocean. Observations carried out in late summer (February-March 2018; project MOBYDICK) revealed higher microbial biomasses and fluxes in the naturally iron-fertilized surface waters of Kerguelen island in comparison to surrounding off-plateau waters. Differences were most pronounced for bacterial heterotrophic production (2.3-fold), the abundance of heterotrophic nanoflagellates (HNF; 2.7-fold). Independent of site, grazing by HNF was the main loss process of bacterial production (80-100%), while virus-induced mortality was low (< 9%). Combining these results with observations from previous investigations during early spring and summer allowed us to describe seasonal patterns in microbial food web fluxes and to compare these to carbon export in the iron-fertilized and high-nutrient, low-chlorophyll (HNLC) Southern Ocean. Our data suggest an overall less efficient microbial food web during spring and summer, when respiration and viral lysis, respectively, represent important loss terms of bacterially-mediated carbon. In late summer, primary production is more efficiently transferred to bacterial biomass and HNF and thus available for higher trophic levels. These results provide a new insight into the seasonal variability and the quantitative importance of microbial food web processes for the fate of primary production in the Southern Ocean.
Food quality is recognized as a key parameter of food web functioning in which zooplankton plays a crucial role not only in linking lower to upper trophic levels but also in transforming the quality of the organic matter available to predators. The influence of size and taxonomic group composition of zooplankton in these processes was assessed in eastern Kerguelen waters (Southern Ocean) at the onset of the spring bloom in 2011. Biochemical (lipids, proteins and carbohydrates) and elemental (carbon and nitrogen) composition were measured in five size-fractions of bulk zooplankton ranging from 80 µm to > 2000 µm and in large copepods, euphausiids, annelids and salps, and energy content was derived from biochemical contents. Proteins were the dominant component of zooplankton dry weight (21.5% dw), followed by lipids (8.9% dw), soluble carbohydrates (2.2% dw) and insoluble carbohydrates (1.0% dw). A concentration increase with zooplankton size for all biochemical components was observed, particularly stronger for proteins and lipids. Copepods and salps provided, respectively, the highest and the lowest amount of lipids and energy.
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