Spatial variations in size, weight and condition factor of the females of Acartia clausi (Copepoda: Calanoida) along a salinity gradient in two contrasting estuaries of the Basque coast (Bay of Biscay)

Variations in prosome length and width, dry weight and condition factor of female Acartia clausi copepods were studied at three salinities (35, 34 and 33 psu) in the euhaline region of two estuaries (Bilbao and Urdaibai) of the Basque coast, with different level of anthropogenic impact. Effect of the environmental variables upon the morphology of A. clausi females on a small geographic scale is discussed. In general, biometric variables showed no significant differences between the two estuaries, but dry weight and condition factor were significantly higher in the estuary of Urdaibai at 35 and 34 psu, whilst at 33 psu they were higher in Bilbao. Body dimensions decreased significantly with decreasing salinity in both estuaries, however, no similar trends were observed for dry weight and condition factor. Temperature appeared the main variable to account size variations, but once eliminated seasonal effect of the temperature body size was related with oxygen concentration in the estuary of Bilbao and with salinity in Urdaibai. This study reveals that morphological characteristics of A. clausi not are only dependent on the temperature, but also, within a limited geographical zone, on local differences in environmental variables, mainly salinity and oxygen concentration.     

Organic Matter,Carbon, Nitrogen and Phosphorus Contents of the Mesozooplankton,Mainly Acartia clausi,in a Tropical Brackish Lagoon (Ebrié Lagoon,Ivory Coast)

Mesozooplankton samples were collected over a period of one year in five stations of the Ebrié lagoon and analysed for organic, carbon, nitrogen and phosphorus contents. When zooplankton was dominated by A. clausi, body composition was relatively stable compared with the broad variability of environmental factors (mainly salinity, food abundance and composition), although a negative hypothetic influence of salinity may have occurred. Body composition was comparable when zooplankton was dominated by Pseudodiaptomus hessei and freshwater species, but contents were significantly lower for assemblages dominated by more exclusively marine species (Paracalanus spp., Oithona spp., marine cladocerans, chaetognates, etc.).     

SEASONAL VARIATIONS IN TOTAL NITROGEN,CARBON AND AMINO ACIDS IN MACROCYSTIS INTEGRIFOLIA AND NEREOCYSTIS LUETKEANA (PHAEOPHYTA)1

Seasonal variations in tissue nitrogen, carbon, amino acids and ammonium were determined for the brown algae Macrocystis integrifolia Bory and Nereocystis luetkeana (Mertens) Pastels and Ruprecht, For M. integrifolia, the proportions of tissue nitrogen and carbon in blades, bulbs and stipes were also determined. The composition of the two algae in terms of the above constituents was similar. In addition, ammonium, nitrogen and protein-bound amino acids showed distinct seasonal trends with high values during the winter and low levels during the summer. The range for nitrogen was 0.8–3.0% and for proteins 7.6–11.7% of dry weight. In contrast, carbon content and C/N ratio showed the reverse trend with higher values during the summer and lower values during the winter. The range for carbon was 19–31% of dry weight, and the C/N ratio showed a range of 9–37. The free amino acids did not show any specific seasonably. Tissue nitrogen and carbon showed higher values in the blades than in the bulbs and stipes.     

Elemental composition, total lipid content, and lipid class proportions in zooplankton from the benthic boundary layer of the Beaufort Sea shelf (Canadian Arctic)

Biochemical analyses such as lipid class and elemental composition can inform us about a species’ role in community energetics and nutrient cycling. The accumulation of lipid-rich energy stores affects the elemental composition and stoichiometry of animal tissues, and this relationship is especially relevant to zooplankton at higher latitudes due to increased seasonal lipid storage. However, due to sampling difficulties, the elemental composition and energy storage capabilities of polar, benthic boundary layer zooplankton are poorly known. We determined elemental and lipid class compositions for 26 taxa of benthic boundary layer zooplankton from the Beaufort Sea shelf. Elemental composition as a percentage of dry weight ranged 21–56% for carbon (C), 4–11% for nitrogen (N), and 0.1–1.1% for phosphorus (P) across all taxa. C concentration and C:N were positively correlated with the storage lipids triacylglycerols (TG) and wax esters/steryl esters (WE/SE) and negatively correlated with membrane lipids (phospholipids and sterols). Most taxa had high levels of storage lipids, generally TG. High levels of WE/SE were found in the copepod Calanus hyperboreus (>90% of total lipid) and the chaetognath Eukrohnia hamata (72%). In contrast, the chaetognath Parasagitta elegans had only minor proportions of both TG and WE/SE. The high levels of storage lipids in most taxa indicate that feeding behavior of benthic boundary layer zooplankton on the Beaufort Sea shelf is tightly linked with seasonal pulses of epipelagic production. This is the first report on the biochemical composition of most of the amphipod and mysid taxa presented here.     

Production ecology of phyto- and zooplankton in a eutrophic pond dominated byChaoborus flavicans (Diptera: Chaobolidae)

Primary production of phytoplankton and secondary production of a daphnid and a chaoborid were studied in a small eutrophic pond. The gross primary production of phytoplankton was 290 gC m⁻² per 9 months during April–December. Regression analysis showed that the gross primary production was related to the incident solar radiation and the chlorophylla concentration and not to either total phosphorus or total inorganic nitrogen concentration. The mean chlorophylla concentration (14.2 mg m⁻³), however, was about half the expected value upon phosphorus loading of this pond. The mean zooplankton biomass was 1.60 g dry weight m⁻², of whichDaphnia rosea and cyclopoid copepods amounted to 0.69 g dry weight m⁻² and 0.61 g dry weight m⁻², respectively. The production ofD. rosea was high during May–July and October and the level for the whole 9 months was 22.6 g dry weight m⁻².Chaoborus flavicans produced 10 complete and one incomplete cohorts per year. Two consecutive cohorts overlapped during the growing season. The maximum density, the mean biomass, and the production were 19,100 m⁻², 0.81 g dry weight m⁻², and 11.7 g dry weight m⁻²yr⁻¹, respectively. As no fish was present in this pond, the emerging biomass amounted to 69% of larval production. The production ofC. flavicans larvae was high in comparison with zooplankton production during August–September, when the larvae possibly fed not only on zooplankton but also algae.     

Inverse relationship between carotenoid and lipid formation in Rhodotorula gracilis according to the C/N ratio of the growth medium

Production of carotenoid by Rhodotorula gracilis was highest at 26 mg/g dry weight with a carbon/nitrogen (C/N) ratio in the medium of 10:1. This was 15 times higher than when the C/N ratio was 160:1. With this high C/N ratio, the yeast produced up to 55% lipid compared only 20% lipid with the low C/N ratio. Both carotenoid and lipid production were non-growth associated.     

Seasonal changes in sedimentation of particulate matter and lipid content of zooplankton collected by sediment trap in the Arctic Ocean off Axel Heiberg Island

Summary Sedimentation of particulate matter measured at a depth of 100 m varied from 0.2 to 6.0 mg dry weight m^-2 d^-1 over approximately monthly intervals between September 1986 and June 1987 on the continental shelf of the western Arctic Ocean north of the Canadian Arctic Islands. Detritus deposited during December and January, the period of maximum sedimentation, contained relatively low amounts of organic carbon and nitrogen (4.0% and 0.5% of dry weight, respectively) with a carbon: nitrogen ratio > 7. Maximum rates of organic carbon and nitrogen sedimentation (0.60 and 0.12 mg m^-2 d^-1, respectively) during February were associated with debris enriched with organic matter (organic carbon and nitrogen content of 17.0% and 3.4% of dry weight, C:N=5). Dry weight of macrozooplankton, predominantly Calanus hyperboreus and Metridia longa, separated from preserved trap contents, equalled or exceeded by up to an order-of-magnitude the weight of sedimented debris. Lipid content of CV and adult female stages of C. hyperboreus decreased from 46%–64% of dry weight in September to 20%–30% in January. Females of C. hyperboreus with lower lipid levels (7% of dry weight) between April and June were probably in a post-reproductive condition.     

Responses of dry weight growth under SO2 stress in an SO2-tolerant plant,Polygonum cuspidatum

The effects of exposure to 0.5–0.7 ppm SO₂ for about one month on the dry weight growth and net photosynthesis ofPolygonum cuspidatum were investigate. Furthermore, the carbon and nitrogen concentrations in each plant organ were measured. The results obtained showed no significant decrease in the total dry weight of SO₂-treated plants in comparison with controls. On the other hand, the leaf area (LA) and/or leaf dry weight of SO₂-treated plants were increased, and the root dry weight (RW) was decreased, in comparison with controls. The leaf carbon assimilation rate (CAR) in SO₂-treated plants was slightly decreased in spite of a clear decrease in net photosynthesis, and the value of (SW+RW)/LA (SW stem dry weight) was decreased in comparison with controls, thus minimizing the reduction in CAR. Furthermore, the ratio of total leaf carbon absorption (leaf area x CAR) to total root nitrogen absorption (root dry weight x nitrogen assimilation rate) in SO₂-treated plants was similar to that in controls. From these results, it can be concluded that an increase in leaf area and/or leaf dry weight and a decrease in root dry weight inP. cuspidatum under SO₂ stress may be induced in order to compensate for the decrease in CAR and to maintain the ratio of total leaf carbon absorption to total root nitrogen absorption in the early stage of vegetative growth.     

Zur chemischen Zusammensetzung der CtenophorePleurobrachia pileus in der Kieler Bucht

The chemical composition of the ctenophorePleurobrachia pileus was investigated in March, May and July 1981 in Kiel Bight, western Baltic. The results of all determinations yielded low values compared with other zooplankton groups. Dry weight made up 1.95 to 2.28% wet weight with a minimum occurring in may. Ash-free dry weight amounted to 28–37% of the dry weight but exhibited a maximum in May. Carbon and nitrogen analyses yielded amounts of between 2.6–4.7% of the dry weight and 0.5–1.0% of the dry weight, respectively. Both elements reached lowest levels in May. Proteins reached a minimum in May, too, and values ranged between 2.5 and 5.1% of the dry weight. However, lipids as well as carbohydrates exhibited highest values in May and ranged from 0.8 to 1.6% and 0.8–1.1% of the dry weight, respectively. The C∶N values increased between March and July from 3.7∶1 to 6.7∶1, indicating a decline in protein content. To relate the biochemical compounds to organic matter I used three different approaches: (1) On the basis of ashfree dry weight, carbohydrates remained constant whereas lipids increased from March to July. A minimum of proteins occurred in May. The three compounds made up only 14–22% of ash-free dry weight. (2) Organic matter approximately equals organic carbon content multiplied by 2. Proteins, lipids and carbohydrates summed up reached 61–100% of this reference value and the seasonal course of these compounds changed in a drastic way: proteins decreased, whereas lipids as well as carbohydrates showed a relative maximum in May. (3) Finally, the carbon content of each biochemical compound was calculated in relation to total carbon content measured via C/N analysis. On this basis, 63–105% of total carbon were recovered, and the course of seasonal changes agreed with that of the second approach. A comparison of these three approaches suggests that comparative calculations based on carbon measurements are more valid than those based on ash-free dry weight. The results show that seasonal changes in the amount of organic matter and the biochemical composition occurred. Dry weight was lowest in May, which could be due to the low salinity environment recorded at that time and the corresponding low salt content of the tissue. The observed relative maxima of lipids and carbohydrates in May may be explained by good food conditions since high zooplankton densities are characteristic for this month in Kiel Bight.      

In situ metabolic budget for the calanoid copepod Acartia clausi in a tropical brackish water lagoon (Ebrié Lagoon,Ivory Coast)

Simultaneous measurements of respiration, excretion and production rates were carried out several times over a year period at five representative stations of the Ebrié Lagoon. Assuming a constant assimilation efficiency rate of 69.4%, we derived metabolic budgets for carbon, nitrogen and phosphorus. Daily specific ingestion rates calculated were rather generally high, and ranged between 54 and 159% of body carbon, between 26 and 102% of body nitrogen and between 108 and 307% of body phosphorus. Regional and seasonal variations depended mainly upon variations in trophic conditions. Curvilinear relationships between ingestion production, or net production efficiency K2, and food concentration (as chlorophyll-a + phaeopigments) showed that food could have been a limiting factor. Furthermore, K2 were low when compared with data from the literature (mean of 21% in carbon, 39% in nitrogen and 11% in phosphorus).Complementary laboratory experiments carried out on adults fed with enriched natural particles or algal cultures (Tetraselmis sp. or Dunaliella sp.) showed similar production (egg-production) vs food concentration curvilinear relationships as in the field. However, considerably higher maximal ingestion and production rates were obtained for animals fed algal cultures suggesting that optima for food acquisition and transformation were not reached in field conditions.Consequently, A. clausi, which represents more than 50% of the zooplankton biomass, appears to be rather inefficient in transforming the abundant particulate organic matter produced in the lagoon. This results from its high level of metabolic expenditure through respiration or excretion (about 50% of ingestion in terms of carbon) and from the small size and poor trophic value of food particles (high percentage of detritus).     

Changes in carbon and nitrogen content during decomposition of three macrophytes in freshwater and marine environments

Three species of aquatic plants were analyzed for their ash, organic carbon and nitrogen content both fresh and after decomposition using the mesh bag method Chara contraria A. Br. ex Kütz in a small freshwater pond and Lemna minor L. in a shallow swamp were examined over a 70 day period of in situ decomposition. Fucus vesiculosus L. was examined over a 63 day period of decomposition in a rocky shore and a salt marsh environment.During decomposition Chara showed a decrease in carbon and an increase in nitrogen content while Lemna increased in carbon and decreased in nitrogen, all on an ash-free dry weight basis. Although the C : N ratio of Chara was high initially and that of Lemna relatively low, after decomposition the C : N ratio for the remains of the two plants was nearly the same. Fucus decomposing in the salt marsh showed no significant change in carbon but increased in nitrogen content while that at the rocky shore decreased in carbon and increased in nitrogen content. Much of the loss in total dry weight in the first few hours of submergence could be attributed to solubilization of ash and of some high C : N ratio organic material. Consistent and significant differences in the C : N ratio of decomposing Fucus at the two marine sites may be attributable to the nature of the decomposer organisms that inhabit these environments. The accumulation of a high proportion of autotrophic microbial biomass (such as purple sulfur bacteria) in the structural carbohydrates of the salt marsh Fucus may have caused these differences.This study suggests that initial differences in nutritional value of aquatic macrophytes diminish during decomposition and that the ultimate C : N ratio attained may be more dependent on the nature of the decomposer organisms present than on the nature of the organic material undergoing decomposition.     

苗期玉米叶片碳氮平衡与干旱诱导的叶片衰老之关系

为了探究干旱诱导的碳氮平衡破坏与干旱诱导的叶片衰老之间的关系,该实验以8个在干旱胁迫下叶片衰老进程有明显差异的玉米品种为实验材料,采用PEG模拟干旱处理,通过测定光合速率、叶绿素含量和叶绿素荧光参数等叶片衰老指标以及非结构性碳水化合物(可溶性糖、淀粉)和全氮含量等变化,分析玉米中干旱诱导的叶片衰老与叶片中碳氮平衡(碳氮比)之间的关系。结果显示:(1)干旱胁迫下,8个玉米品种叶片净光合速率受到严重抑制,Fv/Fm大幅下降,叶绿素含量显著降低,说明干旱诱导了玉米叶片的衰老;(2)干旱诱导玉米叶片衰老的同时,8个玉米品种的叶片中可溶性糖含量显著升高,淀粉含量小幅上升,全氮含量大幅降低,碳氮比显著升高,碳氮平衡遭到了破坏;(3)8个玉米品种叶片的叶绿素含量与非结构性碳水化合物含量以及碳氮比呈极显著负相关关系,与全氮含量呈极显著正相关关系。因此,碳氮代谢与干旱诱导的叶片衰老紧密联系,碳氮平衡可能参与了干旱诱导的叶片衰老调控。     

Inter- and intra-annual variability in the phytoplankton community of a high mountain lake: the influence of external (atmospheric) and internal (recycled) sources of phosphorus

1. The inter‐ and intra‐annual changes in the biomass, elemental (carbon (C), nitrogen (N) and phosphorus (P)) and taxonomical composition of the phytoplankton in a high mountain lake in Spain were studied during 3 years with different physical (fluctuating hydrological regime) and chemical conditions. The importance of internal and external sources of P to the phytoplankton was estimated as the amount of P supplied via zooplankton recycling (internal) or through ice‐melting and atmospheric deposition (external). 2. Inter‐annual differences in phytoplankton biomass were associated with temperature and total dissolved phosphorus. In 1995, phytoplankton biomass was positively correlated with total dissolved phosphorus. In contrast, the negative relationship between zooplankton and seston biomass (direct predatory effects) and the positive relationship between zooplankton P excretion and phytoplankton biomass in 1997 (indirect P‐recycling effects), reinforces the primary role of zooplankton in regulating the total biomass of phytoplankton but, at the same time, encouraging its growth via P‐recycling. 3. Year‐to‐year variations in seston C : P and N : P ratios exceeded intra‐annual variations. The C : P and N : P ratios were high in 1995, indicating strong P limitation. In contrast, in 1996 and 1997, these ratios were low during ice‐out (C : P < 100 and N : P < 10) and increased markedly as the season progressed. Atmospheric P load to the lake was responsible for the decline in C : P and N : P ratios. 4. Intra‐annual variations in zooplankton stoichiometry were more pronounced than the overall differences between 1995 and 1996. Thus, the zooplankton N : P ratio ranged from 6.9 to 40.1 (mean 21.4) in 1995, and from 10.4 to 42.2 (mean 24.9) in 1996. The zooplankton N : P ratio tended to be low after ice‐out, when the zooplankton community was dominated by copepod nauplii, and high towards mid‐ and late‐season, when these were replaced by copepodites and adults. 5. In 1995, the minimum demands for P of phytoplankton were satisfied by ice‐melting, atmospheric loading and zooplankton recycling over 100%. In order of importance, atmospheric inputs (> 1000%), zooplankton recycling (9–542%), and ice‐melting processes (0.37–5.16%) satisfied the minimum demand for P of phytoplankton during 1996 and 1997. Although the effect of external forces was rather sporadic and unpredictable in comparison with biologically driven recycle processes, both may affect phytoplankton structure and elemental composition. 6. We identified three conceptual models representing the seasonal phosphorus flux among the major compartments of the pelagic zone. While ice‐melting processes dominated the nutrient flow at the thaw, biologically driven processes such as zooplankton recycling became relevant as the season and zooplankton ontogeny progressed. The stochastic nature of P inputs associated with atmospheric events can promote rapid transitional changes between a community limited by internal recycling and one regulated by external load. 7. The elemental composition of the zooplankton explains changes in phytoplankton taxonomic and elemental composition. The elemental negative balance (seston N : P < zooplankton N : P, low N : P recycled) during the thaw, would promote a community dominated by species with a high demand for P (Cryptophyceae). The shift to an elemental positive balance (seston N : P > zooplankton N : P, high N : P recycled) in mid‐season would skew the N : P ratio of the recycled nutrients, favouring dominance by chrysophytes. The return to negative balance, as a consequence of the ontogenetic increase in zooplankton N : P ratio and the external P inputs towards the end of the ice‐free season, could alleviate the limitation of P and account for the appearance of other phytoplankton classes (Chlorophyceae or Dinophyceae).     

再生水补水河道芦苇碳氮化学计量特征及其对环境的响应

在再生水补水河道内,芦苇（Phragmites australis）受高氮再生水的长期影响,具有独特的碳（C）、氮（N）化学计量特征。为查明芦苇C、N化学计量特征及其对高氮环境的响应,在芦苇生长季节（5、7、9月份）,分析了再生水补水的潮白河顺义段内河水、土壤及芦苇各器官（根、茎和叶）中C、N含量及碳氮比（C/N）。结果表明：河水中C、N含量和C/N比分别在22.20-37.25 mg/L、2.24-11.20 mg/L和3.33-9.92之间。土壤中C、N含量和C/N比的范围为5.69-35.17、0.28-2.63、8.77-25.39。在整个生长季节的所有采样点内,芦苇根、茎和叶中C含量的平均值分别为（170.84±63.56）、（369.02±39.12）、（431.80±96.70） mg/g;N含量的平均值分别为（8.20±3.96）、（14.11±6.22）和（30.73±8.66） mg/g;C/N比的平均值分别为23.89±12.84、32.65±18.48、15.21±5.60。方差分析表明,芦苇各器官中C、N计量特征具有显著的季节性差异（P<0.05）,这主要与芦苇在生长过程中的生理作用有关。环境中C、N计量特征具有显著的空间差异（P<0.05）,受环境变量的影响,芦苇叶中N含量和C/N比从上游到下游显著降低（P<0.05）。逐步回归分析的结果显示,土壤和河水中的C、N含量能够解释芦苇叶中71.0%的变量（P<0.05）;土壤中C、N含量和河水中N含量能够解释芦苇叶C/N比82.6%的变量（P<0.05）。相关分析指出,河水中N含量与土壤中N含量显著正相关（P<0.05）,说明土壤受到高氮再生水的影响而具有较强的供N能力。高氮环境下,芦苇叶中N含量较高;相较于芦苇茎和叶,根中C含量较小。研究证明在再生水补水河道中,芦苇对环境中的N有良好的吸收能力,其C、N计量特征对高氮环境表现出明显的响应。     

Changes of Photosynthetic Characteristics in Relation to Leaf Senescence in Two Maize Hybrids with Different Senescent Appearance

A field experiment was conducted to investigate the changes in chlorophyll (Chl) and nitrogen (N) contents, ribulose-1,5-bisphosphate carboxylase/oxygenase (RuBPCO) and phosphoenolpyruvate carboxylase (PEPC) contents and PEPC activity, and the photon-saturated net photosynthetic rate (P _Nsat), and their relationships with leaf senescence in two maize hybrids with different senescent appearance. One stay-green (cv. P3845) and one earlier senescent (cv. Hokkou 55) hybrid were used in this study, and we found that Chl and N contents and the P _Nsat in individual leaves of P3845 were greater than those in corresponding leaves of Hokkou 55 at the successive growth stages. In addition, larger contents of RuBPCO and PEPC, and a greater activity of PEPC were observed in P3845. Due to the lower rates of decrease of Chl, RuBPCO, and PEPC amounts per unit of N, and the lower net C translocation rate per unit of N in the stay-green hybrid, leaf senescence was delayed in comparison to the earlier senescent hybrid.     

Copepods distribution in relation to a Cape Ghir upwelling filament (Moroccan Atlantic coast)

The study of the Cape Ghir upwelling filament (31°N) focalizes to describe the dispersive mechanism, caused by the upwelling. The zooplankton was sampled during five oceanographic cruises conducted between 2008 and 2009. Surface temperature and chlorophyll “a” were also measured along with sampling. The distribution of environmental parameters accused extensions that show the path of the filament. Copepods constitute the largest fraction of zooplankton community and represented by 86 species, majorly dominated by Acartia clausi and Oncaea venusta. A number of species of deep or cold waters have been recorded in the area corresponding to a net resurgence of cold water. The analysis of the copepods distribution allowed to view the path of the filament at different times of the year. The distribution of the species A. clausi, neritic specie was observed in the open ocean, shows a result of this dynamic.     

Dry weight and chemical composition (CHN) in relation to population density of cultivatedTisbe holothuriae (Copepoda,Harpacticoida)

The harpacticoid copepodTisbe holothuriae was cultivated at different densities in a running-water system. Dry weight and chemical composition (CHN) of both females and egg-sacs have been determined. Dry weight decreased significantly with increasing density from 3,48 to 1.94μg in egg-sacs, and from 10.80 to 6.58μg in females. Increasing density in both egg-sacs and females results in decrease of carbon, nitrogen and hydrogen contents, expressed as a percentage of dry weight of egg-sacs and females, respectively. Carbon decreases from 52.56 to 50.57% (egg-sacs) and 45.80 to 39.95% (⧫), nitrogen from 12.63 to 11.94% and 10.72 to 9.73% and hydrogen from 9.08 to 7.78% and 7.47 to 6.17%. The dry weight and elemental compositions of the egg-sacs varied in accordance with that of the females, however, a higher percentage of elemental content was observed in egg-sacs. The energy equivalents were calculated from the carbon content. This indicates that more energy was transferred from the maternal body into egg-sacs. The ratio of carbon to nitrogen did not show any marked variations; no clear relation appeared between C:N and density, indicating a relatively constant chemical composition in both females and egg-sacs.     

Pelagic organic matter in the Adriatic Sea in relation to winter hydrographic conditions

The spatial distribution of chlorophyll a (Chla), paniculateorganic carbon (POC) and nitrogen (PON), net zoopiankton ash-freedry weight (AFDW), dry weight (DW) and carbon and nitrogen content,in parallel with primary production, was studied during a jointYugoslav cruise in January 1980. The results were interpretedin relation to hydrographic properties, with special emphasison the relationship between pelagic parameters. Spatial distributionof POC, PON and net zoopiankton AFDW and C and N contents showedsimilarities over the major part of the Adriatic, while Chlaand POC showed dissimilarities since higher Chla values wererestricted to the northwestern part of the Adriatic, separatedfrom the rest of the Adriatic by a pronounced thermal frontextending south of the Istrian peninsula. High POC was foundin the centre of the south Adriatic gyre and in the Jabuka Pit,the latter filled with cold water originating from the arealocated south of the thermal front. The areas of high POC werecharacterized by a higher POC recycling time than in other Adriaticregions. High Chla, POC, PON and net zooplankton AFDW and Cand N contents in parallel with increased primary productionwere found in the southwestern part of the Adriatic off Puglia(Italy) affected by a continuous terrigenous supply of nutrients.The observed spatial distribution pattern of pelagic organicmatter suggests that this distribution is mostly influencedby hydrographic conditions and that the assumption of permanentproductivity zones in the Adriatic is not applicable to thewinter situation.     

马尾松林两种林下植被土壤碳氮特征及其与凋落物质量的关系

以飞播马尾松林为研究对象,通过典型样地调查和样品测定,采用配对样本t检验和冗余分析（RDA）方法分析芒萁类和禾草类两种林下植被类型土壤碳、氮特征及其与凋落物质量之间的关系。结果表明：（1）土壤有机碳、微生物量碳、可溶性有机碳、全氮、速效氮、微生物量氮和可溶性有机氮含量在0-10、10-20 cm土层均表现为禾草类显著高于芒萁类（P < 0.05）,而在20-40、40-80 cm土层两种植被类型碳氮指标的大小未表现出相同的变化规律,且差异不显著（P > 0.05）。（2）两种植被类型凋落物半分解和未分解层的C含量及C/N值均表现为芒萁类显著高于禾草类（P < 0.05）,而N含量则表现为禾草类显著高于芒萁类（P < 0.05）;同一植被类型的未分解层C含量及C/N值均显著大于半分解层,N含量则半分解层显著大于未分解层（P < 0.05）。（3）0-10 cm土层两种类型凋落物C/N值和C含量均与土壤碳氮各指标呈显著负相关（P < 0.05）,N含量与土壤碳氮各指标的相关性不显著（P > 0.05）;10-20 cm土层,芒萁类的半分解层C/N值与土壤碳氮各指标存在显著相关性（P < 0.05）,禾草类的凋落物C含量与土壤碳氮各指标也存在显著相关性（P < 0.01）。林下植被凋落物C/N值越小,其分解速率越快,有利于土壤养分的积累,禾草类凋落物C/N值低于芒萁类是导致其土壤碳氮指标高于芒萁类的重要原因。     

Biomass and elemental composition (C.H.N.) of the rotifer Brachionus plicatilis cultured as larval food

Changes in dry weight, carbon, nitrogen, hydrogen and ash content of the rotifer Brachionus plicatilis were investigated during population growth in culture. Also caloric equivalent was estimated from carbon content. Body dry weight and weight of C, N, and H increased with increasing the egg/female ratio of the population, while ash content remained constant. As percentage of dry weight, C content increased with fecundity, H and N remained constant and ash content decreased. The caloric equivalent ranged from 1278 µcal to 4406 µcal for rotifers from 314 µg to 846 µg of dry weight.