Effects of current velocity on development and survival of lingcod,Ophiodon elongatus,embryos

Synopsis The influence of current velocity on the survival and development of lingcod embryos was investigated in the field and laboratory. Examination of egg masses at five lingcod spawning sites indicated that embryo mortalities were high (up to 95%) at low-current sites because of inadequate ventilation and resulting hypoxia. Development of embryos near the center of poorly ventilated egg masses was retarded relative to development of embryos near the periphery. Hatching of embryos from poorly ventilated eggs was protracted; embryos from the interior of egg masses hatched later and were significantly smaller than embryos from eggs near the periphery. Oxygen levels measured in egg masses at low-current velocity sites during tidal flow average 16% air saturation, corresponding to a Median Tolerance Limit (LT₅₀) of about 73 h. Oxygen levels measured in egg masses at high-current velocity sites during slack water average 69% air saturation, a level that did not adversely affect the embryos. Current velocities of 10–15 cm s^–1 were needed to maintain interstitial oxygen levels in egg masses near that of the ambient water. Water movement may be an important stimulus for spawning site selection by lingcod. In areas where tidal currents were weak, spawn deposition occurred in shallow water where waves and vertical tide motion created water movement. In areas where tidal currents were strong, spawns were consistently deposited in deeper water.     

Seasonal cycle of nitrogen and phytoplankton biomass in a well-mixed coastal system (Eastern English Channel)

The hydrological structure of the French coastal part of the eastern English Channel is strongly linked with tidal regimes and riverine input. Two distinct water masses are separated by a frontal area and drift along the coast in SW–NE direction. These two water masses are well-mixed during the entire year. We studied the seasonal dynamic of nitrogenous nutrients, chlorophyll a and organic particulate carbon and nitrogen at two stations, characteristic of these water masses, during the year 1994. Results show (i) a winter stock of nitrate and ammonium, (ii) a pre-bloom period corresponding to the use of ammonium, (iii) a high bloom period of short duration using nitrate, (iv) a post-bloom period with little phytoplanktonic activity probably limited by nutrients other than nitrogen and (v) an autumnal period of reconstitution of stock. The essential difference between the two stations is the importance of winter stock of nutrients and of bloom chlorophyll a concentration, with the coastal station richer than the offshore one. An assumption about the nitrogen available for new production in this area gives a value of 57% of the winter stock of inorganic nitrogen.     

Diel changes in the specific growth rate and mean cell volume of natural bacterial communities in two different water masses in the Irish sea

Diel changes in the specific growth rates of natural bacterial communities as a whole and of different groups within the communities were followed over 2 days during July 1982, in stratified waters in the vicinity of a shallow sea tidal mixing front in the Irish Sea. Waters well above (4 m) and below (60 m) the thermocline were enclosed in dialysis bags and incubated in situ. The results show that there were periods of altered growth rates of the whole bacterial community and synchronous cell division of morphological groups. An increase in mean cell volume within both 4 and 60 m communities preceded an increase in specific growth rates, with a resultant decrease in the mean cell volume. Above the thermocline the whole bacterial community, as well as the rod and coccoid forms, doubled in number once a day. The doubling time of the whole bacterial community at 60 m was 2 days and slower than that at 4 m. This was due to a slower doubling time (3 days) for the coccoid forms. Rod forms at the two depths had a similar doubling time (1 day). The time of day when maximum division rate occurred was also different in the two water masses. At 4 m more coccoid forms divided during the night, whereas at 60 m more divided during the day. Conversely, at 4 m more rod forms divided during the day, whereas at 60 m more divided at night.These data indicate that the bacterial community and members of the community may be adapted to exploit the diurnal rhythms of dissolved organic carbon (DOC) release by other organisms and that portions of the bacterial community may therefore be more active at certain times of the day. The diurnal growth of the bacterial community may thus vary between different water masses and largely reflects the differences in the chemical and biological characteristics of the two water masses investigated.     

Water-mass influences on summer Antarctic phytoplankton biomass and community structure

The association between the variability of phytoplankton biomass and community structure and the distribution of water masses around the Antarctic Peninsula were examined during austral summer 1993. Phytoplankton biomass showed high variability, and was dominated by an autotrophic flagellate (Cryptomonas sp.) that represented, on average, 91% of total phytoplankton biomass. The lowest phytoplankton biomasses were associated with the strongly mixed, saline, cold waters characteristic of the Weddell Sea water mass, and with the waters influenced by ice melt from the Bellingshausen Sea. The highest biomasses were found in the confluence of these water masses, where a front develops. Community composition also differed among water masses, with eukariotic picoplankton and diatoms having their highest relative contribution to community biomass in stations with Bellingshausen Sea and Weddell Sea water masses, whereas the abundance of Cryptomonas sp. was highest at the confluence of these waters. These results indicate that mesoscale processes, that determine water mass distribution, are of paramount importance in controlling the time and space variability of Antarctic phytoplankton.     

The estuarine character of the Gulf of Nicoya,an embayment on the Pacific coast of Central America

Hydrography and exchange processes in a tropical estuary, the Gulf of Nicoya, Costa Rica, are described from data collected in 1979 and 1980. The measurements and analyses were made in both the dry season and wet season and include temperature, salinity, and density at twenty locations in the gulf and currents (over a semi-diurnal tidal cycle) at five locations. These new results enlarge on the early study by Peterson (1958). Circulation in the lower gulf shows a marked east-west asymmetry due to the predominant runoff along its eastern shore from Rio Barranca and Tarcoles. The freshened surface water from the upper gulf combines with the runoff from these rivers and flows southward along the eastern side of the lower gulf. This flow is compensated by a northward flow of more saline water on the western side at all depths and on the eastern side along the bottom. The boundary between the southward and northward surface flow is marked by a strong salinity front in the rainy season. There is a rapid increase in tidal energy density toward the shoaling northern reaches of the lower gulf, between San Lucas Island and Puntarenas Peninsula. Enhanced mixing must accompany this increase, and direct measurements in the constriction between San Lucas and Puntaneras show that tidal mixing is dominant in transporting salt into the upper gulf against the freshwater runoff.     

Time scales of circulation and mixing processes of San Francisco Bay waters

Conceptual models for tidal period and low-frequency variations in sea level, currents, and mixing processes in the northern and southern reaches of San Francisco Bay describe the contrasting characteristics and dissimilar processes and rates in these embayments: The northern reach is a partially mixed estuary whereas the southern reach (South Bay) is a tidally oscillating lagoon with density-driven exchanges with the northern reach.The mixed semidiurnal tides are mixtures of progressive and standing waves. The relatively simple oscillations in South Bay are nearly standing waves, with energy propagating down the channels and dispersing into the broad shoal areas. The tides of the northern reach have the general properties of a progressive wave but are altered at the constriction of the embayments and gradually change in an upstream direction to a mixture of progressive and standing waves. The spring and neap variations of the tides are pronounced and cause fortnightly varying tidal currents that affect mixing and salinity stratification in the water column.Wind stress on the water surface, freshwater inflow, and tidal currents interacting with the complex bay configuration are the major local forcing mechanisms creating low-frequency variations in sea level and currents. These local forcing mechanisms drive the residual flows which, with tidal diffusion, control the water-replacement rates in the estuary. In the northern reach, the longitudinal density gradient drives an estuarine circulation in the channels, and the spatial variation in tidal amplitude creates a tidally-driven residual circulation. In contrast, South Bay exhibits a balance between wind-driven circulation and tidally-driven residual circulation for most of the year. During winter, however, there can be sufficient density variations to drive multilayer (2 to 3) flows in the channel of South Bay.Mixing models (that include both diffusive and dispersive processes) are based on time scales associated with salt variations at the boundaries and those associated with the local forcing mechanisms, while the spatial scales of variations are dependent upon the configuration of the embayments. In the northern reach, where the estuarine circulation is strong, the salt flux is carried by the mean advection of the mean salt field. Where large salinity gradients are present, the tidal correlation part of the salt flux is of the same order as the advective part. Our knowledge of mixing and exchange rates in South Bay is poor. As this embayment is nearly isohaline, the salt flux is dominated entirely by the mean advection of the mean salt field. During and after peaks in river discharge, water mixing becomes more dynamic, with a strong density-driven current creating a net exchange of both water mass and salt. These exchanges are stronger during neap tides.Residence times of the water masses vary seasonally and differ between reaches. In the northern reach, residence times are on the order of days for high winter river discharge and of months for summer periods. The residence times for South Bay are fairly long (on the order of several months) during summer, and typically shorter (less than a month) during winter when density-driven exchanges occur.     

Formation and retention mechanisms of phytoplankton peak abundance in the Kuroshio front

Observations on phytoplankton and environmental factors weremade across the Kuroshio front. Phytoplankton standing stockwas high just north of the temperature front, and the widthof the peak abundance was <10 km. By analyses of speciescomposition and water masses, the entrainment of coastal waterand/or the Oyashio water was considered to be an important factorfor the formation of the phytoplankton peak abundance. The comparativelyhigh contribution of the microplankton fraction >10 µmin the peak abundance also supported the importance of entrainmentprocess. The incubation experiments of natural phytoplanktonassemblages with nutrient addition showed that the microplanktonfraction has higher growth potential at the front than in theneighboring waters. Dome-like risings of isopleths of temperatureand nutrients were demonstrated in the cross sectional observationof the front Possible upwelling accompanied with nutrient supplyseemed to contribute to the retention of the phvtoptankton peakabundance at the front.     

南黄海潮汐锋对浮游细菌生物量分布的影响

2 0 0 1年 5月 16～ 2 3日、6月 10～ 2 4日和 2 0 0 2年 6月 5～ 12日 ,利用“北斗号”船只对南黄海鱼产卵场进行了 3次专项调查。研究了潮汐锋断面叶绿素 a浓度、浮游细菌生物量的分布 ,目的是阐明潮汐锋的存在对浮游细菌生物量分布的影响。3个航次中的叶绿素 a浓度变化范围分别是 0 .0 6～ 2 .34mg/ m3(2 0 0 1- 0 5 )、0 .0 8～ 0 .9mg/ m3(2 0 0 1- 0 6 )、0 .14～ 3.0 4 mg/ m3(2 0 0 2 - 0 6 )。 3航次的聚球藻 (Synechococcus spp.)蓝细菌生物量变化范围分别为 7.6 2～ 2 2 .0 6 mg C/ m3(2 0 0 1- 0 5 )、8.5 3～2 7.5 2 mg C/ m3(2 0 0 1- 0 6 )、0 .6 9～ 5 5 .90 m g C/ m3(2 0 0 1- 0 6 )。异养细菌生物量变化范围分别为 7.5 6～ 5 1.82 mg C/ m3(2 0 0 1-0 5 )、8.5 4～ 2 4 .77mg C/ m3(2 0 0 1- 0 6 )、3.12～ 10 .0 5 mg C/ m3(2 0 0 2 - 0 6 )。而聚球藻蓝细菌对浮游植物总生物量的贡献 (CB:PB)平均值分别为 :5 8% (2 0 0 1- 0 5 )、77% (2 0 0 1- 0 6 )、31% (2 0 0 2 - 0 6 )。结果表明 :南黄海鱼产卵场在春末夏初 (5～ 6月份 ) ,叶绿素 a浓度最大值及次大值主要分布在锋区及其邻近的层化区2 0 m以浅位置 ;聚球藻蓝细菌生物量最大值主要分布于锋区及层化区表层和水体中层 ;异养     

CIRCULATION IN HIGHLY STRATIFIED SOUTHERN AFRICAN ESTUARIES

Summary

The nature of estuarine circulation under highly stratified conditions is reviewed in the context of southern African estuaries that are small and have a constricted connection to the ocean. While the focus is on the generic hydrodynamic processes and features, attention is given to field observations from a particular estuary as a way of illustrating these processes and features. Notable features are the tidal intrusion front, the bottom density current and the long-residence deep water in the upper estuary. The important hydrodynamic processes, which account for these features, are internal hydraulic control of exchange through the mouth, buoyancy-driven landward intrusion of sea water, upward shear-driven entrainment and ebb tidal outflow.

The context in which these processes and features are expected to occur is addressed through a discussion of seasonal variations in the prototype and through a discussion of these features observed in other southern African estuaries. A distinction is made between those systems that are permanently highly stratified and those that display highly stratified phases. The ecological and management implications of strong stratification in an estuary are discussed briefly.     

Ecological engineering analysis and eco-hydrodynamic simulation of tidal rivers in Shenzhen City of China

A comprehensive approach using ecological engineering analysis and eco-hydrodynamic simulation was conducted on the tidal rivers in Shenzhen City of China in this study. A tidal river along a near-shore city should be evaluated and regulated from a multidisciplinary point of view, focused especially on ecology, in order to maintain and enhance the ecological structure and function of the river. Firstly, eco-hydrodynamic control can be used, based on simulated modeling of tidal water circulation, to trace the distribution of pollutants and to predict circulation of tidal water. Using findings from this modeling effort, some water control facilities, such as additional channel connection and water gates, can be established. Appropriate operation strategy is to use tidal energy to promote effective water exchange in the water bodies and thereby improve water quality in the tidal river. Secondly, ecological engineering methods should be integrated with hydraulic measures to further improve the environment. Appropriate plant communities for this ecological engineering can be selected. Based on the simulated results of eco-hydrodynamic model, the optimum locations for adding reclaimed land can be determined. These ecological engineering methods are as follows: (1) it is necessary to calculate the ecological water requirements for the tidal river. The water effluent from the sewage treatment plant can be considered as reclaimed water and pumped to upstream of the tidal reach for reuse; (2) well planned aquatic plant systems composed of emergent, floating, and submergent plants can be used to promote water treatment; (3) the configuration of the engineered landscape should give preference to indigenous plants and appropriate non-indigenous plant species; (4) constructed wetlands, especially mangroves at coastal city sites, can also improve the tidal river aquatic environment.     

Spatio-temporal structure of tidally mixed coastal waters: variability and heterogeneity

In the tidally mixed coastal waters of the eastern English Channel,the vertical properties of temperature, salinity, in vivo fluorescence,turbidity and light were investigated along an inshore-offshoretransect, sampled in different tidal conditions. The verticaldistribution of these parameters was then characterized in termsof mean value, variability (i.e. standard deviation) and heterogeneity(i.e. fractal dimension), regarded as a quantitative characterizationof the structure of the vertical variability of both physicaland biological parameters. These different estimates were thensubjected to multivariate spatio-temporal analysis and showeda very specific spatio-temporal structure suggesting a differentialcontrol of the vertical properties of water masses associatedwith both inshore-offshore gradient and tidal advection. Inparticular, the fractal dimension (i.e. heterogeneity) of invivo fluorescence is higher during ebb for offshore waters,suggesting a density dependence of the phytoplankton biomassstructure. In contrast, the vertical variability of fluorescenceis higher during flood for inshore waters, leading to an inverserelationship between variability and heterogeneity of the verticaldistribution of phytoplankton biomass.     

Seabirds as monitors of upper-ocean thermal structure. King penguins at the Antarctic polar front, east of Kerguelen sector

The main objective of this work was to assess the potential of diving birds to monitor the hydrographic features near the Antarctic polar front. We compared the temperature/depth profiles recorded by instrumented King penguins Aptenodytes patagonicus at Kerguelen Islands (South Indian Ocean) with the oceanographic and remote sensing (satellite) data available for the same area during the same season. The birds were equipped with time/depth/temperature recorders or Argos transmitters. In addition, two birds were instrumented (of which one successfully) both with a time/depth/temperature recorder and an Argos transmitter. King penguins foraged as far as 400 km from the coast, in water masses with a vertical temperature structure characteristic of the region just south of the polar front. The temperature/depth profiles recorded throughout the dives (up to 270 m) revealed a pronounced thermocline. A three-dimensional distribution of water temperature was reconstructed. Comparison with previous hydrographic data shows a high correlation. Instrumented predators may therefore usefully and cheaply complement the database provided by conventional hydrographic surveys and remote sensing, especially in distant and rough areas such as the Southern Ocean.     

Orientation and navigation in coastal and estuarine zooplankton

The axiom that zooplankton species exhibit upwards migration behaviour at night is challenged by recent findings. Such behaviour is not universal, may vary during ontogeny, and is occasionally reversed. Moreover, in some estuarine and coastal zooplankton species vertical migration rhythms are of tidal, not diel, periodicity. There is evidence for several species that vertical migrations are endogenously controlled, occurring in constant conditions in the laboratory, suggesting that they have arisen under considerable selection pressure. They appear to play a significant role in orientation and navigation of coastal and estuarine zooplankton, predicated on the selective advantage of closure of life cycles. Vertical migrations between water masses moving in different directions at tidal, diel or longer timescales permit dispersal and recruitment, or retention, of planktonic larvae and adults in favourable ecological locations. Exogenous factors serving as cues for, or directly controlling, vertical migration rhythms include light, hydrostatic pressure, salinity, temperature, water movements and gravity responses, besides biological factors such as the timing of larval release, duration of larval life and predator/prey interactions. Behavioural characteristics should be quantified and factored into dispersal models which assume that zooplankton adults and larvae are advected as passive particles.     

红树林生长带与潮汐水位关系的研究

根据海南东寨港林市村,廉江车扳镇那肋村,深圳锦锈中华等３个实验点１０条横断面红树林潮滩高程水准测量,林市村潮汐水位观测,潮汐特征水位及浸淹频率分布计算,参照有关港点潮汐实测或预测报资料,确定红树林外边界为平均海面或稍上,内边界（或林内最大高程）为回归潮平均高高潮位（或大潮平均高潮位）对国内外有关报道进行了评述,指出国内许多红树林文献中使用的“高潮位”,“中潮位”“低潮位”用潮汐学术语表述应为“回归     

Propagation of planktonic copepods: production and mortality of eggs

Data on fecundity and egg mortality of neritic copepods were collected in various seasons, areas and under various hydrographical conditions. On a seasonal basis variations in fecundity (F) were related to temperature rather than to the abundance of phytoplankton (P). However, a strong correlation between F and P was evident when water column stability varied horisontally or temporally (i.e. at a tidal front or subsequent to a storm). Estimated specific egg-mortalities were variable and occasionally very severe, up to 9.1 d^–1, implying that down to 10^–4% of the eggs survive to hatching. The implications for phenology and distribution of copepods are discussed.     

Thermal history of reef-associated environments during a record cold-air outbreak event

Summary Several polar continental air masses intruding into the south Florida/northern Bahama Bank region during January 1981 caused record low air temperatures and rapid chilling of extensive shallow-water carbonate systems. Numerous coral kills along the Florida reef tract and massive fish mortalities in Florida Bay were attributable to unusually cold waters generated at this time. Thermal evolution of Florida Bay/Florida reef tract and northern Bahama Bank waters from 8 to 21 January was assessed from thermal infrared data acquired by the NOAA-6 environmental satellite, in situ water temperatures, local meteorological data, and a computerized heat flux model. Field observations and laboratory experiments identify 16°C as a thermal stress threshold for most reef corals (Mayor 1915; Davis 1981). Temperaturecorrected digital satellite data indicated that water temperatures below 16°C were generated in Florida Bay and on Little and Great Bahama Banks during a 10-day period in January. Lowest temperatures on the Florida reef tract resulted from offshelf transport of Florida Bay water through major tidal channels. Offshelf movement of bay water is driven primarily by strong northerly winds, density gradients, and tidal pumping. Absence of reef development opposite major tidal passes along the Florida reef tract (Ginsburg and Shinn 1964) and aperiodic coral kills along bank margins can be attributed to this process, which has probably had a limiting influence on Holocene reef development in these areas.     

Predominant growth of Alcanivorax strains in oil-contaminated and nutrient-supplemented sea water

We found that bacteria closely related to Alcanivorax became a dominant bacterial population in petroleum-contaminated sea water when nitrogen and phosphorus nutrients were supplied in adequate quantity. The predominance of Alcanivorax bacteria was demonstrated under three experimental conditions: (i) in batch cultures of sea water containing heavy oil; (ii) in columns packed with oil-coated gravel undergoing a continuous sea water flow; and (iii) in a large-scale tidal flux reactor that mimics a beach undergoing tidal cycles with fresh sea water. These results suggest that bacteria related to Alcanivorax are major players in the bioremediation of oil-contaminated marine environments.     

Breeding waterbird wetland habitat availability and response to water-level management in Saint John River floodplain wetlands, New Brunswick

Vegetated areas of rivers and estuaries are capable of affecting the concentration of dissolved and particulate matter in water masses traversing those plant beds. We examined whether different sizes of water chestnut (Trapa natans) beds in the Hudson River, USA, alter dissolved oxygen, nutrients and turbidity of water masses. Ebb–tide water was sampled from four water chestnut beds in the tidal freshwater portion of the Hudson River estuary and each site was sampled multiple times during the growing season and once following plant senescence. Water quality variables included dissolved oxygen, turbidity, dissolved organic carbon, and inorganic nutrients. Samples from the small beds (575 m² and 624 m²) were compared with large beds (16 600 m² and 24 820 m²). Dissolved oxygen of water flooding vegetated beds in the hour before high tide was 7.18±1.03 mg/l (mean±standard deviation) with a range of 5.5–9.8 mg/l throughout the growing season. Water samples collected as water ebbed from the plant beds showed that only the large beds had an effect on dissolved oxygen with the largest declines in oxygen exhibited by the largest bed. Decline of dissolved oxygen in the water ebbing from the largest bed averaged 1.5±0.4 mg/l/h with a minimum of 4.5 mg/l, equivalent to 54% of saturation, a level at which sensitive fauna are negatively affected. There were no significant relationships between bed size or plant presence and inorganic nutrients, turbidity or DOC. Ebb–tide nitrate was never lower than 87% of flood tide means. Effective management of invasive plants must consider both the variability in effects among plant beds and the areal coverage of plant bed sizes.     

Environmental setting of San Francisco Bay

San Francisco Bay, the largest bay on the California coast, is a broad, shallow, turbid estuary comprising two geographically and hydrologically distinct subestuaries: the northern reach lying between the connection to the Pacific Ocean at the Golden Gate and the confluence of the Sacramento-San Joaquin River system, and the southern reach (herein called South Bay) between the Golden Gate and the southern terminus of the bay. The northern reach is a partially mixed estuary dominated by seasonally varying river inflow, and the South Bay is a tidally oscillating lagoon-type estuary. Freshwater inflows, highest during winter, generate strong estuarine circulation and largely determine water residence times. They also bring large volumes of dissolved and particulate materials to the estuary. Tidal currents, generated by mixed semidiurnal and diurnal tides, mix the water column and, together with river inflow and basin geometry, determine circulation patterns. Winds, which are strongest during summer and during winter storms, exert stress on the bay's water surface, thereby creating large waves that resuspend sediment from the shallow bay bottom and, together with the tidal currents, contribute markedly to the transport of water masses throughout the shallow estuary.     

The tidal freshwater reach of the Weser estuary: Riverine or estuarine?

The tidal freshwater reaches of estuaries have received little attention in ecological research although they are often heavily stressed by environmental impacts. We have thus compiled published and previously unpublished data from the Weser Estuary, Germany. Physical, chemical and biological properties are described within the tidal freshwater reach and compared with the upstream (riverine) and downstream (mixohaline) habitats. The tidal freshwater region is different from riverine sites, mainly due to tidally induced physical processes such as prolonged residence time of the water, oscillating water levels and changing current velocities and directions. Distinctions from the mixohaline situation are mainly due to differences in salinity and particulate suspended matter concentration. It is thus possible to define the tidal freshwater reach of the Weser Estuary as a separate biotope with a specific community structure. The phyto- and zooplankton is a mixture of riverine and autochthonous species whereas marine species are almost completely lacking. In the macroinvertebrate component, as well as in the fish community, marine and riverine species are combined with autochthonous species. This is probably typical for the tidal freshwater reaches of many river dominated coastal plain estuaries. We conclude that the tidal freshwater reaches are an important site of physical, chemical and biological processes which may alter riverine input considerably before it reaches the freshwater-seawater interface. For a better understanding of the ecological functioning of estuaries, it is essential to include these areas within estuarine research programmes.