Biogeographic structure of the microphytoplankton assemblages of the south Atlantic and Southern Ocean during austral summer

Microphytoplankton distribution in the Atlantic sector of theSouthern Ocean was investigated along a transect during theSAAMES II cruise undertaken in late austral summer (January/February) 1993. Samples were collected at 60 km intervals between34 and 70°S for the analysis of mineral nutrients, and theidentification and enumeration of microphytoplankton. Peaksin microphytoplankton abundance were recorded in the neriticwaters of Africa and Antarctica, at all major oceanic fronts,and in the marginal ice zone (MIZ). Partial correlation analysisindicated that 45% of the total variance associated with microphytoplanktonabundance could be explained by silicate and phosphate concentrations,while temperature accounted for 65% (P<0.001). Cluster andordination analyses identified two major groups of stations,one north and one south of the Subantarctic Front (SAF). Thisdivision appears to be related to differences in temperatureand silicate concentrations. Each region comprised distinctmicrophytoplankton subgroups associated with specific watermasses or hydrological features. Indicator species could beidentified for some water masses. In the MIZ, microphytoplanktonspecies composition and succession were strongly affected bysea-ice throughout the summer.     

Microphytoplankton assemblages in the waters surrounding South Georgia, Antarctica during austral summer 1994

The composition and distribution of microphytoplankton assemblages in the vicinity of South Georgia were examined during a krill survey conducted during voyage 119 the RV Africana in austral summer (January/February) 1994. Microphytoplankton distribution was studied at 83 stations along a zig-zag transect in the waters surrounding South Georgia. Oceanographic and zooplankton data suggest that conditions were anomalous during the investigation, in that sub-Antarctic surface waters had probably been advected southwards and were present around the island. The two most widely distributed species were Corethron criophilum and Eucampia antarctica, which were recorded at all stations sampled. Also well-represented amongst the microphytoplankton assemblages were temperate, neritic species such as Chaetoceros atlanticus, Proboscia alata and Odontella weissflogii. This can probably be related to the intrusion of sub-Antarctic surface waters unusually far south. Cluster and ordination analysis identified three distinct groupings of stations in the waters surrounding the islands. These were found to the east, west and north of the islands. The diatom groupings identified during this investigation broadly correspond to three water masses previously described in the vicinity of South Georgia. Despite the anomalous hydrographical conditions that existed during the investigation, the differences in phytoplankton were negligible when compared to normal years. Small mesoscale features are, however, important in imposing biogeographic patterns on microphytoplankton. Received: 21 February 1996 / Accepted: 3 November 1996     

Mesozooplankton community structure and grazing impact in the region of the Subtropical Convergence south of Africa

Mesozooplankton distribution and community structure in theregion of the Subtropical Convergence (STC) south of Africawere investigated during the SAAMES III cruise in austral winter(June–July) 1993. Both the STC and an associated warm-coreeddy (WCE) exhibited enhancements in zooplankton abundance,compared to the Subantarctic waters. Particularly, elevatedzooplankton densities were found in the centre of the STC andin the region north of it as well as at the edge of the WCE.Copepods (mainly Pleuromamma abdominalis and Metridia lucens),euphausiids (Euphausia spinifera, E.similis and E.recurva),pteropods (Limacina spp.) and chaetognaths (Eukrohnia hamataand Sagitta spp.) dominated numerically and accounted for >60     

Epipelagic zooplankton assemblages and a warm-core eddy off East Cape, New Zealand

Zooplankton assemblages in the vicinity of a warm-core eddyoff East Cape in January 1978 were divided by a form of clusteranalysis into four groups: an Eddy Centre Group, an oceanicNorthern Group, a mixed group with oceanic and coastal species(Coastal Group) and a Southern Group apparently originatingfrom the south. The latter three groups were entrained aroundthe eddy centre. The processes which lead to the observed distributionsare discussed. Significant differences between the Southernand Eddy Centre populations, both dominated numerically by salps,suggests that advection was not a major source of zooplanktonbiomass in the eddy. It is concluded that the population compositionof the eddy is mainly the result of in situ biological processes.     

The distribution of hyperiid amphipods (Crustacea:Peracarida) in relation to warm-core eddy J in the Tasman Sea

Hyperiid amphipods were sampled in and around warm-core eddyJ in the Tasman Sea off eastern Australia in August, Septemberand October 1979. Samples were taken at night to a depth of400 m with a midwater trawl (RMT-8). In all, 22 798 hyperiidsrepresenting 38 species and 10 families were collected. Sevenspecies, individually found in numbers >4% of the total amphipodpopulation, together contributed 87.1% to the total. Of these,Scina crassicornis, Phronima sedensataria, P.atlantica, Phrosinasemilunata, Primno johnsoni and Brachyscelus crusculum wereusually found in highest numbers outside the eddy. Streetsiachallengeri was the only abundant species with significantlyhigher numbers inside the eddy. Outside the eddy, samples werecharacterized by large numbers of few species, whereas abundanceswere more evenly distributed between species inside the eddy.The size distributions of two abundant species (B.crusculumand S.challengeri) were not significantly different betweenthe inside and outside of eddy J. Hyperiid faunal patterns wereassociated with depth and temperature (August), position withrespect to the eddy (September, October) and the presence ofgelatinous zooplankton (September, October).     

Small-scale distribution of a cnidarian population in the western Mediterranean

The neritic area of the coast of Catalonia (north–westMediterranean) has a continental shelf narrower in the northernhalf and broader in the southern half. This area is crossedfrom north to south by a coastal current whose intensity decreasesto the south. Both conditions, together with other local geographicaland hydrographical features, are thought to be the key factorsin determining the distribution of planktonic cnidarian assemblages,along two main variational axes: a north-south axis and a coast-opensea axis. Aiming to find support to this hypothesis, the planktoniccnidarians collected in two seasons of the year 1983 have beenstudied. The first season (April–May) corresponds to thehighest abundance and heterogeneity, and the second (September–October),to the epoch when the cnidarian population is lower, but constant,along the coastal area. In a global principal component analysisthe factor that best explains the group distribution in thearea is the coastal character, as given by the bottom depthof the sampling station. The number of individuals is greaternear the coast (due to the dominance of a euryhaline species,Muggiaea atlantica), but the species number increases towardsthe open sea (due to the addition of more oceanic species, suchas Narcomedusae and Trachymedusae and the effect of a permanenthydrographic front at the shelf-slope boundary). The secondfactor is the latitudinal axis. The northern half of the coastis under the influence of waters favouring a greater numberof species and individuals. On the contrary, the southern halfshows a less marked influence of the north–south current,their cnidarian assemblages being more constant over time. Althoughthe global cnidarian population follows this general pattern,the most abundant and frequent species (M.atlantica and Aglaurahemistoma) show a broad distribution over all the studied areabecause they are rather insensitive to hydrographical variations.     

Size-fractionated Primary Production in the South Atlantic and Atlantic Sectors of the Southern Ocean

Results are presented from size fractionated chlorophyll a (Chla) and primary production studies along a transect between Antarcticaand southern Africa during the second South African AntarcticMarine Ecosystem Study (SAAMES II), conducted in late australsummer (January to February) 1993. Total integrated Chl a alongthe transect was highest in the vicinity of the Marginal IceZone (MIZ) and Antarctic Polar Front (APF). At these stations,integrated Chl a biomass was always >25 mg Chl a m^–2and was dominated by microphytoplankton. Although nominal increasesinChl a biomass were also associated with the Subantarctic Front(SAF) and Subtropical Convergence (STC), total Chl a biomassin these regions was dominated by nanophytoplankton. Withinthe inter-frontal regions, total integrated Chl a biomass waslower, generally <25 mg Chl a m^–2, and was always dominatedby nanophytoplankton. An exception was found in the AgulhasReturn Current (ARC) where picophytoplankton dominated. Totaldaily integrated production along the transect ranged between60 and 436 mg C m^–2 day^–1. Elevated production rateswere recorded at stations occupied in the vicinity of the MIZand at all the major oceanic frontal systems. The contributionsof the various size fractions to total daily production displayedthe same spatial pattern as integrated biomass, with microphytoplanktonbeing the most important contributor in areas characterizedby elevated phytoplankton biomass. Outside these regions, nanophytoplanktondominated the total phytoplankton production. Again, an exceptionwas found in the ARC north of the STC where picophytoplanktondominated total production. There, the lowest production alongthe entire transect was recorded, with total daily integratedproduction always <90 mg C m^–2 day^–1. The increasedproduction rates recorded in the MIZ appeared to result fromincreased water column stability as indicated by a shallow mixed-layerdepth. Within the inter-frontal regions, the existence of adeep mixed layer appeared to limit phytoplankton production.Low silicate concentrations in the waters north of the APF mayalso have limited the growth of large microphytoplankton.     

Size-fractionated primary production studies in the vicinity of the Subtropical Front and an adjacent warm-core eddy south of Africa in austral winter

Results are presented of size-fractionated primary productionstudies conducted in the vicinity of the Subtropical Front (STF),an adjacent warm-core eddy, and in Sub-antarctic waters duringthe third South African Antarctic Marine Ecosystem Study (SAAMESIII) in austral winter (June/July) 1993. Throughout the investigation,total chlorophyll (Chl a) biomass and production were dominatedby small nano- and picophytoplankton. No distinct patterns intotal Chl a were evident. At stations (n = 7) occupied in thevicinity of the STF, total integrated biomass values rangedfrom 31 to 53 mg Chl a m^–2. In the vicinity of the eddy,integrated biomass at the eddy edge (n = 3) ranged from 24 to54 mg Chl a m^–2 and from 32 to 43 mg Chl a m^–2 inthe eddy (n = 2). At the station occupied in the Sub-antarcticwaters, total integrated biomass was 43 mg Chl a m^–2.Total daily integrated production was highest at stations occupiedin the vicinity of the STF and at the eddy edge. Here, totalintegrated production ranged from 150 to 423 mg C m^–2day^–1 and from 244 to 326mg C m^–2 day^–1, respectively.In the eddy centre, total integrated production varied between134 and 156 mg C m^–2 day^–1. At the station occupiedin the Sub-antarctic waters, the lowest integrated production(141 mg C m^–2 day^–1) during the entire survey wasrecorded. Availability of macronutrients did not appear to limittotal production. However, the low silicate concentrations duringthe survey may account for the predominance of small nano- andpicophytoplankton. Differences in production rates between theeddy edge and eddy core were related to water column stability.In contrast, at stations occupied in the vicinity of the STF,the control of phytoplankton production appears to be relatedto several processes, including water column stability and,possibly, iron availability.     

Variation of the phytoplankton community across the subtropical convergence zone in the west pacific sector of the southern ocean during early austral Summer 1995/6

Phytoplankton of the Southern Ocean, 140–148°E and 40–53°S, was sampled from early austral summer Nov. 1995 to Dec. 1995 to examine cell abundance, cell volume and biomass (cell carbon) distribution across the fronts. A total of 90 phytoplankton taxa were identified. They were 50 diatoms, 37 dinoflagellates, 2 silicoflagellates, and 1 prymnesiophyte. 73 species were observed from north of the subtropical convergence zone and 71 species from south of the subtropical convergence zone.Pseudonitzschia spp. was the most widely distributed species. Nanoplankton predominated cell number of phytoplankton throughout the stations. The abundance of diatoms was higher than that of dinofiagellates. Total biomass profiles were dependent to microphytoplankton biomass. Maximum cell number and biomass were observed from subsurface layer. Phytoplankton community changed across the subtropical convergence zone and 50–53°S (antarctic convergence zone), and physicoehemical factors seem to controll the distribution.     

An immunofluorescent survey of the brown tide chrysophyte Aureococcus anophagefferens along the northeast coast of the United States

Surveys were conducted along the northeast coast of the USA.between Portsmouth, NH, and the Chesapeake Bay in 1988 and 1990,to determine the population distribution of Aureococcus anophagefferens,the chrysophyte responsible for massive and destructive ‘browntides’ in Long Island and Narragansett Bay beginning in1985. A species-specific immunofluorescent technique was usedto screen water samples, with positive identification possibleat cell concentrations as low as 10–20 cells ml^–1.Both years.A.anophagefferens was detected at numerous stationsin and around Long Island and Barnegat Bay, NJ, typically athigh cell concentrations. To the north and south of thus ‘center’,nearly half of the remaining stations were positive for A.anophagefferens,but the cells were always at very low cell concentrations. Manyof the positive identifications in areas distant from Long Islandwere in waters with no known history of harmful brown tides.The species was present in both open coastal and estuanne locations,in salinities between 18 and 32 practical salinity units (PSU).The observed population distributions apparently still reflectthe massive 1985 outbreak when this species first bloomed, giventhe number of positive locations and high abundance of A.anophagefferensin the immediate vicinity of Long Island. However, the frequentoccurrence of this species in waters far from this population‘center’ is disturbing. Aureococcus anophagefferensis more widely distributed than was previously thought. Numerousareas thus have the potential for destructive brown tides suchas those associated with the sudden appearance of the speciesin 1985.     

The distribution of benthic invertebrates along a natural turbidity gradient in Lake Temiskaming,Ontario-Quebec

Lake Temiskaming, a rift valley lake on the Ontario-Quebec border, exhibits a permanent gradient of turbidity due to tributary streams which cut through clay deposits to the north of the lake. Concentrations of total phosphorus (TP) also decreased from north to south, with values suggesting mesotrophic conditions. Concentrations of chlorophyll a were characteristic of oligotrophic lakes and showed little relationship to either turbidity or TP. Large numbers of Tubificidae were found at our northernmost sampling station at a depth of 50 m, probably reflecting the localized impact of allochthonous organic matter introduced by a tributary stream. Numerical abundance of the benthic fauna was much lower and did not vary significantly among the six more southerly 50 m stations, but biomass declined from north to south as Heterotrissocladius oliveri relaced Pontoporeia hoyi. Numerical abundance did not differ significantly among stations at depths of 10 m, but biomass decreased from north to south reflecting the distributions of the largest species, Hexagenia sp. and P. hoyi. Intensive sampling on two transects showed that maximum numbers of invertebrates occurred in the profundal zone. While these results are consistent with the correlation between TP and zoobenthic biomass reported by other investigators, size selective predation by fish may also be important in controlling the distribution of benthic invertebrates in Lake Temiskaming.     

Taxonomic composition and growth rates of phytoplankton assemblages at the Subtropical Convergence east of New Zealand

Off the eastern coast of New Zealand, warm, saline, nutrient-poorSubtropical Waters (STW) are separated from cool, fresher, relativelynutrient-rich Sub-Antarctic Waters (SAW) by the SubtropicalConvergence (STC). The Chatham Rise, a submarine rise, restrictsthe latitudinal movement of the STC as well as mixing of STWand SAW. Due to this restriction, this sector of the STC ischaracterized by sharp gradients in temperature, macro- (nitrate,silicate and phosphate) and micro- (iron) nutrient concentrations.Shipboard incubations were conducted during austral spring 2000and 2001 to test the hypothesis that these gradients affectthe taxonomic composition and/or growth rates of phytoplanktonon either side of and at the STC. Maximum chlorophyll a concentrationsduring 2000 were 0.39 µg L^–1, but were an orderof magnitude higher in 2001. During both years, STC phytoplanktonwere dominated by diatoms (77% of the total chlorophyll a duringaustral spring 2000 and 70% during spring 2001), whereas cryptophytesand prasinophytes dominated STW assemblages (27 and 36% during2000, and 63 and 17% during 2001). Chlorophyll in the SAW wasdominated by procaryotes and photosynthetic nanoflagellatesduring 2000 (17% procaryotes, 68% nanoflagellates), and by diatomsduring the austral spring 2001 cruise (53%). Growth rates ofthe phytoplankton assemblage were determined by ¹⁴C-labelingof chlorophyll a and photosynthetic pigments. During 2000, temperature-normalizedgrowth rates were near maximal at the STC, and decreased onaverage to less than half of the maximum north and south ofthat front, whereas in 2001 both absolute and relative growthrates were low at all stations. Growth rates did not closelyparallel biomass of the various taxa, suggesting that nutrientlimitation and/or grazing were significantly impacting standingstocks. It appeared that growth was strongly influenced by nutrientsand light, but that biomass was more strongly influenced bygrazing. The STC is a globally important region of enhancedbiomass and productivity; however, the phytoplankton assemblagereflects control by both top–down and bottom–upprocesses that makes a predictive understanding of the area'sbiogeochemical cycles extremely difficult.     

On the presence of Pseudo-nitzschia calliantha Lundholm, Moestrup et Hasle and Pseudo-nitzschia delicatissima (Cleve) Heiden in the Southern Adriatic Sea (Mediterranean Sea, Italy)

This investigation included a 2-year monitoring program aimedat assessing the abundance and distribution of harmful marinephytoplankton along the Southern Adriatic coast of Italy. Monthlysampling was conducted from April 1995 to March 1997 at foursampling stations along four transects, to determine the temporaland spatial presence/abundance of the potentially toxic Pseudo-nitzschiaspecies. The study focussed on the most abundant taxa Pseudo-nitzschiacalliantha and Pseudo-nitzschia delicatissima, the identitiesof which were confirmed by TEM on cleaned net material. Thedistribution patterns of these potential Amnesic Shellfish Poisoning(ASP) toxin producers were statistically analysed by GeneralisedLinear Model ANalysis Of VAriance, Principal Component Analysis(GLM ANOVA, PCA) and Spearman’s correlation analysis inorder to address relationships between environmental variableand population dynamics. Abundances displayed horizontal andvertical structure in the study area. Inter-annual variabilitywas also observed for both species that appeared to responddifferently to the environmental factors investigated. Distributionsof P. calliantha showed a stronger seasonality and was morecorrelated with winter water conditions than P. delicatissima,which in turn exhibited a broader temporal distribution andappeared independent from major environmental constraints. Thisis the first report of the occurrence and dynamics of P. callianthaand P. delicatissima populations in Southern Adriatic coastalwaters. First two authors equally contributed to this work.     

Biogeographic study of the planktonic communities of the Prince Edward Islands (Southern Ocean)

Microphytoplankton and zooplankton composition and distributionin the vicinity of the Prince Edward Islands and at the Sub-antarcticFront (SAF) were investigated in late austral summer (April/May)1996. Samples were collected for analysis of chlorophyll a concentration(Chi a), microphytoplankton and zooplankton abundance. Generally,the highest Chl a concentrations (up to 2.0 µg l^–1)and zooplankton densities (up to 192 ind. m^–3) were recordedat stations within the inter-island area while the lowest values(<0.4 µg l^–1) were observed at stations upstreamof the islands. High Chl a and zooplankton biomass values werealso associated with the SAF. Microphytoplankton were dominatedby chain-forming species of the genera Chaetoceros (mainly C.neglectus),Fragilariopsis spp. and the large diatom Dactyliosolen antarcticus.The zooplankton assemblages were always dominated by mesozooplanktonwhich at times contributed up to 98% of total zooplankton abundanceand up to 95% of total biomass. Among mesozooplankton, copepods,mainly Clausocalanus brevipes and Metridia lucens numericallydominated. Among the macrozooplankton euphausiids, mainly Euphausiavallentini, E.longirostis and Stylocheiron maximum, and chaetognaths(Sagitta gazellae) accounted for the bulk of abundance and biomass.Cluster and ordination analysis did not identify any distinctbiogeographic regions among either the microphytoplankton orzooplankton.     

Patterns of β‐diversity in a Mexican tropical dry forest

Abstract. Patterns of β‐diversity in a highly diverse tropical dry forest tree community are described; the contribution of environmental heterogeneity and distance to β‐diversity was assessed. Significant differences in elevation, insolation, slope and soil water holding capacity (p < 0.01), variables related to water availability, were found among 830 m × 100 m transects laid along contrasting slopes of a system of three parallel microbasins. A gradient in elevation and insolation was found within north‐facing transects, among 10 m × 10 m sites; south‐facing transects showed an elevation gradient while crest transects showed a gradient in water holding capacity. In total 119 species were registered, with 27 to 64 species per transect, and 4 to 16 species per site. A large β‐diversity was found among and within transects; two indices of β‐diversity consistently showed a higher β‐diversity within transects than among them. Among transects, 64% of the variance in species composition could be attributed to the environmental variables; an additional 22% to the spatial distribution of sites. Within transects, 42% of the deviance in β‐diversity values was explained by insolation, and 19% by distance. β‐diversity increased with distance and with difference in insolation among sites; north‐facing transects, those with most contrasting insolation conditions, had the steepest increase in β‐diversity with distance. Such increase was clearly associated with changes in species composition, not with changes in species richness.     

Distribution of epiplanktonic Chaetognatha along a transect in the Indian Ocean

Chaetognaths were identified and counted in 23 samples collectedin the west Indian Ocean along a transect from the Gulf of Adento the Cape of Good Hope, in February–March 1967. Althoughthe hydrographic front located at 5°S does not seem to representa barrier for the distribution of the majority of the species,some of them are in a preferential area south or north of thefront. The principal component analysis indicates the locationswhere the more intense overlapping of species takes place. Itis important to mention the occurrence of S.pseudoserratodentatain the proximity of Madagascar Island.     

The distribution of dinoflagellate cysts along the Galician (NW Spain) coast

We have studied the distribution of dinoflagellate cysts along10 Galician rías and part of their adjacent continentalshelf. Cyst abundance in the area averaged 856 cysts ml^–1,which is of the same order of magnitude as those found in otherareas of the western European coast. It was higher in the ríasthan in the shelf, having a very heterogeneous distribution,especially in the former. Cyst assemblages in these two areaswere different, suggesting that differences are due to cystproduction rather than to accumulation. Principal componentanalysis, cluster analysis, distribution of macroscopic characteristicsof cyst populations and distribution of single species suggestthat local factors control the distribution in the rías.Nevertheless, a general pattern that splits the whole area intotwo-to the north and to the south of the ría de Camariñas-canbe distinguished. This latter trend was also observed in theshelf and, in our opinion, It should be attributed to threeconcurrent causes: the effect of different upwelling intensitiesor frequencies, the effect of the different numbers and sizesof the ría in each area, and the effect of the presenceof different water masses in these areas. The cyst distributionof a number of individual species was examined and showed threegeneral groups: species with very restricted distribution, suchas Alexandrium sp2 or Scrippsiella sp4, species with a widespreaddistribution along the rías, such as several Scrippsiellaspecies, and species mainly distributed along the shelf, suchas Gymnodinium catenatum. The distribution of cysts belongingto red tide organisms fits quite well with that of their correspondingmotile phases dunng the three previous years for most of theorganisms studied and also during the 1992–1993 period(7–8 years later), but the role of this resting stagein initiating such blooms seems to be highly variable with species.     

Acoustics and freshwater zooplankton

We investigated the potential of acoustic technology for estimatingzooplankton distribution as part of an ongoing study of sockeyesalmon (Oncorhynchus nerka) production in three lakes of theFraser River system, British Columbia. Simultaneous acousticand zooplankton samples were obtained in 1 and 2 m depth incrementsfrom the surface to 30 m at mid-lake stations. We derived asignificant regression relationship (r²=0.71, n=79) betweenzooplankton biomass ranging between 5 and 220 mg m^–3 andacoustic backscatter (V²). The ensuing regression model wasused to predict zooplankton biomass distribution from acousticdata collected along transects representing different lake areas.     

Can predators maintain parapatry? Ant distribution across a tick parapatric boundary in South Australia

Abstract Ants were sampled by pitfall traps at 85 sites, 0.5 or 1.0km apart, along six transects across a parapatric boundary between the reptile ticks Aponomma hydrosauri and Amblyomma limbatum near Mt Mary in South Australia. There was no tendency for overall ant density, or for the distribution of any single species of ant, to be related to the tick distribution. Thus the survey found no support for the hypothesis that predation by ants was maintaining the boundary. Along transects there were no correlations between ant and tick densities. Thus the survey found no support for the hypothesis that ant predation was a major factor controlling tick densities. These negative results provide further evidence that single, strong ecological processes cannot explain this well-studied parapatric boundary.     

Control of microplankton size structure in contrasting water columns of the Celtic Sea

Water column structure, microphytoplankton size spectra andnutrient concentration were analysed at six sampling stationsin the Celtic Sea. Three types of stations were distinguished:(i) where the upper mixed layer (UML) reaches the total depth(TD), (ii) where the UML is about half of TD and (iii) wherethe UML is considerably less than half the TD. The UML was nutrientrich at type A stations and was nutrient depleted at type Bstations. At type C stations, the UML was nitrate depleted andsilicate rich. Two groups of microplankton size-abundance spectra(SAS) were found: (i) a typical linear SAS and (ii) a more complex‘atypical’ SAS, with a linear part up to 160 µmand a dome at 300 µm caused by a Coscinodiscus wailesiibloom. The dome was observed at all depths at type A stationsand above the pycnocline and at the seafloor of type B stations.Combining intrinsic growth rate, sinking rate and mixing layerdepth, the C. wailesii dome persists only at type A stationsbut settles out of the UML at the remaining stations. This suggeststhat a large part of the perturbation at the right extreme ofphytoplankton SAS does not propagate along the planktonic SASbut sinks to the seafloor. This paper was presented in a session on "Size Structure ofPlankton Communities", at the ASLO Summer International Meeting,held in Santiago de Compostela, Spain, between 19 and 24 June,and coordinated by Xabier Irigoien, Roger Harris and Angel Lopez-Urrutia.