Insights gained from a web-based atlas of halocyprid ostracods of the Southern Ocean

Planktonic ostracods are an important, but poorly studied component of open ocean plankton communities, which inhabit all depths and play a significant role in detrital cycles. A web-based atlas (http://ocean.iopan.gda.pl/ostracoda) of the distribution of Southern Ocean planktonic ostracods has been developed compiling all extractable published data together with a considerable amount of unpublished data from samples collected during Discovery investigations (1929–1952). The northern boundary of the Southern Ocean was taken pragmatically as 52°S. The website includes information that includes distributional maps, taxonomic drawings (mostly original), size data and systematic notes on 47 species. All the data are freely downloadable as PDF files and are thus available to anyone, anywhere, with access to the web.Published data are subject to a number of errors generated by faulty identifications and changes in the taxonomy. Most, but not all, published data could be included in drawing up the maps. Not all publications have included detailed positional data and from those that included distributional maps, it was not always possible to relate the plotted distributions to the published station listings. A lack of archived data and specimens for some of the records meant dubious records could not be validated. Data are now generally archived by national oceanographic data centres, but unless supported by voucher specimens further confusion may arise for those current species which are found to include cryptic species after classical morphological studies or molecular studies.One species (Boroecia antipoda) had an apparently anomalous distribution; specimens archived in the Copenhagen Museum were reexamined and the anomalies were shown to result from the fact that some of the specimens belong to a novel species. Generally, the limits to the distributional ranges of the species showed little coherence with major oceanographic features, such as the Antarctic convergence and hence, biogeographical provinces; possible reasons are discussed. Despite these possible inherent errors, the website not only provides a resource for species identification, but is also proving to be a powerful tool for generation of hypotheses and highlighting taxonomic problems.     

On the preservation of carapaces of some limnic ostracods: An exercise in actuopalaeontology

The way in which the ostracod carapace decomposes through biological and physico-chemical processes is illustrated with Recent and Neogene non-marine ostracods (candonines, herpetocyprines and cytherids) from lacustrine and groundwater habitats. The degree of carapace preservation for Recent Candoninae, in the Mondsee (Austria) is shown to be dependent on the sedimentary microenvironment. The carapaces of herpetocyprines, because of their special morphological structure, decay very easily. This could explain the rare occurrrence of this ostracod group in Palaeogene deposits in Europe.     

Pliocene ostracods of Southwestern Europe

This paper analyzes the lithostratigraphic features and ostracod associations of the Pliocene deposits located in the western sector of the Guadalquivir basin (SW Spain). A regressive cycle is defined by the vertical distribution of five main facies (FA-1 to FA-5), which were deposited in upper bathyal to fluvial palaeoenvironments. The broad palaeontological record is utilized to draw a general outline of the food chain in each palaeoenvironment. A comparison with the Pliocene ostracod distribution of southeastern Spain, southwestern France and Portugal permits to define a common ostracod biozonation for southwestern Europe during this period. Four main marine biozones are distinguished: (a): Pontocythere elongata biozone (infralittoral); (b): Costa edwardsii biozone (shallow circalittoral); (c): Bosquetina carinella biozone (deep circalittoral); and (d): Henryhowella asperrima biozone (upper bathyal). Freshwater, brackish and lower bathyal/abyssal species are very scarce in this area during this period.     

Patterns in early embryonic motility: effects of size and environmental temperature on vertical velocities of sinking and swimming echinoid blastulae

Early embryonic swimming is widespread among marine invertebrates, but quantitative information about swimming behaviors is scarce. Swimming may affect encounters with predators, positioning in the water column, and nutrient absorption. Measured rates and patterns of swimming and sinking for blastulae of four eastern Pacific echinoid species show that sinking speeds equal or exceed swimming speeds. Swimming speed scaled negatively with embryo size, though sinking speed did not scale with size. Analysis of swimming paths of Strongylocentrotus franciscanus revealed a temperature dependency in swimming pattern that affected speed of upward movement. Sinking speeds were significantly greater at 10 degrees C than at 14 degrees C for blastulae of all four species examined. In Dendraster excentricus, killing the blastulae annulled this temperature effect, indicating an active density regulation by these embryos. Finally, measurements of particle velocities around sinking and swimming D. excentricus blastulae show that swimming creates a more localized disturbance than sinking. Embryonic swimming may therefore decrease rather than increase encounters with pelagic predators. Results from subsequent experiments in which embryos were reared in low-oxygen environments suggest that any oxygen-absorption advantages of swimming have little, if any, effect on the development of D. excentricus embryos.     

Palaeozoic roots of the sigilliid ostracods

Podocopine ostracods rapidly increased in species diversity after the Palaeozoic, and 32 out of the 36 podocopine families are extant (Whatley et al., 1993), but the phyletic origins are known for only a few. The Sigilliacea are unique in having a long and detailed fossil record. The Sigilliidae known from the recent and Mesozoic faunas differ from others ostracods in having large adductor muscle scars with many spots, a character typical rather to Palaeozoic forms. Paleozoic Microcheilinellidae were morphologically close to the sigilliids, but details of their hingement and carapace margin structures were unknown until now.Silicified specimens of Microcheilinella mendelgrammi, new species, from the Early Carboniferous of southern China and Microcheilinella mandelstami, from the Middle Devonian of north-western Poland show merodont hingement and narrow calcified inner lamella. This makes their relationship to the Mesozoic, Tertiary, and recent sigilliids Saipanetta, Cardobairdia, Sigillium, and Kasella likely. The sigilliid lineage was thus established already in the Devonian.Tubulibairdia, with adont hingement and tubulous shell wall, and Microcheilinella s. s., with merodont hingement and no tubules, are distinct genera in different families.     

The in situ sinking rates of herbivore fecal pellets

The vertical flux of pigmented fecal pellets was measured forperiods of 4 h or less with closely spaced sediment traps. Thesettling of the nighttime injection resulting from macrozooplanktongrazing activity could be monitored as the pellets settled throughthe water column. Sinking rates of fecal pellets showed a rangeof 31 – 122 m d^–1 with an average of 87 m d^–1.Longer term experiments show that the vertical phaeopigmentflux is conservative, and that there is no significant lossof pigments en route to the sea floor. In Dabob Bay, coprophagyin the water column is most likely a minor consideration. Theamount of chlorophyll sinking out of the euphotic zone usuallyrepresents <1% of the standing crop, and is usually only5% or less than the phaeopigment flux. This suggests that grazingis the predominant process accounting for the major loss ofchlorophyll from the water column. ¹Contribution no. 1332 from the School of Oceanography, Universityof Washington, Seattle, WA 98195, USA. ²Present address: The Biological Laboratories, Harvard University,Cambridge, MA 02138, USA.     

Functional morphology of Palaeozoic ostracods: phylogenetic implications

Recent discussions of ostracod systematics have focused on soft anatomy, both as seen in extant groups and as recorded by rare examples of special fossil preservation. The position of the fossil Palaeocopina and Leperditicopida, for which no substantial soft part evidence has yet been found, remains in the view of post-Palaeozoic workers uncertain, with some doubt as to whether they should be retained within the Ostracoda. The evolution of carapace bauplans (e.g. the development of brood pouches and lobal structures in palaeocopids as well as the development of adductor muscle scar patterns, calcified inner lamellae and carapace incisures in podocopines) is discussed in relation to presumed soft anatomy. It seems possible to distinguish between plesiomorphic (ancestral, simple) and apomorphic (derived, advanced) characters and consider their significance in ostracod systematics. Although the presumed ‘protostracod’ is not known, the combination of soft anatomy, carapace architecture and behaviour (feeding techniques, brood care) provide evidence of a general body plan which appeared (at the latest) during the Ordovician and continuously evolved towards the anatomy of modern ostracods. In parallel lineages, plesiomorphic forms have died out (leperditicopids and most palaeocopines as well as metacopines), while apomorphic lineages (‘drepanellid archetype’ of palaeocopines; resistant platycopines, podocopines and myodocopines) have survived all extinction events. The evidence supports the retention of the Palaeocopina (and probably the Leperditicopida) in the Ostracoda.     

A review of the freshwater ostracods of New Zealand

Summary The freshwater ostracod fauna of New Zealand is reviewed, and a key is given to the 28 known living species, belonging to 18 genera. 10 new species are described, and 8 genera are recorded for the first time from New Zealand. Brief notes on the habitat and life-history of some of the species are given.Present address: Dept. of Zoology, The University, Glasgow     

Arctic quaternary ostracods and their use in paleoreconstructions

The paper deals with original and published data on fossil ostracodal assemblages from the Eurasian Arctic Kara, Laptev and Chuckchi seas. As a whole, six ecologically different assemblages were distinguished (freshwater, brackish water, marine of the inner, middle and outer shelves and upper continental slope), they replace each other upcore reflecting a gradual increase in water depth and distance from the coast. These assemblages are stable in the entire Arctic region and can be used for interpretation of environments in different Arctic areas.     

Evolution of antennules of cytheroidean ostracods (Crustacea)

Phylogenetic analysis and fossil records indicate that antennules with whip-like setae are the most plesiomorphic state in cytheroidean ostracods and that antennulae with claw-like setae are derived from antennulae with whip-like setae. Character distributions on the 18S rDNA molecular phylogenetic tree suggest that two phenotypic features of cytheroidean antennules (W/L ratio and claw-like/whip-like setae) have morphological plasticity. These features have evolved as an ethological adaptation rather than due to phylogenetic constraints such as the evolution of shell outline in cytheroideans. However, the species of the Leptocytheridae–Trachyleberididae clade generally have stout, robust antennules, indicating a phylogenetic constraint. The character state of setae (claw/whip) in cytheroidean ostracods is reflected more through their ethology than the W/L ratio of the antennules. On the basis of the present analysis and the fossil record, diversification in the morphology of the antennules seems to have occurred during the early Mesozoic.     

生物相容性MEDPOR仪眼治疗眼窝塌陷畸形

目的：探讨眼窝塌陷畸形的重建手术方法和临床效果,方法：对42例无眼球或眼球萎缩伴眼窝塌陷形的患者,行高密度多孔聚乙烯（MEDPOR）义眼座植入联合穹隆成形术,结果：所有患者眼窝畸形均得以矫正,随访6个月－3年,义眼座在眼眶内无脱出,移位或合并感染,装入仿真义眼片后,双眼对称,义眼活动度可达10－20度,结论：MEDPOR义眼座植入联合穹隆成形术矫治复杂性眼窝畸形在总体上取得了良好的效果,MEDPOR义眼具有良好的组织相容性,是矫正眼窝塌陷畸形的理想材料。     

Two new species of freshwater ostracods from Southern India

Two new species of freshwater ostracods are described from Southern India and their taxonomic validity is discussed.     

The causes of sinking and floating in turions of Myriophyllum verticillatum

The sinking and floating (density) of the special winter buds (turions) produced by many aquatic plants play important roles in their life cycles, yet there has been little experimental study of these phenomena. However, it has been postulated that starch determines the density of turions. In order to test this hypothesis, turions of Myriophyllum verticillatum L. were collected from October through April and analyzed for density, dry-to-fresh-weight ratio and starch content. Density did not correlate closely (R² = 0.37) with the dry-to-fresh-weight ratios. Density strongly correlated (R² = 0.99) with starch only in the January collections, but not at several other times, so starch content alone is not always the major determinant of turion density. Intracellular lacunae (potentially gas spaces) also occur within the axes of these turions, and the lacunal volumes increased ca. 20-fold as they resumed growth, at which time the turions started to float. Significantly, turions, which were near the density of water, could be sunk or floated by changing the ambient pressure (which would alter their internal gas volume). Thus, starch has a role in determining the density of M. verticillatum turions, but the amount of intercellular gas space may be more important, especially when they resume growth in the spring.     

The morphology of the upper lip of Cypridoidea ostracods: taxonomic and phylogenetic significance

This paper represents the first study of the morphology of the upper lip (labrum) and hypostome of ostracods using scanning electron microscopy (S.E.M.). There is considerable variation in the upper lip morphology of the 23 species of Cypridoidea (Podocopina) ostracods used in this study. The detail of the upper lip morphology of each species is very distinctive, so that species determination can be made on this feature alone, but it is not useful in diagnosing genera or subfamilies. The hypostome is not readily studied due to the large amounts of dense pseudochaetae (small, setae-like projections) protruding from it and hence is considered not to be a useful taxonomic feature. Several features of the upper lip and mouth region are documented for the first time. Comparisons of the general morphology of the upper lips of Recent ostracods with the upper lip of the fossil ostracod Pattersoncypris micropapillosa Bate, 1972, indicate that there has been very conservative evolution in these features since the Cretaceous.     

On the wind-induced sinking of Sargassum

Sargassum has been photographed on the sea floor at depths of 5000 m. Sargassum was subjected to various pressures to simulate the effect of it being carried down in Langmuir circulation. The time-depth relation for Sargassum to become negatively buoyant was measured; the plant can become negatively buoyant at pressures of only 30 db if left at this pressure for ≈ 5 h. Both the higher critical pressure for the failure of gas vesicles and the longer resistance to subcritical pressure of pelagic Sargassum, compared with the benthonic varieties, suggest an evolutionary adaptation to an open ocean existence. Once negatively buoyant, Sargassum will sink to the sea floor in about 40 h. The measurements are consistent with large scale sinking of Sargassum given the conditions of strong winds and a deep mixed layer both of which exist in winter months in the Sargasso Sea.     

The sinking ark: pollution and the worldwide loss of biodiversity

Humans are making increasing demands on natural ecosystems. One recent study has concluded that our species is consuming or diverting some 40% of the net photosynthetic productivity of our planet. Many habitats are being converted to simpler systems which provide more harvestable goods to people. As a result, genetic diversity, species and whole ecosystems are disappearing; some scientists suggest that as many as 25% of the world's species could be lost in the next several decades.The sinking ark is usually characterized in terms of pollution, habitat loss, poaching, introduced species and illegal trade in wildlife products, but these are symptoms rather than causes. At a more fundamental level, many of the same factors which have enabled pollution to become such a problem have also been responsible for the loss in biodiversity; the most important factor is that the effects of pollutants on biodiversity have been considered an externality, an unintended side effect of industrial activity which brought measurable benefits to people. Development activities which have depleted biodiversity have proven profitable only because the real costs have been hidden.Keeping the ark afloat will require the Five-I Approach: investigation (learning how natural systems function); information (ensuring that the facts are available to inform decisions); incentives (using economic tools to help conserve biodiversity); integration (promoting a cross-sectoral approach to conserving biodiversity); and international support (building productive collaboration for conserving biodiversity).     

Critical flow velocities for the growth and dominance of Anabaena circinalis in some turbid freshwater rivers

SUMMARY 1. From measurements at several weir pool sites along the turbid and freshwater Barwon‐Darling River, Australia, the development of persistent stratification (for periods of >5 days) was related to river discharge. For the sites examined, the required discharge to allow the development of persistent stratification was between 100 and 450 ML day^?1 during the hotter months. High discharge during the hotter months did not allow the formation of persistent stratification, although diel stratification did occur. Low discharge through the cooler months resulted in diel stratification, although persistent stratification lasting for a few days could occur at times. 2. The growth and dominance of Anabaena circinalis at these sites was closely related to the establishment and maintenance of persistent and strong thermal stratification. Growth only occurred during extended periods (>5 days) of persistent stratification. These conditions not only restrict the displacement of A. circinalis downstream, they also allowed the alga to accumulate in surface waters. 3. The discharge levels required to suppress the formation of persistent stratification at the study sites were variable because of large differences in channel cross‐sectional area. To compensate for this variation, the discharges were converted to flow velocities. A critical velocity of 0.05 ms^?1 was sufficient for the suppression of persistent thermal stratification and concurrent A. circinalis growth for all sites. The turbulent velocity (u*) under weak wind mixing at the study locations varied between 2.66 × 10^?3 and 2.91 × 10^?3 ms^?1 at the critical flow velocities. These values may have potential to be applied to other rivers in similar climatic zones to suppress nuisance cyanobacterial growth.     

First record of ostracods (Crustacea) in Baltic amber

Ostracods were found in two pieces of Baltic amber for the first time. The animals belong to the freshwater genus Cyclocypris. Since Baltic amber was formed during Eocene times in southern Scandinavia, the age of the specimens is estimated at 42–54 million years. As aquatic organisms, ostracods are seldom trapped in amber; it is considered that one specimen, already dead and dried, was either blown onto sticky resin on a plant stem, or washed there by a high flood level, while the other was probably splashed, alive, in a drop of water against the flowing resin, again probably during a flood. Associated faunal remains, including other crustaceans, suggest a coastal palaeoenvironment with some marine as well as freshwater influence.