The family Xystonellidae (Ciliophora, Tintinnina) in the Adriatic Sea

This paper reports quantitative, horizontal and vertical distributiondata of the 11 species of the family Xystonellidae found inthe Adriatic Sea and in the Strait of Otranto. The samples werecollected in coastal and open waters, with a plankton net equippedwith a closing system, in the period from 1973 to 1986. At thedeeper stations of the South Adriatic Pit, hauls were takenin eight vertical layers, while at other stations sampling dependedon the respective depth of each station. Xystonellidae are oceanictintinnines, mainly present in the South Adriatic and the Straitof Otranto throughout the year. They are characteristic of SouthAdriatic and Eastern Mediterranean water masses. Horizontaldistribution of lower mesopelagic species is limited by the200 m isobath. Only sparse individuals of the upper mesopelagicand epipelagic species were found in the Jabuka Pit, probablydue to the late autumn and winter current. These species werenot registered to the north of this region. They were registeredbelow the 200 m depth as dominant tintinnines, while in summerthey represented an average of 81% of the total tintinnine population.     

Vertical distribution and abundance of juvenile chaetognaths in the Weddell Sea (Antarctica)

The composition, abundance and vertical distribution of chaetognaths were analysed along a transect in the Weddell Sea during late spring. Three species were identified: Eukrohnia hamata (90.8%), Sagitta marri (6.4%) and S. gazellae (2.8%). Only juvenile stages were collected in the samples, a result related both to the type of sampling gear employed (mesh size: 100 μm) and the species' life-cycles. The vertical distributions showed that the juvenile stages of these species tended to aggregate at considerable depth (1000–500 m). It is postulated that this pattern may be related to the life-cycles of these species in association with seasonal Antarctic conditions, similar to the pattern postulated for krill and other polar crustaceans. Accepted: 10 July 2000     

Bathymetric distribution of medusae in the open waters of the middle and south Adriatic Sea during spring 2002

Twenty-eight species of hydromedusae and one scyphomedusa werecollected from the middle and south Adriatic in Spring 2002.Haliscera bigelowi was recorded for the first time in the AdriaticSea and Dicodonium adriaticum for the southern Adriatic. Thecosmopolitan species Rhopalonema velatum, Aglaura hemistomaand Persa incolorata averaged 88% of total medusan abundance.The Mediterranean species Rhabdoon singulare and Solmissus albescenswere numerous at the deeper stations. These species were foundeither in the southern or in middle Adriatic, and their abundanceis greater than in other regions of the Mediterranean Sea. Speciesdiversity and abundance generally were highest in the upper200 m and decreased with depth. Diel vertical migration patternsincluded some species that nocturnally sought shallower or deeperlayers, and some species migrated in both directions. A fewspecies did not show any vertical migration. Although lightlikely triggers vertical movements, data suggest that foragingstrategies also influence the vertical migration of medusae.     

Distribution and feeding of chaetognaths in the epipelagic zone of the Lazarev Sea (Antarctica) during austral summer

This study seeks to determine the effects of local hydrography on the distribution, abundance and feeding of chaetognaths in the Lazarev Sea, an area strongly controlled by physical processes which has been held responsible for initiating the Weddell Polynya. Zooplankton samples were taken at 39 stations on four transects located between 6°W and 3°E and from 60°S to 70°S between surface and 350 m. The dominant species, Eukrohnia hamata, accounted for 86.5% of all chaetognaths, followed by Sagitta gazellae (8.1%) and Sagitta marri (5.4%). These three species showed distinct vertical and horizontal distribution patterns. While E. hamata and S. marri had maximum abundances below 250 m depth, S. gazellae showed a narrow distribution band in the upper 150 m depth. The distribution pattern was strongly modified at the Greenwich meridian with an upward transport of a high abundance of deep dwelling organisms (S. marri and E. hamata) and a displacement of S. gazellae to the surface, likely coupled with the rise of the warm, saline halo around the Maud Rise. Small copepods were the main prey of all three chaetognath species. Feeding rates (FR) varied among species and depth. Sagitta marri showed the highest FR with 0.38 prey d⁻¹, followed by S. gazellae and E. hamata (0.22 and 0.07 prey d⁻¹). Feeding rates were usually highest in the 25–80-m stratum. Size distribution and maturity of E. hamata revealed a dominance of small and immature organisms along all depths and stations, suggesting that this area might be acting as an important source of recently spawned organisms to the surface.     

Vertical distribution of protozoan and microcopepod communities in the South Adriatic Pit

The qualitative composition, numerical abundance and verticaldistribution of radiolarians, tintinnines, nauplii and smallcopepod assemblages were studied in the central area of theSouthern Adriatic Pit at three stations during 10 cruises fromOctober 1985 to May 1990. The samples were collected with aplankton net of 53 µm mesh size equipped with a closingsystem in eight vertical layers. Data are presented for 53 radiolarians,61tintinnines and for the first time for 22 poecilostomatoidspecies in the Adriatic Sea. According to the numerical abundanceof assemblages and the frequency of occurrence of the bulk ofthe individual species population in the water column, fourcommunities could be defined: the surface (0–50 m), thesubsurface (50–100m), the midwater (100–600 m) andthe deep-sea community (below 600 m). The euphotic layer wascharacterized by tintinnines, copepod nauplii, cyclopoids andjuvenile calanoid copepods, while radiolarians and poecilostomatoidcopepods dominated in the deeper layers. The highest numericaldifferences between stations and seasons were noted only onthe surface. Towards the deeper layers, the differences wereconstantly smaller, and below400 m there was a uniform distributionof all assemblages. This research, on the basis of the numericalabundance of protozoans and micrometazoans, shows that the centralpart of the South Adriatic Pit is considerably richer than mentionedby earlier authors.     

东海表层沉积中的翼足类及其地质意义

对东海84个表层沉积中翼足类进行了定量分析,共获得7属15种,其中Limacinainflata在陆架外缘和上陆坡为优势种,Limacinatrochi formis,Creseisacicula和Creseis virgule在中外陆架最为丰富。根据翼足类的深度分布确定东海现代文石补偿深度在约600m水深处。以冲绳海槽北部柱状样B3GC为例,说明翼足类是研究地质时期古海洋学变化的重要证据。     

Demographic structure and distribution of John Dory, Zeus faber L. 1758, in the Adriatic Sea

Recent demographic structure and distribution of the fish species Zeus faber in the Adriatic Sea were investigated in this study and compared with a 1948–1949 study. The presence of John Dory in the Adriatic Sea was recorded at a depth range from 21 to 239 m, with the highest biomass indices at depths between 50 and 100 m. The length frequency distribution, length–weight relationships, sex ratio and length at first sexual maturity were determined. Results based on data from the 1948–1949 ‘Hvar’ expedition and the MEDITS surveys of 1996–1998 showed in the 50‐year interval that the index of biomass and area of distribution of this species in the Adriatic Sea have been reduced and that the demographic structure of the population has changed. Negative changes described in the paper indicate an overfishing of the Z. faber species in the Adriatic Sea.     

Vertical distribution of pelagic chaetognaths and feeding of Sagitta enflata in the Central Equatorial Pacific

The vertical distribution and feeding of pelagic chaetognathsat 5°S, 160°W in the Central Equatorial Pacific wereinvestigated using a series of 0–500 m vertical haulswith a VMPS net over a 24 h period between 6 and 7 October 1990.The total number of individuals per haul was between 370 and688. Fourteen species in four genera were found at this station.The most abundant species was Sagitta enflata which comprised32.4–61.1% of the individuals collected from the 0–500m layer. Mesopelagic species made up 9.3–15.1% of thetotal number of individuals. Sagitta enflata and Pterosagittadraco were found in the upper part of the thermocline both byday and at night. The fraction of the population containingfood items (FCF) of S.enflata in the 0–50 m layer variedbetween 4.8 and 12.5% (mean 10.8%) and feeding activity washighest between sunrise and noon. The percentages of Copepoda,Foraminifera, crustacean larvae, Chaetognatha, Pteropoda, Ostracoda,fish and unidentified material in the gut of S.enflata were51.9,6.7,3.8,2.9,1.9,1.9 and 30.9%, respectively. Sagitta enflataconsumed food organisms which were mainly between 0.5 and 1.0mm in length. The daily feeding rate of S.enflata was 1.81 preyper individual, which was equivalent to 8.06 mg C m^–2day^–1. This corresponded to     

Chaetognatha of the Namibian Upwelling Region: Taxonomy,Distribution and Trophic Position

In October 2010, the vertical distribution, biodiversity and maturity stages of Chaetognatha species were investigated at four stations located off Walvis Bay, Namibia. Seventeen species were detected and classified as pelagic, shallow-mesopelagic, deep-mesopelagic and bathypelagic species based upon the weighted mean depth derived from their average vertical distribution. High abundances of Chaetognatha were found in the upper 100 m at all stations of the Walvis Bay transect with a maximum value of 20837 ind. 1000 m⁻³ at the outer shelf station near the surface. The community was dominated by species of the Serratodentata group. Furthermore, the distribution of Chaetognatha did not seem to be influenced by low oxygen concentrations. Stable isotope ratios of carbon and nitrogen in Chaetognatha were determined for seven different areas located off northern Namibia. The values of δ¹⁵N ranged from 6.05 ‰ to 11.39 ‰, while the δ¹³C values varied between −23.89 ‰ and −17.03 ‰. The highest values for δ¹⁵N were observed at the Walvis Bay shelf break station. The lowest δ¹³C values were found at the Rocky Point offshore station, which was statistically different from all other areas. Stable isotopes of carbon and nitrogen were determined for four taxa (Sagitta minima, Planctonis group, Sagitta enflata, Sagitta decipiens). In this case, the δ¹⁵N values ranged from 6.17 ‰ to 10.38 ‰, whereas the δ¹³C values varied from −22.70 ‰ to −21.56 ‰. The lowest δ¹⁵N values were found for S. minima. The C- and N-content revealed maximum C-values for S. decipiens and maximum N-values for the Planctonis group. The C:N ratio of Chaetognatha ranged between 5.25 and 6.20. Overall, Chaetognatha are a diverse group in the pelagic food web of the Benguela Upwelling System and act as competitors of fish larvae and jelly fish by preying on copepods.     

Species composition and depth distribution of chaetognaths in a Kuroshio warm-core ring and Oyashio water

Chaetognath species composition, diversity and depth distributionwere investigated inside and outside a warm-core ring off thenorth-east coast of Japan. Time series samples were collectedat a station inside a Kuroshio warm-core ring (KWCR) and ata station in the surrounding Oyashio water. Greater mean abundanceof 2.51 ± 0.116 (mean ± SE) chaetognaths m^-3 wasfound outside the ring compared with 1.75 ± 0.321 chaetognathsm^-3 collected within the ring. However, species diversity valueswere higher within the KWCR (Shannon–Weaver index). Eukrohniahamata was the dominant species outside the ring, comprising79.8–87.9% of the total chaetognaths per haul. Inside,Sagitta minima was dominant, comprising 35.1–44.3%. MostE. hamata were collected in deeper layers within the KWCR andtheir abundance was on average only 9% of that found in theOyashio region. Only E. hamata and Sagitta scrippsae had differentdepth distributions in the KWCR. The vertical distribution ofE. hamata by body size appeared altered by the KWCR. Althoughthe mean length of E. hamata was not significantly differentbetween regions, sexual development appeared inhibited in thering. Sagitta elegans collected in the KWCR were mostly smallin size (<10 mm), significantly smaller than in the Oyashiowater.     

Vertical distribution and ecological significance of chaetognaths in the Arctic environment of Baffin Bay

Summary The vertical distributions of species of chaetognaths are described to a depth of 1043 m in Baffin Bay during the summer. The dominant species in the southern region of the Bay were Eukrohnia hamata and Sagitta maxima and, in the northern region, E. hamata and S. elegans. The younger stages of all chaetognath species were found at depths above the older more mature stages. There was no evidence of any diurnal vertical migration by any species. The population structure of E. hamata was bimodal suggesting two sub-populations and a two year life cycle. Sagitta maxima showed a multimodal population suggesting a life cycle of four or more years. The population structure of E. elegans was unimodal. Gut contents showed that E. hamata fed at a higher rate than did S. maxima. E. hamata fed at a higher rate during the night but there was no significant difference between day/night feeding rates for S. maxima. It was estimated that E. hamata consumed up to 1.8 prey items day^-1 and S. maxima 0.5 prey items day^-1. The daily ration was influenced by the water temperature. Calculations showed chaetognaths are major predators on copepods consuming between 1.2 and 1.3% of the standing crop of copepods per day. Generally the maximum concentration of chaetognaths was found at a depth below the maximum concentration of copepods.     

Meso- and bathypelagic distribution and abundance of chaetognaths in the Atlantic sector of the Southern Ocean

We conducted multinet sampling during winter and summer in the Southern Ocean (Atlantic sector) to investigate the effect of water mass, season and water depth on abundance and species composition of meso- and bathypelagic chaetognaths. Eukrohnia hamata (mean 115 ind. 1,000 m⁻³) and Sagitta marri (mean 51 ind. 1,000 m⁻³) were dominant, complemented by E. bathypelagica (mean 19 ind. 1,000 m⁻³) and E. bathyantarctica (mean 19 ind. 1,000 m⁻³) below 1,000 m. A further six species were identified, among them the rare bathypelagic species Heterokrohnia fragilis and the subtropical Eukrohnia macroneura that is new to the Antarctic. Water depth and season were the principal determinants of abundance and species composition patterns, indicating vertical seasonal migration and vertical segregation of species. The life cycles of E. hamata and S. marri were studied additionally. Their maturity stages were vertically segregated and prolonged reproductive periods are suggested for both species.     

Notes on feeding of Chaetognatha in Guanabara Bay, Brazil

A preliminary analysis, by means of the gut content, of thediet of Sagitta friderici and Sagitta enflata occurring in GuanabaraBay was carried out. The samples were collected at differenttimes over a 4day period in September 1995, during verticaltows with a conical net of 200 µm mesh size at a fixedstation (30 m depth). In total, 1000 individuals were examined.Copepoda were the numerically dominant group of prey of S.fridericiand S.enflata (67.2 and 74.6%, respectively); both species behaveas opportunistic carnivores, feeding mainly on the more abundantcopepod species throughout the water column. Adult individualsof S.fnderici and S.enflata (stages III and IV) seem to havefood requirements different from juveniles: adults fed on otheritems (chaetognaths, crus tacean larvae, hydromedusae and luciferidae),and the food containing ratio (FCR) was higher in indi vidualsof stage Ill. In general, only one prey per gut was registered.Chaetognaths may have chosen their prey in relation to theirsize, since the size of the prey was proportional to the sizeof their predators. Feeding intensity (NPC) was higher in individualscollected during the night periods.     

THE CLICK-SOUNDS OF NARWHALS (MONODON MONOCEROS) IN INGLEFIELD BAY, NORTHWEST GREENLAND

We studied the sounds of narwhals ( Monodon monoceros ) foraging in the open waters in Northwest Greenland. We used a linear, vertical array of three hydrophones (depth 10 m, 30 m, 100 m) with a fourth hydrophone (depth 30 m) about 20 m from the vertical array. A smaller fifth hydrophone (depth 2 m) allowed for registering frequencies up to 125 kHz (± 2 dB) when signals were recorded at 762 mm/set on an instrumentation tape recorder. Clicks were the prevalent signals, but we heard whistles occasionally. We separated the clicks into two classes: click trains that had rates of 3-10 clicks/sec and click bursts having rates of 110-150 clicks/sec. The spectra of train clicks had maximum amplitudes at 48 ± 10 kHz and a duration of 29 ± 6 psec. The spectra of burst clicks had maximum amplitudes at 19 ± 1 kHz and a duration of 40 ± 3 psec. By analogy with other dolphin species, narwhals presumably use the clicks for echolocation during orientation and for locating prey. The narwhal click patterns resemble those of insectivorous bats. Click trains might correspond to bat searching signals and click bursts to the bat's terminal "buzz", emitted just before prey capture.     

Impact of date mussel harvesting on the rocky bottom structural complexity along the Istrian coast (Northern Adriatic, Croatia)

A survey of 50 km of the coast, including islands, rocks and offshore shallows, in the region of Rovinj (North Adriatic, Croatia) showed that the harvesting of the European date mussel Lithophaga lithophaga (L., 1758) is restricted to inclined, approximately vertical, surfaces. Usually, a stratum of rock, varying from several to about ten cm is removed by hammering, resulting in the complete eradication of sessile organisms. The damage was heavily widespread up to 6 m depth (47% of the total inclined surfaces for the whole area). Between 6 and 14 m depth, the damage was much less (14% from 6 to 10 and 7% from 10 to 14 m depth); below this depth, no damage was observed. The damage patterns coupled with the date mussel distribution, which was constrained by the nature of the substratum (limestone or dolomitic limestone), the general architecture of the rocky bottom and the depth. The structural complexity of inclined surfaces was quantified by 5 indices previously used in biota-substratum interaction studies. Heights of 11 pins placed 3 cm apart in a profile gauge were measured to determine the standard deviation of heights, the coefficient of variation of heights, the sum of squared heights, chain and tape ratio and circular variance of angles. Comparisons of these indices, among damaged and intact surfaces in different habitats and sites within habitats, showed a substantial decrease in complexity of the rocky substratum due date mussel harvesting. Thus, this human disturbance can permanently affect rocky shallow water communities as physical features of the substratum may exert strong effects on species.     

Long-term changes in distribution and demographic composition of thornback ray, Raja clavata, in the northern and central Adriatic Sea

Population structure and distribution of the thornback ray, Raja clavata , L. 1758, in the northern and central Adriatic Sea were described based on data from bottom trawl surveys conducted in the area between 1996 and 2006 within the scope of the 'MEDITS' project. R. clavata was caught at depths between 23 and 270 m; highest abundance and density indices were recorded at a depth stratum 50–100 m. The sex ratio was close to 1 : 1. Length at first sexual maturity for both sexes was calculated. Length–weight relationships were obtained for males, females and the whole sample. Calculated parameters of the length–weight ratio showed a positive allometry for both sexes. The recent state of the population was compared with data from the 1948–49 'Hvar' expedition. The comparison revealed that significant changes have occurred in distribution and abundance of R. clavata in the Adriatic Sea since the time of the 'Hvar' expedition. During the 1948–49 'Hvar' expedition R. clavata was distributed throughout the entire continental shelf; during the 1996–2006 MEDITS expedition the species was found only in restricted areas and with much lower abundances. Significant changes also occurred in the demographic composition of the population. All described changes indicate an over-fishing of the thornback ray in the Adriatic Sea, a result of the high fishing intensity to which the species has been exposed for the past 60 years.     

Composition, spatial and temporal variations of Chaetognatha in Guanabara Bay, Brazil

This paper presents the specific composition and distributionof adult chaetognaths in Guanabara Bay, Brazil. A comparisonhas been made between chaetognath and copepod distribution patterns.Three areas were distinguished within Guanabara Bay: an externalarea, influenced by oceanic waters; an internal area, influencedby fluvial waters; and a transitional area between the two.Monthly samples were collected by horizontal surface hauls usinga conical net with 200µm mesh. Three species were identified:Sagitta friderici, S.enflata and S.hispida. Sagitta fridericiwas the dominant species and occurred throughout the year atthe three areas. Sagitta enflata and S.hispida were limitedto the more saline waters. Generally, greater densities of chaetognathswere observed following copepod peakden sities. Temperatureand salinity associated with copepod abundance were the mostimportant factors affecting the distribution pattern and theabundance of chaetognath species in Guanabara Bay.     

Vertical zonation patterns for Mediterranean copepods from the surface to 3000 m at a fixed station in the Tyrrhenian Sea

The vertical zonation and community structure of Mediterraneancopepods collected from the surface to 3000 m in the TyrrhenianSea were examined for different depth intervals and periodsof the year. Three major copepod communities, identified usingmultivariate analysis techniques, differed mainly in speciescomposition and less in depth distribution from those reportedfor the open ocean. The surface community (0–100 m) includednumerous offshore species comprising relatively uniform butquantitatively poor populations. These included a number ofcoastal forms that dominated offshore waters at certain periodsof the year. The midwater community (100–600 m) consistedof species that were primarily confined to intermediate waters,of which few underwent extensive vertical migrations. The deepcommunity (>600 m) consisted essentially of intermediate-water species with ample distribution ranges that formed a truebathypelagic community at these depths. Temporal changes incommunity structure affected only surface populations and diminishedvery rapidly with increasing depth. Species composition in deeplayers was not affected by did and seasonal changes. Biomassdistribution patterns indicated that the low quantities of planktonrecorded for deep layers were probably related to low surfacestanding crops for this region. The relationship between surfaceand deep biomass values appeared similar to those reported foropen ocean systems suggesting that the efficiency of the deepMediterranean subsystem was not offset by the absence of a truebathypelagic fauna.     

Mesozooplankton community structure in the Southern Ocean upstream of the Prince Edward Islands

A meso-scale oceanographic grid survey was conducted during the first cruise of the Marion Offshore Ecosystem Variability Study in the upstream region of the Prince Edward Islands in austral autumn (April/May) 2001. Mesozooplankton samples, collected using a Bongo net (fitted with 200-µm and 300-µm mesh nets), were separated into three size fractions, 200-500 µm, 500-1,000 µm, 1,000-2,000 µm, by reverse filtration. Total surface (depth<5 m) chlorophyll-a concentration during the study ranged between 0.11 and 0.34 µg l^-1 and was always dominated by picophytoplankton (0.45-2.0 µm). Total mesozooplankton abundance and biomass during the survey ranged between 49 and 1,512 ind. m^-3 and between 0.7 and 25 mg Dwt. m^-3, respectively. Throughout the survey, the 200 to 500 µm class numerically dominated the mesozooplankton community, with an average of ~69% (SD=ᆠ.3%). The dominant species in the 200- to 500-µm size fraction were the copepods, Oithona similis, Calanus simillimus and Metridia lucens, and the pteropod, Limacina retroversa. However, in terms of biomass, the 1,000- to 2,000-µm group was predominant, with dry weight values constituting an average of ~66% (SD=ᆞ.2%). The most well-represented species in this group were the carnivorous Euphausia vallentini, Thysanoessa vicina, Sagitta gazellae and Eukrohnia hamata. Three distinct groupings of stations were identified by numerical analysis. The different station groupings identified reflect changes in the relative contributions of the dominant species, as opposed to the presence/absence of species.     

舟山渔场及邻近海域浮游动物数量分布特征

依据2006年8月(夏)、2007年1月(冬)、5月(春)和11月(秋)在舟山渔场及其邻近海域(29°30′-31°30′N,124°30′E以西)开展海洋生态系统综合调查时,用浅水Ⅰ型浮游生物网采集的浮游动物样本资料,分析了浮游动物总丰度及中华哲水蚤(Calanus sinicus)、精致真刺水蚤(Euchaeta concinna)、百陶箭虫(Sagitta bedoti)、肥胖箭虫(Sagitta enflata)等主要种类的数量分布和季节变化特征。结果表明:调查海域浮游动物平均丰度季节变化明显,春季(555.87ind./m3)夏季(270.87ind./m3)秋季(138.39ind./m3)冬季(127.70ind./m3);其水平分布呈现南部高、北部低的特点。中华哲水蚤为广温广盐种,春季数量最大且分布均匀,大部分海域丰度≥100.00ind./m3;夏季丰度急剧下降,主要分布在30°00′N以南海域;秋、冬季丰度较低,无明显高密集区。精致真刺水蚤为热带种,以夏、冬季丰度较高,主要分布在沿岸水与外海高盐水交汇区和调查海域的南北两端;春、秋季丰度较低且分布均匀。百陶箭虫、肥胖箭虫分别属于暖水种和热带大洋性种,冬、春季丰度都很低,无明显密集区,夏、秋季丰度较大。百陶箭虫主要分布在盐度梯度较大、外海高盐水与沿岸水的交汇区,肥胖箭虫则主要分布在外海高盐水与沿岸水交汇区的靠高温高盐水一侧,其分布与外海高温高盐水的消长有密切关系,可作为暖流指示种。温盐和水系消长变化是影响舟山渔场及邻近海域浮游动物丰度水平分布的重要因素。