Zooplankton Community During the Transition from Spring Bloom to Oligotrophy in the Open NW Mediterranean and Effects of Wind Events. 1. Abundance and Specific Composition

Short-term changes in the zooplankton community were investigatedat a time-series station in the open NW Mediterranean duringthe DYNAPROC cruise programme (May 1995). Based on the samplesobtained with three devices (12 l bottle, 200 µm and 500µm mesh nets), the abundance and specific compositionare presented for mesozooplankton (copepods mainly), macroplanktonand micronekton. Over the 3 week sampling period, overall densityof the copepod community decreased and changes in the specificcomposition occurred. The decline was also observed in naupliiand was more marked in small-sized copepod species than in largerones; one species, Centropages typicus, even disappeared. Anincrease in the proportion of carnivorous organisms appearedin both copepods (Euchaeta acuta, Heterorhabdus spp.) and euphausiids(Nematoscelis megalops, Stylocheiron longicorne). These changesare discussed in relation to environmental features and in thecontext of seas-onal variability, the observational period coincidingwith the transition from spring bloom to oligotrophy in thisarea. Effects of a major wind event that appeared to have inducedlong-lasting changes are also explored.     

Seasonal plankton dynamics in a Mediterranean hypersaline coastal lagoon: the Mar Menor

The seasonal distribution of plankton in a Mediterranean hypersalinecoastal lagoon has been studied through a dataset, comprisingthe taxonomic composition and the size–abundance distributionof both phyto- and zooplankton, measured by image analysis techniquesduring a one-year time series of weekly samplings. The studiedorganisms ranged from small nanoplanktonic heterotrophic flagellates(2 µm diameter) to fish larvae (>2 µm). The phytoplanktonannual succession was characterized by a winter period dominatedby Rhodomonas spp. and Cryptomonas spp. with Cyclotella spp.as the main diatom represented, a spring phase where diatoms(mainly Cyclotella) were the dominant group with some monospecificblooms of other diatoms (mainly of Chaetoceros sp.), a summerphase characterized by diatoms with blooms of Niztschia closterium,and a post-summer phase where dinoflagellates increased withpeaks of Ceratium furca. High densities of the microbial foodweb elements, flagellates and ciliates, indicate the importanceof the microbial loop in the ecosystem. Meroplankton contributedwidely to the seasonal character of the zooplankton distribution.Copepods, represented by Oithona nana, Centropages ponticusand Acartia spp. (mainly latisetosa), remained relatively constantthroughout the year, exhibiting a lower density in the warmerwater period (July–September). At the end of the samplingperiod, a massive proliferation of copepods (>1000 ind l^–1), mainly due to O. nana, took place. The autotrophsto heterotrophs biovolume ratio (A:H) remained lower than 1throughout the year except when, occasionally, large phytoplanktoncells bloomed. Persistent very low values of A:H suggest thatadditional sources of energy, such as the microbial loop ordetrital pathways, would be needed to sustain the high heterotrophicbiovolume found in the lagoon.     

Annual Zooplankton Succession in Coastal NW Mediterranean Waters: The Importance of the Smaller Size Fractions

Zooplankton abundance, biomass (biovolume) and taxonomic compositionwere studied within an annual cycle (August 1995–October1996) in the Bay of Blanes (northwest Mediterranean). Weeklyzooplankton sampling included oblique tows made with a 200 µmJuday–Bogorov net, and vertical tows made with a 53 µmnet, to adequately sample both mesoplankton and the smallerzooplankton fractions. Total zooplankton abundance showed highvariability, lacking any clear seasonal pattern. However, thedifferent species within the zooplankton community displayeda clear succession throughout the year. In general, cyclopoidcopepods (Oithona spp.) and cladocerans (Peniliaavirostris)dominated the summer and autumn communities, whereas in winterand spring, calanoid copepods (Clausocalanus spp., Paracalanussp. and Centropages typicus) were predominant. The zooplanktonannual cycle in the Bay of Blanes does not resemble those ofother Mediterraneanlittoral areas, probably due to the inherentparticularity and variability associated with open coastal environments.On average, the abundance of organisms estimated with a traditional200 µm Juday–Bogorov net was 8.1 times lower thanthe values obtained with a 53 µm net. Even if only organisms>200 µm collected in the 53 µm tows were considered,the total abundance within the 53 µm net was still 4.4times higher than the estimates from the Juday–Bogorovnet. These results suggest the need for accurate samplings ofthe entire zooplankton assemblage when characterizing the structureand dynamics of zooplanktonic communities.     

Size-fractionated mesozooplankton biomass, metabolism and grazing along a 50{degrees}N-30{degrees}S transect of the Atlantic Ocean

Size-fractionated mesozooplankton grazing and metabolism wereinvestigated along the wide latitudinal range (50°N–30°S)covered during the Atlantic Meridional Transect (AMT) 11 cruise.Five different oceanic provinces were traversed in this cruise:North Atlantic Drift (NADR), North Atlantic Subtropical Gyral(NAST), Canary Coastal (CNRY), Eastern Tropical Atlantic (ETRA),and South Atlantic Gyral (SATL). CNRY and ETRA were affectedby the upwelling Mauritanian and equatorial respectively andprimary production in these provinces was higher than in theoligotrophic subtropical gyres (NAST and SATL). Both mesozooplanktonand phytoplankton biomass were highest around the equator. Theamount of chlorophyll a ingested daily by copepods was noticeablyhigher in mesotrophic than in oligotrophic provinces as shownby the spatial distribution of gut content values and the highabundances of copepods recorded at the equator. Grazing impactalong the transect ranged from 0.2 to 5.6% of the phytoplanktonstanding stock and from 1.6 to 14.5% of primary production.If only phytoplankton >2 µm are considered, the rangesare 1.0–19.4% (stock) and 3.4–44.7% (primary production).Grazing impact upon both phytoplankton biomass and primary productionfollowed a spatial distribution similar to that of chlorophylla ingestion, with higher values in upwelling zones than in thegyres. Weight-specific rates of respiration and NH₄⁺ and PO₄^3–excretion showed large variability both along the transect andwithin provinces, but did not differ between provinces. Therefore,zooplankton assemblages inhabiting the different provinces visitedin the AMT 11 seem to be adapted to the prevailing thermal conditions.Given the substantial proportion of nitrogen and phosphorusthat are supplied to primary producers through the excretoryactivity of mesozooplankton (the percentage of nitrogen andphosphorus requirements of phytoplankton accounted for by mesozooplanktonexcretion was >30% in all the provinces) it follows thatthey may play a crucial role as nutrient regenerators, especiallyin the oligotrophic gyres where regenerated production dominates.     

Subsurface chlorophyll maxima and vertical distribution of zooplankton in the Gulf of Maine

The vertical disthbution of chlorophyll, zooplankton and physicalstructure were measured using a pumping system and CTD on twocruises in the Gulf of Maine during June and September 1982.The vertical distribution of chlorophyll was closely relatedto the density structure of the water column. In waters witha pronounced pycnocline subsurface chiorphyll maxima (SCM) werelocated at or just above the pycnocline. Chlorophyll concentrationswere maximal in the surface waters at those stations sampledin June where the pycnocline was not well defined. The relationshipbetween the zooplankton and chlorophyll distribution differedbetween cruises. In June, the zooplankton, particularly post-naupliarcopepods, were associated with the depth of the chlorophyllmaxirnum, while in September the post-naupliar copepods weremost abundant in the surface waters above the SCM at the stratifiedstations. During the September cruise we observed that the copepodnauplii were most abundant at the depth of the SCM, and thatthe larger protozoans (>35 µm) were most abundant atdepths of 55–85 m, which were well below the SCM and pycnocline. ^*Bigelow Laboratory for Ocean Sciences Contribution No. 83025     

Vertical distributions of zooplankton across the Almeria-Oran frontal zone (Mediterranean Sea)

The vertical distribution of zooplankton in the upper 700 mof the water column was investigated across the Almeria–Oranfront (Alboran Sea) during winter 1997/98 (Almofront 2 cruise).Eight sites corresponding to three hydrodynamic structures (theAtlantic jet, an anticyclonic gyre and the surrounding Mediterraneanwaters) were explored, by day and at night, using multiple-netsampling. Results are presented for the major species of copepods(>500 µm), macroplankton and microplankton. Speciesinhabiting the surface layer or occupying it at night extendeddeeper in the gyre. On the other hand, mesopelagic species (e.g.Pleuromamma borealis, Pleuromamma abdominalis, Euphausia krohniand Cyclothone braueri) were found to live deeper, at leastby day for the migrants, in the Mediterranean waters comparedwith the two other structures. These changes in preferentialdepths across the front are discussed in relation to environmentalfeatures, such as light level, abundance of food and mixed layerdepth. This study also documented the vertical distributionof some overwintering copepod species (Calanus helgolandicus,Eucalanus hyalinus and Eucalanus monachus).     

Impacts of nutrients and zooplankton on the microbial food web of an ultra-oligotrophic lake

In ultra-oligotrophic lakes and the sea, calanoid copepods arethe dominant mesozoo-plankton and cladocerans are generallysparse or absent. To determine the effects of predation andnutrient enrichment on the pelagic microbial food web of anultra-oligotrophic lake, we added copepods and cladocerans atlow biomasses (<60 µg l^–1 to in situ enclosuresin Lake Wakatipu, New Zealand, in the presence and absence ofadded nutrients (nitrogen and phosphorus). In response to nutrientfertilization, the concentrations of phototrophs >3 µmand heterotrophic bacteria increased by 50 and 15%, respectively,over 4 days, but those of cyanobacterial picoplankton decreasedby 68%. The presence of calanoid copepods (Boeckella dilatata)at ambient densities (1 and 4 l^–1) rapidly and severelysuppressed ciliate population growth over 4 days and also loweredthat of flagellates >3 µm, even when microbial growthwas enhanced by added nutrients. The presence of a small cladoceran,Ceriodaphnia dubia, at double the densities, but similar biomasses,to those of copepods, depressed the net growth rates of ciliatesand flagellates to a lesser degree. The net growth rate of heterotrophicbacteria after 4 days declined with flagellate abundance, consistentwith the possibility of regulation by flagellates. Althoughbacteria and algae increased in response to nutrient fertilization(bottom-up control), predation (top-down control) appeared toplay an important role in structuring the microbial food webof this ultra-oligotrophic lake in summer.     

Copepod grazing impact on the trophic structure of the microbial assemblage of the San Pedro Channel, California

In August 2002 and March 2003 the trophic structure of the microbialassemblage from the San Pedro Channel, California was studiedfollowing the experimental alteration of the number of copepods.Changes in the abundance/biomass of microorganisms <80 µmduring 3-day incubations were monitored in (i) the absence ofmetazoa >80 µm, (ii) the presence of natural abundancesof metazoa and (iii) the presence of an elevated number of copepods.Prokaryotes and small-sized eukaryotes (<4 µm) dominatedplankton biomass during both experimental months. Diatoms numericallydominated the 10–80 µm plankton in August 2002,but ciliate and heterotrophic dinoflagellate biomass generallyexceeded diatom biomass on both dates. Ingestion of protozooplankton(predominantly ciliates) contributed substantially to copepoddaily carbon rations. The adult copepod assemblage removed 4.6and 36% per day of the microzooplankton standing stocks (10–80µm size fraction) in August and March, respectively. Elevatedcopepod grazing pressure on protozooplankton resulted in increasedbiomass of nanoplankton (<5 µm) presumably via a trophiccascade. Accordingly, the copepod–protozoan trophic linkappears to be a key factor structuring the planktonic microbialassemblage in the San Pedro Channel. This paper is one of six on the subject of the role of zooplanktonpredator–prey interactions in structuring plankton communities.     

Basin scale distribution of zooplankton in the Ligurian Sea (north-western Mediterranean) in late autumn

Mesozooplankton biomass and abundance were evaluated in epipelagic waters at 59 stations covering the Italian sector of the Ligurian Sea (north-western Mediterranean) in December 1990. This region is characterised by a cyclonic circulation which encloses a central divergence zone and is associated with a main thermohaline front offshore the western Ligurian coast. At the end of autumn, mesozooplankton biomass (range: 0.80–4.24 mg DW m⁻³) and the abundance (range: 83.8–932 ind. m⁻³) were lower in the divergence zone. On the contrary, in the Ligurian frontal zone at the periphery of the divergence and on the eastern continental shelf the greatest values of biomass and abundance were recorded. Copepods and appendicularians dominated the mesozooplankton community, the main taxa being the copepods Clausocalanus spp. (46% of total zooplankton) and Oithona spp. (15%) and the appendicularian Fritillaria spp. (12%). Three hydrological sub-regions, i.e. the divergence, the eastern continental shelf and the periphery of the divergence, were characterised by different zooplankton communities and characteristic species. Environmental differences between the three zones were mainly related to changes in bottom topography, sea surface temperatures and quantity of particulate organic matter. Vertical mesozooplankton abundance and taxa distribution from the surface to 1,900 m depth were also examined in one station. The results showed that the bulk of the community was concentrated in the upper 200 m, small copepods being dominant particularly in the upper 50 m. The copepod community was more diversified in sub-superficial waters, with a maximum observed in the 200–400 m layer. The distributions of main zooplankton taxa described in epipelagic waters in the eastern Ligurian Sea in autumn were compared with their distribution at surface in the north-western Mediterranean obtained by sampling performed with the Continuous Plankton Recorder in 1997–1999. The analysis of the zooplankton community in CPR samples confirms the dominance of small copepods (Paracalanus spp., Clausocalanus spp., Oithona spp.) and appendicularians in the north-western Mediterranean in late autumn-winter and shows that their distribution is mainly related to the main mesoscale hydrographic features characterising this basin. Guest editors: S. Souissi & G. A. Boxshall Copepoda in the Mediterranean: Papers from the 9th International Conference on Copepoda, Hammamet, Tunisia     

Zooplankton biomass gradient off south-western Nova Scotia: nearshore ctenophore predation or hydrographic separation?

A persistent large-scale cross-shelf gradient in zooplanktonbiomass >1050 µm was evident off south-western NovaScotia during annual spring surveys between 1985 and 1987, withrelatively low levels inshore and higher levels offshore. Conversely,the abundance of the tentaculate ctenophore Pleurobrachia pileuswas the greatest inshore, and distributed reciprocally to zooplankton>1050 µm. The principle prey of both adult ctenophoresand post-larval cod is zooplankton >1050 µm (primarilycalanoid copepods), and cod growth rates are strongly influencedby prey biomass. Ctenophore predation appears to have been responsiblefor the low nearshore zooplankton biomass, whereas the influenceof hydrographic factors on the zooplankton gradient was minimal.On a smaller scale, persistent, abrupt changes in zooplanktonbiomass >1050 µm and ctenophore density existed 3–30km from shore, in contrast to linear gradients in water density(₁) during a 5 week sampling period in spring 1987. Ctenophoreswere confined to depths <55 m and zooplankton >1050 µmpredominantly occurred at depths >55 m. High concentrationsof chlorophyll and phaeopigment were evident at depths <55m also suggesting intense predation by ctenophores on largeherbivores. The relatively high proportion of smaller zooplankton(153–308 –m) in the nearshore is also consistentwith the predation hypothesis. The reduced growth experiencedby post-larval cod inshore appears generated by ctenophore predationof a common prey resource.     

Zooplankton, especially calanoid copepods, in the upper 1000 m of the south-east Arabian Sea

Abstract. Vertical distribution of zooplankton in the upper1000 m was studied from the south-east Arabian Sea in orderto determine the variations in zooplankton at different depths.The distribution and migration patterns of calanoid copepodspecies were given special attention. The mean zooplankton standingstock in the upper 1000 m was 2.1 g dry Wt m^–2, of which97.7% was concentrated in the upper 400 m. Herbivores were generallymore abundant at all depths, but did not predominate. An increasein zooplankton at night occurred in the upper 200 m, as wellas at the 600–1000 m stratum. The maximum diversity ofcalanoid copepods also coincided with these two depths. Basedon vertical ranges, the calanoid copepod species were assignedto three groups: (i) species occurring predominantly in theepipelagic layer and forming the bulk of the calanoids; (ii)relatively sparser deeper living species confined below 200m; and (iii) species occurring throughout the water column.Some amount of vertical niche separation among congeneric specieswas indicated. While some species showed active migration, agood number of species were non- migratory.     

Grazing of copepod assemblages in the north-east Atlantic: the importance of the small size fraction

The North Atlantic was the site for the 1989 JGOFS Pilot Study,an international study of ocean fluxes in relation to the carboncycle. In this paper we present preliminary estimates of thegrazing pressure by copepod assemblages at four stations 60,56, 52 and 47°N, along the JGOFS 20°W transect, duringJune–July. Three major size fractions of mesoplanktoniccopepods were considered, small (200–500 µm), medium(500–1000 µm) and large (1000–2000 µm).At each station, copepod composition and abundance were analysedand the gut fluorescence method was used to estimate ingestionrates. The results support the importance of the small sizefraction relative to the other fractions, in terms of numericalabundance and their grazing impact. However, the total grazingpressure of copepods on phytoplankton was relatively minor duringthe period of sampling since the fraction of phytoplankton standingstock and primary production consumed by the copepods was onaverage <1 and 2% respectively. The implications of theseresults as well as the potential sources of bias involved inthese types of measurements and estimations are discussed.     

Diurnal residence of the larger stages of the calanoid copepod Acartia tonsa in the anoxic monimolimnion of a tropical meromictic lake in New Guinea

We studied diel vertical migration of the calanoid copepod Acartiatonsa in a coastal meromiclic lake (Lake Nagada, Papua New Guinea).During the day, the animals migrate several metres below theoxycline to just above or into the sediments, and remain inanoxic water. Vertical migration patterns differ between ontogeneticstages; adults and larger copepodites do not occur in appreciablenumbers in the water samples during the day (deepest sampletaken at {small tilde}0.5 m above the sediment). Around sunset,the larger copepodites gradually appear in the water column,reaching the near-surface food layer (0–2 m) only wellafter sunset. Our results suggest that the evening ascent ofthe copepods in this tropical lake is related to relative changesin light intensity, and that there are age- and sex-relateddifferences in the responses to these stimuli.     

A comparison of performance of WP2 and MOCNESS

Zooplankton biomass in the Barents Sea was monitored during1988–97 using WP2 and MOCNESS plankton nets. These twosampling gears differ in their size and mode of operation. Theplankton samples were size fractionated into three categoriesand the dry weight per square metre was calculated. The smallestand the medium size fractions (< 2000 µm) representedmainly copepods, and the larger size fraction (> 2000 µm)consisted mainly of macrozooplankton such as krill and amphipods.WP2 biomass values were higher for the smallest size fraction,whereas the MOCNESS tended to give higher values for the largestsize fraction However, the total amount of zooplankton biomass(g m^–1) obtained by these two methods was not significantlydifferent.     

Spatial and temporal distribution of mesozooplankton in the Gulf of Aqaba and the northern Red Sea in February/March 1999

The distribution pattern, taxonomic composition and communitystructure of mesozooplankton was studied along a transect with10 positions between the Gulf of Aqaba and the northern RedSea. Five positions were resampled two or three times duringa cruise of RV ‘Meteor’ in February/March 1999.In spite of clear differences in the density stratificationbetween the Gulf of Aqaba and the northern Red Sea, the mesozooplanktoncomposition was very similar: Copepods were by far the mostabundant taxon, contributing 76–95% to the total community.The remainder was composed largely of ostracods, chaetognaths,appendicularians and molluscs. The mesozooplankton of the deeplymixed stations was homogeneously distributed, at all other stationsthe bulk of the mesozooplankton (>70%) was concentrated inthe mixed surface layer with peaks of calanoids, cyclopoidsand appendicularians in the vicinity of the chlorophyll a (Chla) maximum layer. Ostracods and poecilostomatoids dominatedthe layers below. Standing stocks within the total water column(550–1200 m) varied between 93 and 431 x 10³ individualsm^–2 for copepods and 5–76 x 10³ individuals m^–2for other mesozooplankton with highest numbers in the northernGulf of Aqaba, where vertical mixing was deep (400–500m) and Chl a and mesozooplankton distributions homogeneous throughoutthe water column. Towards the south, the mixed depth decreasedfrom 300 m in the central Gulf of Aqaba to 50 m in the Red Sea.Cluster analysis separated three distinct groups of stations,compounding the observed differences between the northern Gulfof Aqaba (Position I) and the other positions. The analysisalso revealed temporal differences between the February andMarch sections of the cruise, indicating the winter–springtransition. The stations sampled in March are characterisedby a higher total abundance and by a higher percentage of appendiculariansand ostracods than the stations sampled in February     

Effects of Planktonic Copepods on Transparent Exopolymeric Particles (TEP) Abundance and Size Spectra

Diatoms exude considerable quantities of polymers, mainly polysaccharides,that play an important role in the process of sestonic particleaggregation in the sea. We investigated the impact of copepodson transparent exopolymeric particles (TEP) generated by thediatom Thalassiosira weissflogii. Grazing experiments with ¹⁴C-labelledalgae exudates demonstrated that copepods typical of the BalticSea were not actively filtering TEP. Control experiments showedthat ‘uptake’ of radioactivity could be ascribedto passive uptake, such as adsorption of radioactively-labelledparticles to the body surface. Furthermore, we tested the effectof copepods on TEP size spectra. The abundance and size distributionof TEP (from 1.4 to 180 µm of Equivalent Spherical Diameter)were analysed in a 4 h incubation experiment. In the presenceof copepods, the proportion of larger TEP was higher. An increasein total volume of TEP in jars containing copepods (~2 x 10⁷µm ml^–1) compared with control jars without copepods(~0.5 x 10⁷ µm³ ml^–1) was also observed. The processof aggregation of TEP demonstrated in this work, whereby copepodsincrease downward particle flux without consuming carbon, canhave far-reaching consequences for carbon fluxes along the watercolumn and for copepods feeding dynamics.     

Correspondence among methods of zooplankton biomass measurement in lakes: effect of community composition on optical plankton counter and size-fractionated seston data

The effectiveness of the optical particle counter (OPC) to estimatezooplankton biomass depends on the variability in zooplanktonshape and the presence of interfering particles. In marine environmentswhere zooplankton are composed of similarly shaped copepods,an average shape is relatively easily obtained. However, infreshwater environments, spheroid cladocerans mix with ellipsoidcopepods and make the application of a single morphometric modeldifficult. To expand the use of the OPC to freshwater environments,we developed new ellipsoid models for three common lake types(eutrophic, mesotrophic, and oligotrophic). In addition, weassessed how closely different size fractions of seston correspondedto zooplankton biomass. When expressed in common dry mass units,OPC- and seston-derived zooplankton biomass estimates showeda 1:1 correspondence with taxonomically derived estimates inproductive lakes (r > +0.70, P < 0.001) but not in oligotrophicsystems. OPC ellipse models differed among lake sets (major-to-minoraxis ratio: 1.5 to 2.7) but were not a simple function of thecladoceran-to-copepod ratio. The seston size fraction that providedthe best estimates of zooplankton biomass was smaller in mesotrophiclakes (>200 µm) than in eutrophic or oligotrophic lakes(>500 µm). The presence of algae and rotifers had nodetectable influence on OPC and size-fractionated seston estimates.Overall, these analyses suggest that OPC and seston providereliable estimates of lacustrine zooplankton biomass as longas region-specific ellipse models and size fractions, respectively,are used.     

Seasonal and interannual variability of size-fractionated phytoplankton biomass and community structure at station Kerfix, off the Kerguelen Islands, Antarctica

Time series of phytoplankton biomass and taxonomic compositionhave been obtained for the 3 years 1992, 1993 and 1994 in thenorthern part of the Southern Ocean (station Kerfix, 5040'S,6825;E) Autotrophic biomass was low throughout the year (<0.2mg m^–3 except during a short period in summer when a maximumof 1.2 mg chlorophyll (Chl) a m– was reached. During winter,the integrated biomass was low (<10 mg m^–2) and associatedwith deeply mixed water, whereas the high summer biomass (>20mg m^–2) was associated with increased water column stability.During summer blooms, the >10 µ;m size fraction contributed60% to total integrated biomass. Large autotrophic dinoflagellates,mainly Prorocentrum spp., were associated with the summer phytoplankton maxima and accounted for >80% of the total autotrophcarbon biomass. In November and December, the presence of thelarge heterotrophic dinoflagellates Protoperidinium spp. andGyro dinium spp. contributed a high proportion of total carbonbiomass. During winter, the <10 µm size fraction contributed80% of total Chi a biomass with domination of the picoplanktonsize fraction. The natural assemblage included mainly nakedflagellates such as species of the Prasinophyceae, Cryptophyceaeand Prymnesiophyceae. During spring, picocyanobacteria occurredin sub-surface water with a maximum abundance in September of106 cells 1^–1     

Biomass, feeding and production of Noctiluca scintillans in the Seto Inland Sea, Japan

The abundance and biomass of the large heterotrophic dinoflagellateNoctiluca scintillans, together with the changes in its potentialprey items, were monitored in the Seto Inland Sea, Japan, duringsummer 1997 (17 July-11 August). Growth and grazing rates ofNscintillans fed natural plankton populations were also measuredeight and seven times, respectively, during the survey period.The abundance and biomass of N scintillans averaged over thewater column (19 m) were in the range 1–345 cells 1^–1(temporalaverage = 93 cell1^–1) and 0.1–49.6 µg C l^–1(temporalaverage = 13.8 µg C l^–1; three times higher thanthat of calanoid copepods during the same period). Noctilucascintillans populations followed the changes in phytoplankton:N.scintillans biomass was increasing during the period of diatomblooms and was at a plateau or decreasing during periods oflow chlorophyll a. The growth rates of N.scintillans (µ)were also consistent with the wax and wane of the N.scintillanspopulation: N.scintillans showed highest growth rates duringdiatom blooms. A simple relationship between µ and chlorophylla concentration was established, and the production of N.scintillanswas estimated using this relationship and the measured biomass.The estimated production averaged over the water column wasin the range >0.1–5.2 µg C l^–1 day^–1(temporalaverage = 1.4 µg C l^–1 day^–1; 64% of the productionof calanoid copepods during the same period). Diatom clearancerates by N.scintillans were in the range 0.10–0.35 mlcell^–1 day^–1, and the phytoplankton population clearanceby N.scintillans was >12% day^–1. Thus, although thefeeding pressure of N.scintillans on phytoplankton standingstock was low, N.scintillans was an important member of themesozooplank-ton in terms of biomass and production in the SetoInland Sea during summer.     

Remote detection of algae by copepods: responses to algal size, odors and motility

Selective feeding on large algae by copepods involves remotedetection of individual particles and subsequent active captureresponses In this study we use radiotracer experiments to quantifythe clearance rates of five coexisting freshwater copepods andto investigate the relative merits of the chemoreception andmechanoreception hypotheses of remote detection Tropocyclopsand three diaptomid copepods exhibited relatively high clearancerates when feeding on low concentrations of large algae, suggestingthat most previous studies with freshwater copepods have underestimatedmaximal clearance rates and the degree of size selectivity.All five species of copepods exihibited strong selection foran intermediate-sized flagellate (25 µm Cartena) or alarge-sized nonmotile alga (80 µ.m Pediastrum) over asmall-sized flagellate (6 µ.m Chlamydomonas). The weight-specificclearance rate for Tropocylops prasmus feeding on motile Cartena(271 ml mg^–1 h^–1) was about twice that of threediaptomid copepods and more than an order-of-magnitude higherthan the estimate for Epischura lacustris feeding on its preferredalga, Pediastrum Assuming that distance chemoreception (‘smell’)is important in remote detection, we predicted that the additionof high concentrations of ‘algal odors’ would obscureany chemical gradients emanating from individual algal cellsand would thereby hinder the remote detection and active captureof large algae Contrary to this hypothesis, the addition ofamino acids, sucrose, and algal extracts had no effect on theclearance rates and selectivity of Diaptomus birgei. These results,together with recent cinematographic studies (Vanderploeg etal.,1990), suggest that mechanoreception is the primary mechanismfor the remote detection of large particles by diaptomid copepods.A raptorial cyclopoid, Tropocyclops prasinus, exhibited strongpreferences for motile algae, whereas a suspension-feeding calanoid,D birgei, did not select between motile and nonmotile cells.Motility appears to be an important factor in algal detectionfor small cyclopoid copepods but not for suspension-feedingdiaptomids