Taxonomy and sexual dimorphism of a new species of Loxoconcha (Podocopida: Ostracoda) from the Pleistocene of the Japan Sea

A new ostracod, Loxoconcha kamiyai sp. nov. in the Family Loxoconchidae, is described from the Pleistocene Omma Formation of Japan. Its geological and geographical distributions suggest that this species was once endemic to the Japan Sea, where it would have evolved until the Pliocene. Since the early Pleistocene, this species would have become extinct within this marginal sea during glacial maxima, probably due to its narrower salinity tolerances and geographical distributions than those of extant species inhabiting the euryhaline environments in other seas. The distributional patterns of pore systems in this species strongly suggest its closest phylogenetic affinities to a living species, Loxocorniculum mutsuense . These two species show a unique adult sexual dimorphism in the anterior element of the hingement. Taking the female hingement morphology as a standard, the male hingement can be explained in terms of heterochrony, i.e. paedomorphosis. Sexual hingement dimorphism with paedomorphosis occurs in only one phylogenetic group of the genus Loxoconcha , which is distinguished by the ontogenetic distributional patterns of pore systems. This morphology may represent relict primitive characters of ancient ostracods and could be an important character for evaluating the history of sexual dimorphism in ostracods since the Palaeozoic.  © 2008 The Linnean Society of London, Zoological Journal of the Linnean Society , 2008, 153 , 239–251.     

Calcium translocations during the moulting cycle of the semiterrestrial isopod <Emphasis Type="Italic">Ligia hawaiiensis</Emphasis> (Oniscidea,Crustacea)

Terrestrial isopods moult first the posterior and then the anterior half of the body. During the moulting cycle they retain a significant fraction of cuticular calcium partly by storing it in sternal CaCO₃ deposits. We analysed the calcium content in whole Ligia hawaiiensis and the calcium distribution between the posterior, the anterior ventral, and the anterior dorsal cuticle during four stages of the moulting cycle. The results indicate that: (1) overall, about 80% of the calcium is retained and 20% is lost with the exuviae, (2) in premoult 68% of the calcium in the posterior cuticle is resorbed (23% moved to the anterior ventral cuticle, 17% to the anterior dorsal cuticle, and the remaining 28% to internal tissues), (3) after the posterior moult 83% of the calcium in the anterior cuticle is shifted to the posterior cuticle and possibly to internal storage sites, (4) following the anterior moult up to 54% of the calcium in the posterior cuticle is resorbed and used to mineralise the new anterior cuticle. ⁴⁵Ca-uptake experiments suggest that up to 80% of calcium lost with the anterior exuviae may be regained after its ingestion. Whole body calcium of Ligia hawaiiensis is only 0.7 times that of the fully terrestrial isopods. These terrestrial species can retain only 48% of whole body calcium, suggesting that the amount of calcium that can be retained by shifting it between the anterior and posterior integument is limited. We propose that fully terrestrial Oniscidea rely to a larger degree on other calcium sources like internal stores and uptake from the ingested exuviae.     

Late Glacial and Holocene Ostracoda of the Gulf of Gdańsk,the Baltic Sea,Poland

To trace environmental changes in water hydrology and salinity in the Late Glacial to Holocene of the Gulf of Gdańsk, a south‐eastern bay of the Baltic Sea within the maritime zone of Poland, the distribution of ostracod valves was studied in 20 sediment cores collected from both the shallow‐ and deep‐water zones (depth 10.9–67.5 m). The studied sediment sequences yielded ca. 3000 valves of 21 ostracod species, of which only five are known to live today in the Gulf, which has a present maximum depth of 118 m and water salinity up to 7–8‰. The majority of the studied sediment layers that contained ostracod valves corresponded to the period of the Late Glacial to Mid‐Holocene and was dominated by non‐marine species, of which the most common were Candona neglecta (present in 17 cores), Cytherissa lacustris (15 cores) and Candona candida (14 cores). By clustering classification five major ostracod assemblage types were recognised in the studied cores. Initial assemblage types dominated mostly by inhabitants of the profundal/sub‐littoral zones of modern oligo‐mesotrophic lakes (C. lacustris and C. neglecta) in some sediment sequences were replaced in stratigraphical order by the assemblages dominated by brackish‐water species (Cyprideis torosa or Cytheromorpha fuscata). The structure and species composition of the distinguished ostracod assemblage types as well as their successional transitions indicate that the studied sediments were deposited initially in the Late Glacial in freshwater lacustrine conditions, and subsequently, during the Holocene marine transgression, covered by marine sands. The present results confirm and consolidate inferences based on previously published data on ostracods from the western part of the Gulf of Gdańsk as well as on other biotic (molluscs, diatoms) and abiotic (seismoacoustic) indices from this area (© 2012 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)     

Development of the venom ducts in the centipede Scolopendra: an example of recapitulation

In contrast to previous claims that (a) there is a law of recapitulation and, conversely, (b) recapitulation never happens, the evolutionary repatterning of development can take many forms, of which recapitulation is one. Here, we add another example to the list of case studies of recapitulation. This example involves the development of the venom claws (forcipules) in the centipede Scolopendra subspinipes mutilans, and in particular the development of the duct through which venom flows from the gland that produces it (proximal) to the opening called the meatus (distal) through which it is injected into prey. Most of the information we present is from early postembryonic stages—these have been neglected in previous work on centipede development. We show that the venom ducts arise from sutures that are invaginations of the cuticle. In S. s. mutilans, the invagination in each forcipule forms into a tubular structure that detaches itself from the exoskeleton and moves toward the center of the forcipule. This is in contrast to extant Scutigera, and also, probably, Scolopendra's extinct Scutigera‐like ancestors, where the duct remains attached to the cuticle of throughout development. Thus, S. s. mutilans exhibits a recapitulatory repatterning of development.     

The affinities of the ostracod genus Cypridea Bosquet, 1852, and its allies, with consideration of implications for the phylogeny of nonmarine cypridoidean ostracods

The nonmarine ostracod genus Cypridea s.l., characterized by an antero-ventral “beak” (rostrum and alveolus) in both valves, achieved high diversity and global distribution in the Early Cretaceous but declined in the Late Cretaceous and became extinct during the Paleogene. Although it clearly belongs to the Superfamily Cypridoidea (Order Podocopida, Suborder Cypridocopina), the precise affinities of Cypridea s.l. have been controversial, different authors variously suggesting it to be most closely related to the cypridoidean families Ilyocyprididae, Cyprididae or Notodromadidae. Since Cypridea s.l. was responsible for much of the explosive radiation of nonmarine cypridoidean taxa during the Mesozoic, a clear understanding of its affinities is crucial to the elucidation of nonmarine ostracod phylogeny. We evaluate some of the key morphological features of cypridoidean carapaces as indicators of phylogenetic affinity, paying special attention to adductor muscle scar patterns and the structure of the anterior marginal zone. The morphology of Cypridea s.l. is compared with certain cypridoideans that bear similar beak-like or lip-like antero-ventral marginal structures, notably genera of the Family Cyprididae such as Bennelongia, Chlamydotheca, Cypris and Talicypridea, and consider whether these similarities represent close phylogenetic relationships or homeomorphy.     

Purification of phenolic compounds and a phenoloxidase from larval cuticle of the red-humped oakworm,Symmerista cannicosta francl

A phenoloxidase has been extracted, purified, and characterized from cuticle of last-instar larvae of the red-humped oakworm, Symmerista cannicosta. It is a typical tyrosinase (EC 1.10.3.1., o-diphenol:O₂ oxidoreductase), active toward o-diphenols but not p-diphenols, inhibited by thiourea and phenylthiourea, with a pH optimum between 6.0 and 7.2. In these respects it resembles enzyme A of C. vicina, one of the few species from which this presumed wound healing enzyme has been purified and characterized. Hydrolysis of either exuviae or intact cuticle from last instar larvae yielded a number of ketocatechols of which the most abundant, 2-hydroxy, 3′,4′-dihydroxyacetophenone, represented 2.9% of the dry weight of head capsule exuviae, 0.3% of exuviae from the remainder of the body, and 4.6% of the dry weight of head capsule cuticle from previously frozen intact larvae. Differences in the type and amount of ketocatechol recovered from these cuticles are described.     

Exuviae eating: a nitrogen meal?

Many insects eat their cast cuticle (exuviae) after moulting. The functional significance of this behaviour has not been addressed experimentally. I tested the hypothesis that exuviae eating constitutes a meal, so the animal recycles its nitrogen content. Nitrogenous compounds (protein and chitin) are major components of the cuticle in Periplaneta americana, accounting for as much as 87% of the total weight. It was found that insects almost invariably ate their exuviae during their larval life. The frequency of the behaviour decreased in newly emerged adults and varied between the sexes, males eating their exuviae less frequently than females. This may be due to the extra nitrogen endowment which females need for reproduction. Aposymbiotic animals, which lack the supply of essential amino acids from endosymbiotic bacteria, always ate their exuviae regardless of sex. When animals were reared on different diets throughout their larval life protein level in the diet correlated with exuviae eating. Animals reared on a low protein diet showed the highest levels of exuviae eating; animals reared on a high protein diet showed the highest levels of exuviae rejection. Analysis of the frass produced after exuviae meals showed that over 58% of the nitrogen present in the exuviae was recycled. This demonstrated that cockroaches digested nitrogenous compounds contained in the cuticle. The possibility that the exuviae meal has other functions is discussed, although the evidence supports a nutritional role.     

A new giant cypridid ostracod (Crustacea) from southern Buenos Aires Province,Argentina

Amphicypris argentinensis sp. nov., is described and illustrated from Laguna Caliba, an ephemeral fresh water lake from the southern coast of Buenos Aires Province, Argentina. Specimens were raised from dried sediment recovered from a bank of ostracod shells found at the edges of the lake. Deposition of progressively smaller ostracod valves stacked one into another (cup-in-cup structure) is documented. The geographical distribution and ecology of the genus is briefly discussed.     

A new giant cypridid ostracod (Crustacea) from southern Buenos Aires Province, Argentina

Amphicypris argentinensis sp. nov., is described and illustrated from Laguna Caliba, an ephemeral fresh water lake from the southern coast of Buenos Aires Province, Argentina. Specimens were raised from dried sediment recovered from a bank of ostracod shells found at the edges of the lake. Deposition of progressively smaller ostracod valves stacked one into another (cup-in-cup structure) is documented. The geographical distribution and ecology of the genus is briefly discussed.     

Catechols involved in sclerotization of cuticle and egg pods of the grasshopper,Melanoplus sanguinipes,and their interactions with cuticular proteins

N‐Acetyldopamine (NADA) is the major catechol in the hemolymph of nymphal and adult grasshoppers, Melanoplus sanguinipes (F.), and mainly occurs as an acid‐labile conjugate indicated to be a sulfate ester. Its concentration increases in last instar nymphs and peaks during adult cuticle sclerotization. Dopamine (DA), the precursor of NADA and melanic pigments, is about 10 times lower in concentration than NADA, but shows a similar pattern of accumulation. NADA also predominates in cuticle, but its concentration is lowest during the active period of sclerotization, reflecting its role as a precursor for quinonoid tanning agents. Two other catechols, 3,4‐dihydroxybenzoic acid (DOBA) and 3,4‐dihydroxyphenylethanol (DOPET), also occur in hemolymph and cuticle, and their profiles suggest a role in cuticle stabilization. Solid‐state NMR analysis of sclerotized grasshopper cuticle (fifth instar exuviae) estimated the relative abundances of organic components to be 59% protein, 33% chitin, 6% catechols, and 2% lipid. About 99% of the catechols are covalently bound in the cuticle, and therefore are involved in sclerotization of the protein‐chitin matrix. To determine the types of catechol covalent interactions in the exocuticle, samples of powdered exuviae were heated in Hcl under different hydrolytic conditions to release adducts and cross‐linked products. 3,4‐Dihydroxyphenylketoethanol (DOPKET) and 3,4‐dihydroxyphenylketoethylamine (arterenone) are the major hydrolysis products in weak and strong acid, respectively, and primarily represent NADA oligomers that apparently serve as cross‐links and filler material in sclerotized cuticle. Intermediate amounts of norepinephrine (NE) are released, which represent N‐acetylnorepinephrine (NANE), a hydrolysis product of NADA bonded by the b‐carbon to cuticular proteins and possibly chitin. Small quantities of histidyl‐DA and histidyl‐DOPET ring and side‐chain C‐N adducts are released by strong acid hydrolysis. Therefore, grasshopper cuticle appears to be sclerotized by both o‐quinones and p‐quinone methides of NADA and dehydro‐NADA, which results in a variety of C‐O and C‐N covalent bonds linked primarily through the side‐chain carbons of the catechol moiety to amino acid residues in cuticular proteins. The primary catechol extracted from both the female accessory glands/calyx and the proteinaceous frothy material of the egg pod is DOBA, which also commonly occurs in cockroach accessory glands and oothecae, presumably as a tanning agent precursor. 3,4‐Dihydroxyphenylalanine (DOPA) was also detected in extracts of the accessory glands/calyx of grasshoppers, and may serve as a precursor for DOBA synthesis. Arch. Insect Biochem. Physiol. 40:119–128, 1999. © 1999 Wiley‐Liss, Inc.     

Ostracod fauna of Duvensee,an ancient lake in Northern Germany

About 4000 ostracod valves have been analysed from a sediment core of a cultivated bog NW of Hamburg. The deepest deposits are sands free of subfossils, the uppermost layers consist of peat. In the sediment in between, there are three layers containing undestroyed valves. The ostracod assemblies of the older claygyttja (Late-glacial) and the two younger, fine detritus deposits (Post-glacial) are strikingly different. Cytherissa lacustris, Candona neglecta, Ilyocypris bradyi, Herpetocyrpis reptans, and two Limnocythere species were found in the Late-glacial layers. Changes in abundance of these species indicate alterations in climate, lake ground, water inflow and waterlevels. Postglacial layers are rich in Metacypris cordata valves associated with numerous Candona species, L. inopinata, Darwinula stevensi, and Cyclocypris laevis. These species are characteristic of a small lake with a large littoral zone. A similar development in ostracod assemblages is found in middle Europe by Absolon (1973), although the main Candona species is not C. neglecta but C. candida. Ostracod analysis cannot demonstrate an influence of anthropogenic impacts on ostracod successions.     

Cyanoglucoside storing cuticle of Zygaena Larvae (Insecta,Lepidoptera)

Summary As a deterrent against predators, larvae of Zygaena trifolii release droplets of fluid containing cyanoglucosides from segmentally arranged cuticular cavities. Histological examinations show that during the moulting period, the old cuticle, including the cavities and the secretion within them, is degraded, with the exception of a thin mesocuticular layer forming the exuviae. When the endocuticular layer of the new cuticle is deposited, the cuticle detaches from the underlying epidermis in specific areas, which leads to the formation of the cuticular cavities. During a moult-intermoult sequence the concentration of cyanoglucosides in both the haemolymph and the defensive secretion shows specific changes. These changes seem to be related to the formation and degradation of the cavities. We suggest that during the moult the cyanoglucosides are transported through the epidermis into the haemolymph to prevent them from being wasted with the exuviae and, after ecdysis, are retranslocated into the newly formed cavities.     

Trace elemental distribution in ostracod valves. From solution ICPMS and laser ablation ICPMS to microprobe mapping: a tribute to Rick Forester

A historical perspective on our understanding of the formation of ostracod valves and what they consist of is presented here, together with the history of investigations on the chemistry of ostracod valves. It is now clear that ostracod valves are made of 3 distinct layers consisting of calcite crystallites/rhombs that are held together by a significant network of organic fibrils which may also contribute to the trace elemental composition of ostracod valves when analysed by solution chemistry. The outer epicuticle of ostracod valves, when well preserved such as in modern material, contributes to an enrichment in magnesium, and this ought to be taken into account when interpreting the Mg/Ca of ostracod valves for use with water temperature reconstructions. Recommendations about the analytical techniques used for chemical analysis of ostracod valves are presented.     

Experimental adaptation to marine conditions by a freshwater alga

The marine‐freshwater boundary has been suggested as one of the most difficult to cross for organisms. Salt is a major ecological factor and provides an unequalled range of ecological opportunity because marine habitats are much more extensive than freshwater habitats, and because salt strongly affects the structure of microbial communities. We exposed experimental populations of the freshwater alga Chlamydomonas reinhardtii to steadily increasing concentrations of salt. About 98% of the lines went extinct. The ones that survived now thrive in growth medium with 36 g?L^?1 NaCl, and in seawater. Our results indicate that adaptation to marine conditions proceeded first through genetic assimilation of an inducible response to relatively low salt concentrations that was present in the ancestors, and subsequently by the evolution of an enhanced inducible response to high salt concentrations. These changes appear to have evolved through reversible and irreversible modifications, respectively. The evolution of marine from freshwater lineages is an example that clearly indicates the possibility of studying certain aspects of major ecological transitions in the laboratory.     

Feeding by Priapulus caudatus (Cephalorhyncha: Priapulidae): observations of the effects of seasonal temperature change and molting

The ecdysozoan Priapulus caudatus belongs to a phylum of exclusively marine worms that reigned among the most abundant benthic metazoans during the Cambrian. Usually found at great depths, this species can occasionally be found among intertidal habitats fed by exceptionally cold sea water and predominated by soft mud, as in the Lower Bay of Fundy. Live priapulids were collected there and the effects of molting and seasonally changing ambient sea water temperature on feeding were observed in the laboratory beginning in February. Feeding increased as ambient sea water temperatures increased from March through April, a relationship significantly correlated (p < 0.001). This association rapidly deteriorated once 11 °C was reached in May with no animals feeding above 13 °C. Priapulids fed until the first molt day when feeding significantly decreased (p = 0.016). This response was short-lived, and feeding slowly resumed among animals within a week post-molt. Exuvia were not consumed. The onset of molting followed color changes in cuticle appearance and was significantly correlated with increasing temperature (p < 0.001). Molting was rapid, with the exuviae clearly separated from the new cuticle within 24 h at places where the process began. Without substrate to burrow into, animals emerged from shed exuviae between 3 and 29 days, with larger animals taking longer. While the cold deep-sea is the primary habitat of P. caudatus, this species shares some of the effects of temperature and molting on feeding shown by other ecdysozoans. The observations made during this study place a limit on where P. caudatus might be found intertidally.     

Patterning of a compound eye on an extinct dipteran wing

We have discovered unexpected similarities between a novel and characteristic wing organ in an extinct biting midge from Baltic amber, Eohelea petrunkevitchi, and the surface of a dipteran's compound eye. Scanning electron microscope images now reveal vestigial mechanoreceptors between the facets of the organ. We interpret Eohelea's wing organ as the blending of these two developmental systems: the formation and patterning of the cuticle in the eye and of the wing. Typically, only females in the genus carry this distinctive, highly organized structure. Two species were studied (E. petrunkevitchi and E. sinuosa), and the structure differs in form between them. We examine Eohelea's wing structures for modes of fabrication, material properties and biological functions, and the effective ecological environment in which these midges lived. We argue that the current view of the wing organ's function in stridulation has been misconstrued since it was described half a century ago.     

Appendage Homologies and the First Record of Eyes in Platycopid Ostracods, with the Description of a New Species of Keijcyoidea (Crustacea: Ostracoda) from Japan

A median nauplius eye is reported for the first time in a platycopid ostracod, a group hitherto considered to be blind. A new species of the platycopid ostracod genus Keijcyoidea is described from coastal rocky marine habitats on the Pacific coast of Japan. Observations of living specimens in the laboratory show that it is capable of burrowing to a depth of several millimeters in sandy sediment, using the first two head appendages (antennulae and antennae) and the furca. Females brooded a maximum of five eggs in the posterior brood space of the carapace. The homologies and phylogenetic implications of the trunk segmentation and limbs are discussed, paying particular attention to the sexually dimorphic fifth and sixth limbs; the copulatory appendages of both sexes are interpreted as being attached to trunk segments T6–T7 (counting from the posterior; T1 = posteriormost segment).     

川东中侏罗统新田沟组介形类化石壳体方解石化特征及元素成分初步分析

首次利用扫描电子显微镜观察川东新田沟组介形类化石的保存情况,并利用X射线能谱分析部分化石的元素含量及分布。研究发现新田沟组介形类壳体绝大部分方解石化,不同层位介形类壳质方解石化有所不同,且方解石化特点显示其可能与有机质作用有关。通过与前人研究结果对比发现,新田沟组壳体保存处在介形虫壳体埋藏作用的第二阶段和第三阶段。     

Accessory Pollen Adhesive from Glandular Trichomes on the Anthers of Leonurus sibiricus L. (Lamiaceae)

Abstract: Glandular trichomes (ca. 16 per anther) on the anthers of Leonurus sibiricus produce a secretion that, when touched, is liberated at once and becomes sticky when in contact with the air. With successive visitations of the pollinators (species of Bombus in naturalized populations) the number of secretion‐containing glands on each anther diminishes by mechanical rupture. On the pollinators, the secretion mixed with pollen was found adhered to the integument on the parts making contact with the anthers and stigma, mostly on the scape of the antennae. These trichomes are anatomically identical to the glandular scales common in the entire family and are formed by a multicellular cuticle‐bounded structure, with a foot and head. The secretion is accumulated as a milky emulsion under the cuticle, outside the primary cell wall, and is liberated by rupture of the cuticle. The composition possibly differs from what generally distinguishes these glandular trichomes, i.e. volatile oils that give these plants their particular smell. Such volatile compounds are generally assumed to have defensive or attractive functions, different from those observed in this study, which would be strictly mechanical.