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In this paper eight tribes (Gyrophaenini, Placusini, Homalotini, Diestotini, Falagriini, Athetini, Lomechusini, and Oxypodini), 19 genera and 42 species are recognized. Four genera (Brachyglyptaglossa n. gen. [Homalotini], Trisporusa n. gen., Daccordiusa n. gen. [Lomechusini], and Antistydatusa n. gen. [Oxypodini]) and 37 species are described as new. Each new genus and species is illustrated. Placusa fauveli Pasnik, 2001, from Sydney, is placed in synonymy with Placusa tridens Fauvel, 1878, from Sydney. A new combination to Spallioda for Calodera carissima Oliff is proposed.
A taxonomic study of the Staphylinid subfamily Aleocharinae of the Australian Region is presented, including a critical revision of 14 typical series, the lectotype of which is designated when necessary. 10 new genera are deseribed (3 in Athetini, 2 in Thamiaraeini, and 5 in Oxypodini) and 38 species (3 in Gyrophaenini, 2 in Bolitocharini, 4 in Diestotini, 21 in Athetini, 5 in Thamiaraeini, and 3 in Oxypodini). New combinations are proposed for 12 species (l in Homalotini, 1 in Diestotini, 3 in Athetini, 6 in Oxypodini, and 1 in Aleocharini). The genus Correa Fauvel is considered junior synonym of the genus Aleochara. Every new genus and species is described and illustrated.
Australia has a diversity of vectors and vector-borne human diseases. Mosquito-borne arboviruses are of greatest concern, but there are issues with other vector and pathogen systems. Mosquitoes were responsible for more than 35,000 cases of Ross River virus during 1991-1997. Barmah Forest virus is increasing nationwide, and unidentified bunyaviruses suspected of causing illness have been isolated. Cases of Murray Valley encephalitis have occurred in 14 of the past 20 years in northern Australia. Dengue is a continuing problem for northern Queensland, with various serotypes being active. Japanese encephalitis has appeared in the Torres Strait Islands and threatens mainland Australia. Although malaria is eradicated, almost 1,000 cases are imported annually and occasional cases of local transmission occur. With ticks, paralysis in children occurs annually in eastern Australia. Tick typhus (Queensland Tick Typhus--Rickettsia australis) occurs down the east coast, and (Flinders Island Spotted Fever--Rickettsia honei) in Bass Strait and probably Tasmania. Lyme disease is reported but its presence is controversial. Fleas were responsible for a recent outbreak of murine typhus (Rickettsia typhi) in Western Australia. Mites cause scrub typhus (Orientia tsutsugamushi), and there was a recent fatality in the Northern Territory. Overall, resources for investigation and control of vector-borne disease have generally been meager. However, various avenues of basic and applied research have been pursued, and have included investigations into mosquito ecology, vector competence, disease epidemiology, and vector control. Disease surveillance programs vary between states, and mosquito control programs are organized and effective in only a few regions. There are concerns for import of vectors such as Aedes albopictus and export of pathogens such as Ross River virus; the former has occurred but the species has not become established, and the latter has occurred and has resulted in a major outbreak in the South Pacific. The predicted scenarios of increased temperature and rainfall with global warming are also causing concern for increases in vector-borne diseases, particularly the endemic arboviruses. Interest by health authorities is gravitating more towards epidemiological reporting and less towards public health action. In many respects, humans have much to do to get "on top" of vectors and their pathogens "down under" in Australia.
The Siwalik formations of northern Pakistan consist of deposits of ancient rivers that existed throughout the early Miocene through the late Pliocene. The formations are highly fossiliferous with a diverse array of terrestrial and freshwater vertebrates, which in combination with exceptional lateral exposure and good chronostratigraphic control allows a more detailed and temporally resolved study of the sediments and faunas than is typical in terrestrial deposits. Consequently the Siwaliks provide an opportunity to document temporal differences in species richness, turnover, and ecological structure in a terrestrial setting, and to investigate how such differences are related to changes in the fluvial system, vegetation, and climate. Here we focus on the interval between 10.7 and 5.7 Ma, a time of significant local tectonic and global climatic change. It is also the interval with the best temporal calibration of Siwalik faunas and most comprehensive data on species occurrences. A methodological focus of this paper is on controlling sampling biases that confound biological and ecological signals. Such biases include uneven sampling through time, differential preservation of larger animals and more durable skeletal elements, errors in age-dating imposed by uncertainties in correlation and paleomagnetic timescale calibrations, and uneven taxonomic treatment across groups. We attempt to control for them primarily by using a relative-abundance model to estimate limits for the first and last appearances from the occurrence data. This model also incorporates uncertainties in age estimates. Because of sampling limitations inherent in the terrestrial fossil record, our 100-Kyr temporal resolution may approach the finest possible level of resolution for studies of vertebrate faunal changes over periods of millions of years. Approximately 40,000 specimens from surface and screenwash collections made at 555 localities form the basis of our study. Sixty percent of the localities have maximum and minimum age estimates differing by 100 Kyr or less, 82% by 200 Kyr or less. The fossils represent 115 mammalian species or lineages of ten orders: Insectivora, Scandentia, Primates, Tubulidentata, Proboscidea, Pholidota, Lagomorpha, Perissodactyla, Artiodactyla, and Rodentia. Important taxa omitted from this study include Carnivora, Elephantoidea, and Rhinocerotidae. Because different collecting methods were used for large and small species, they are treated separately in analyses. Small species include insectivores, tree shrews, rodents, lagomorphs, and small primates. They generally weigh less than 5 kg. The sediments of the study interval were deposited by coexisting fluvial systems, with the larger emergent Nagri system being displaced between 10.1 and 9.0 Ma by an interfan Dhok Pathan system. In comparison to Nagri floodplains, Dhok Pathan floodplains were less well drained, with smaller rivers having more seasonally variable flow and more frequent avulsions. Paleosol sequences indicate reorganization of topography and drainage accompanying a transition to a more seasonal climate. A few paleosols may have formed under waterlogged, grassy woodlands, but most formed under drier conditions and more closed vegetation. The oxygen isotopic record also indicates significant change in the patterns of precipitation beginning at 9.2 Ma, in what may have been a shift to a drier and more seasonal climate. The carbon isotope record demonstrates that after 8.1 Ma significant amounts of C4 grasses began to appear and that by 6.8 Ma floodplain habitats included extensive C4 grasslands. Plant communities with predominantly C3 plants were greatly diminished after 7.0 Ma, and those with predominantly C4 plants, which would have been open woodlands or grassy woodlands, appeared as early as 7.4 Ma. Inferred first and last appearances show a constant, low level of faunal turnover throughout the interval 10.7–5.7-Ma, with three short periods of elevated turnover at 10.3, 7.8, and 7.3–7.0 Ma. The three pulses account for nearly 44% of all turnover. Throughout the late Miocene, species richness declined steadily, and diversity and richness indices together with data on body size imply that community ecological structure changed abruptly just after 10 Ma, and then again at 7.8 Ma. Between 10 and 7.8 Ma the large-mammal assemblages were strongly dominated by equids, with more balanced faunas before and after. The pattern of appearance and disappearance is selective with respect to inferred habits of the animals. Species appearing after 9.0 Ma are grazers or typical of more open habitats, whereas many species that disappear can be linked to more closed vegetation. We presume exceptions to this pattern were animals of the mixed C3/C4 communities or the wetter parts of the floodplain that did not persist into the latest Miocene. The pace of extinction accelerates once there is C4 vegetation on the floodplain. The 10.3 Ma event primarily comprises disappearance of taxa that were both common and of long duration. The event does not correlate to any obvious local environmental or climatic event, and the pattern of species disappearance and appearance suggests that biotic interactions may have been more important than environmental change. The 7.8 Ma event is characterized solely by appearances, and that at 7.3 Ma by a combination of appearances and disappearances. These two latest Miocene events include more taxa that were shorter ranging and less common, a difference of mode that developed between approximately 9.0 and 8.5 Ma when many short-ranging and rare species began to make appearances. Both events also show a close temporal correlation to changes in floodplain deposition and vegetation. The 7.8 Ma event follows the widespread appearance of C4 vegetation and is coincident with the shift from equid-dominated to more evenly balanced large-mammal assemblages. The 7.3 to 7.0 Ma event starts with the first occurrence of C4-dominated floras and ends with the last occurrence of C3-dominated vegetation. Absence of a consistent relationship between depositional facies and the composition of faunal assemblages leads us to reject fluvial system dynamics as a major cause of faunal change. The close correlation of latest Miocene species turnover and ecological change to expansion of C4 plants on the floodplain, in association with oxygen isotopic and sedimentological evidence for increasingly drier and more seasonal climates, causes us to favor explanations based on climatic change for both latest Miocene pulses. The Siwalik record supports neither “coordinated stasis” nor “turnover pulse” evolutionary models. The brief, irregularly spaced pulses of high turnover are characteristic of both the stasis and pulse models, but the high level of background turnover that eliminates 65–70% of the initial species shows there is no stasis in the Siwalik record. In addition, the steadily declining species richness and abrupt, uncoordinated changes in diversity do not fit either model.
High-performance liquid chromatography (HPLC) has proved extremely versatile over the past 25 yr for the isolation and punfication of peptides varying widely in their sources, quantity and complexity. This article covers the major modes of HPLC utilized for peptides (size-exclusion, ion-exchange, and reversed-phase), as well as demonstrating the potential of a novel mixed-mode hydrophilic interaction/cation-exchange approach developed in this laboratory. In addition to the value of these HPLC modes for peptide separations, the value of various HPLC techniques for structural characterization of peptides and proteins will be addressed, e.g., assessment of oligomerization state of peptideslproteins by sizeexclusion chromatography and monitoring the hydrophilicitykydrophobicity of amphipathic cr-helical peptides, a vital precursor Tor the development of novel antimicrobial peptides. The value of capillary electrophoresis for peptide separations is also demonstrated. Preparative reversed-phase chromatography purification protocols for sample loads of up to 200 mg on analytical columns and instrumentation are introduced for both peptides and recombinant proteins. Key Words: Peptides; proteins; size-exclusion chromatography (SEC); anion-exchange chromatography (AEX); cation-exchange chromatography (CEX); mixed-mode hydrophilic interaction chromatography (HIL1C)/cation-exchange chromatography (CEX); reversed-phase high-performance liquid chromatography (RP-HPLC); preparative RP-HPLC of peptides and proteins; amino acid side-chain hydrophilicitylhydrophobicity coefficients; amino acid U-helical propensity values; amino acid side-chain stability coefficients
This is the most comprehensive analysis of higher-level relationships in Odonata conducted thus far. The analysis was based on a detailed study of the skeletal morphology and wing venation of adults, complemented with a few larval characters, resulting in 122 phylogenetically informative characters. Eighty-five genera from forty-five currently recognized families and subfamilies were examined. In most cases, several species were chosen to serve as exemplars for a given genus. The seven fossil outgroup taxa included were exemplar genera from five successively more distant odonatoid orders and suborders: Tarsophlebiidae (the closest sister group of Odonata, previously placed as a family within "Anisozygoptera"), Archizygoptera, Protanisoptera, Protodonata and Geroptera. Parsimony analysis of the data, in which characters were treated both under equal weights and implied weighting, produced cladograms that were highly congruent, and in spite of considerable homoplasy in the odonate data, many groupings in the most parsimonious cladograms were well supported in all analyses, as indicated by Bremer support. The analyses supported the monophyly of both Anisoptera and Zygoptera, contrary to the well known hypothesis of zygopteran paraphyly. Within Zygoptera, two large sister clades were indicated, one comprised of the classical (Selysian) Calopterygoidea, except that Amphipterygidae, which have traditionally been placed as a calopterygoid family, nested within the other large zygopteran clade comprised of Fraser´s "Lestinoidea" plus "Coenagrionoidea" (both of which were shown to be paraphyletic as currently defined). Philoganga alone appeared as the sister group to the rest of the Zygoptera in unweighted cladograms, whereas Philoganga + Diphlebia comprised the sister group to the remaining Zygoptera in all weighted cladograms. "Anisozygoptera" was confirmed as a paraphyletic assemblage that forms a "grade" towards the true Anisoptera, with Epiophlebia as the most basal taxon. Within Anisoptera, Petaluridae appeared as the sister group to other dragonflies.
The larvae of Orthocladiinae (Diptera: Chironomidae) of the Holarctic region : keys and diagnoses
(1983)
The paper deals with the biology, morphology and anatomy of seven species of syrphid larvae viz. Syrphus luniger Meig., S. balteatus De Greer, S. ribesii Linne, Catabomba pyrastri Linne, Sphaerophoriae flavicauda Zett., Sph. scripta Linne, and Platychirus scutatus Meig. The habitat, mode of progression, aphidophagous habits and characteristic coloration are described for each species. It is shown that the larvae of aIl the above species, like larvae of other cyclorrhaphous Diptera, definitely pass through three stages separated by two moults. The mode of dehiscence of the puparium is described briefly. Each of the species, except Catabomba pyrustri, has three generations in the breeding season which lasts from May to October. Platychirus scutatus hibernates only in the larval stage, but the other species may be found in both the larval and pupal stages during the winter. The larvae of all the above species, except syrplzus balteatus, are commonly parasitized by ichneumonid larvae. The morphology of the egg, the three larval stages and the puparium of S. luniger is described in detail. The characters common to the third stage larvae of all the species deaIt with are summarized and short descriptions of the third stagelarvae andpuparia of the individual species are given. The general appearance of the living larvae and details of the buccopharyngeal armature, spiracles and puparia of each of the species is represented in figures. In connexion with the pupae a number of new structures are described arid it is suggested that some of them are concerned with the formation of the characteristic shape of the puparium and with the dehiscence of the puparium. Internal pupal spiracles are present in all the species dealt; with, but external pupal spiracles are present only in Platychirus scutatus. The anatomy of P. scutatus is described and figured, an account being given of all the structures except the musculature of the body wall. Study of the anatomy affords evidence as to the carnivorons mode of Iife of the larvae and also indicates that tho larvae have evolved from aquatic forms. The comparative morphology of the Syrphinae is discussed with respect to the relationship of the Syrphinae to other Aschiza aiid to the cyclorrhaphous Diptera.
This paper is a monographic revision of tlie Holarctic genus Hilarimorpha Schiner. Twenty-seven species are recognized, twenty-two of which are new: Hilarimorpha abuta, bumulla, californica, clavata, cunata, desta, kena, lamara, Iantha, loisae, mandana, mentata, modesta, parva, pitans, punata, reparta, robertsoni, sidora, stena, tampa, and varda. Two described species from Asia, Hilarimorpha maculata and orientalis, are removed from the genus. In addition to a taxonomic revision of the genus, this study treats geographical distribution of the species, and the relationship of the genus to othe families of brachycerous Diptera.
1. The root tip of Cucurbita maxima possesses a single histogen from which all the primary root tissues arise. 2. The primary root is exarch, tetrarch. Differentiation of the large central metaxylem vessels is retarded; pith is not present. 3. The primordium of a secondary root is formed from the cortex, including the endodermis, as well as the pericycle of the primary root. 4. The transition extends from approximately 1 cm. below the peg to just above it. At the lowest level pith differentiates in the center and the metaxylem takes a peripheral position just within the phloem. Each primary xylem strand diverges into two arms extending laterally and joining the metaxylem. These arms separate, resulting in a siphonostele of four tangential transition bundles. These divide into two parts each, forming a total of eight bundles which become endarch. 5. Of these eight bundles usually two pairs anastomose, then divide into three, producing a total of ten bundles which continue through the hypocotyl. Additional bundles may arise. 6. The bundle is considered bicollateral on the basis of ontogeny; it shows a differentiation of internal phloem from the procambial tissue at the same time that the external metaphloem differentiates. (The study of a single species allows no interpretation on the basis of phylogeny.) 7. A suggestion is made concerning the differentiation of two types of phloem, the one called fascicular phloem and the other called connective phloem. Differences in origin, structure, and distribution of the two types are described. 8. In the cotyledonary node tangential anastomoses produce a cotyledonary plate of four parts. Continuations from these form two traces to each cotyledon. Before the cotyledon diverges completely, each trace branches laterally to form a basal vein from which arise four or more bundles which are the principal veins in the blade of the cotyledon. 9. The bundles of the epicotyl differentiate against the parts of the cotyledonary plate. The epicotyl is retarded in its development except for the median trace to the first foliage leaf. The early differentiation of this trace may account for the characteristic short first internode.
Plastid behavior in reciprocally different crosses between two races of Medicago truncatula Gaertn.
(1962)
During my mork on the inheritance of symmetry characters in Medicago (1956), chance played into my hands a case of fairIy pronounced reciprocal differentes in the behavior of plastids in a cross between two local races of Medicago truncatula GAERTN. which so far I know are not given even varietal rank. The facility in producing the hybrids encouraged me to investigate the material, and the results are reported in this paper.
Introductory chapters on the geography, vegetation and history of botanical ex loration are followed by a catalogue of 331 species of wild vascular plants, 90% of which represent first records for the island. Synonymy, references, localities and ecological data are given for each species in a condensed form. The taxonomy, nomenclature and distribution of some taxa are discussed; in one case (Silene cythnia) a drawing and a distribution map are supplied. Nomenclatural novelties are validated in the genera Centaurea, Matricana, Melica (by W. Hempel) and Trifolium. A phytogeographical and ecological analysis of the flora demonstrates its striking banality and the unexpectedly high proportion of anthropophytes. No pliytogeographical link with tlie other E. Aegean Isiands and Anatolia exists, but there are some affinities with the Cyclades. The observations are consistent with the hypotliesis of a long insular isolation leading to a strong depletion or even destruction of the original flora, which has been replaced by long-distance dispersed and anthropophytic elements.
A world revision of the four entedonine (Hymenoptera: Eulophidae: Entedoninae) genera of larval parasitoids of thrips (Thysanoptera) is presented: Ceranisus Walker, 1841, Entedonomphale Girault, 1915 stat. rev. (reinstated as a valid taxon from previous synonymy under Ceranisus, with type species E. margiscutum Girault, 1915 stat. rev.), Goetheana Girault, 1920, and Thripobius Ferrière, 1938. The following new generic synonymies are proposed: Cryptomphale Girault, 1917, Entedonastichus Girault, 1920, Pirenoidea Girault, 1922, and Thripoctenoides Erdös, 1954 under Entedonomphale. The proposed new combinations are as follows: Entedonomphale bicolorata (Ishii, 1933), E. nubilipennis (Williams, 1916), and Thripobius javae (Girault, 1917) from Ceranisus; Entedonomphale carbonaria (Erdös, 1954), E. dei (Girault, 1922), E. kaulbarsi (Yoshimoto, 1981), and E. mira (Girault, 1920) from Entedonastichus. New synonymies are proposed for the following species: Ceranisus vinctus (Gahan, 1932) under Ceranisus menes (Walker, 1839), Diglyphus aculeo Walker, 1848 under Ceranisus pacuvius (Walker, 1838); Ceranisus maculatus (Waterston, 1930) and Thripobius semiluteus Boucek, 1976 under Thripobius javae (Girault, 1917); Entedonastichus albicoxis (Szelényi, 1982) under Entedonomphale carbonaria (Erdös, 1954), and Entedonastichus gaussi (Ferrière, 1958) under Entedonomphale bicolorata (Ishii, 1933). Eleven new species are described: Ceranisus barsoomensis and C. votetoda (Australia), C. udnamtak (Nepal); Entedonomphale boccaccioi (USA), E. esenini (Madagascar), E. lermontovi (South Africa), E. quasimodo and E. zakavyka (Australia); Goetheana pushkini (Japan and Republic of Korea) and G. rabelaisi (Australia); and Thripobius melikai (China). Three species are excluded from Ceranisus: C. ancylae (Girault, 1917) (mistakenly listed in Ceranisus) as well as C. nigricornis Motschulsky, 1863 and C. semitestaceus Motschulsky, 1863, both taxa incertae sedis. New data are provided on the distribution and host associations of many of the species included in this review.
Neogastropods are usualiy accepted as the most advanccd prosobranchs, though their organization is approached in several respects in some higher families of Mesogastropoda. This seems, however, to be due to parallel evolution and the neogastropods originated from a much lower grade of mesogastropod. Although some workers derive them from an archaeogastropod stock there are too many features in their anatomy characteristic of mesogastropods rather than of archaeogastropods for this to bc acceptable. On the whofe, neogastropods are a rather uniform group of prosobranchs in their shell, external features, and internal anatomy. In only one System do they show, by comprison with archaeo- and mesogastropods, both extreme specialization and considerable variation: this is the gut, which is in several ways unlike that of any other prosobranch. This is to be associated with their carnivorous way of life, in which respect they again differ markedly from meso- and archaeogastropods. Taylor, Morris Br Taylor (1980) have shown how neogastropod species differ amongst themselves not, primarily, in their rnode of life, but in their often narrow choice of prey. Since the anatomical requirements for predation are more or less constant, the different species remain similar in organization and are often sympatric. In these respects neogastropods differ markedly from mesogastropods, whose adaptive radiation has been extensive and primarily in relation to mode of life. Separation of neogastropods from mesogastropods rests mainly on the siphonal canal in the shell, the siphon on the mantle edge, the rachiglossate or toxoglossate radula, and the presence of a pleurembolic proboscis or one of its varieties (Smith, 1967). The osphradium is large and its axis carries a double series of lamellae, giving it a gill-like appearance. Males always have a penis and females usually a ventral pedal gland. lnternally the anterior part of the alimentary caiial has becorne elaborate, with a complex glandular equipment, and the wall of the kidney is more folded than in mesogastropods. The nervous systern is concentrated, though the visceral ganglia remain posteriorly placed. Eggs are laid in capsules attached to the substratum. A free larval stage is often suppressed and food eggs are common, but neither of these features has much taxonomic significance, occurring apparently randomly throughout the group. Because of their general similarity classification of the Neogastropoda has proved to be no easy task, and there is still no universally-accepted subdivision of the order into superfamilies. It is generally agreed, however, that the order may be split into two groups, primarily on the basis of radular structure. The more primitive of these, the Rachiglossa, has a radula with typically 3 teeth per row; the more advanced, the Toxoglossa, has a radula which, in more primitive genera, resembles the rachiglossate, but which Comes, in more advanced toxoglossans, to have only a single tooth in action at a time. Each tooth has then become scroll-like and is used for the injection of poison from a poison gland into the prey (Shimek & Kohn, 1981). The group Toxoglossa is agreed to contain the superfamily Conacea which includes (as Recent forms) the families Turridae, Conidae, and Terebridae, all with poison apparatus, though with very different shells. Risbec (1955), followed by Taylor & Sohl (1962), has added a second superfamily Mitracea containing, in the family Mitridae, a grouping of genera selected from that family as earlier understood. These have a rachiglossate radula and an apparent poison gland not irnrnediately comparable with that of undoubted toxoglossans. This reclassification of mitrids has not found favour with subsequent workers (Cernohorsky, 1966, 1970; Ponder, 1972). Ponder (1973) made a case for adding a third suborder to the two mentioncd above. This was to contain the single superfamily Cancellariacea with the one family Cancellariidae. The case rests on the unique character of their radula. It is, however, when one turns to the remaining rachiglossan families and- attempts to assign them to superfamilies that difficulties mount. Three groupings Iiave been conventionally recognized - Muricacea, Buccinacea, and Volutacea, though it has often appeared that the last was a collection of animals not obviously assignable to the other two rather than clearly related amongst thernselves. Ponder (1973) came to the somewhat pessimistic conclusion that all rachiglossans should be put into a single taxon, for which he used the name Muricacea. It seems to us, however, that certainly within the limited group of anirnals with which we have to deal here, but even in a broader context, there is still some validity - and certainly convenience - in the older Separation, when due importance is given to internal anatomy; we propose, therefore, to retain the three superfamilies in dealing with a group which is otherwise too large for easy treatment. We adopt this arrangement the more readily as we have no volutacean mernbers of the fauna with which we have to deal, provided that we accept Ponder's proposal to create a separate superfamily for cancellariids. This allows the remaining superfamilies to be split into Muricacea and Buccinacea, and it is between these two superfamilies that lines of division may most obviously be drawn. Taylor & Sohl (1962) noted about 800 genera and subgenera in the rachiglossan group. The Buccinacea, with nearly 400, is rivalled for size only by the superfamilies Rissoacea and Cerithiacea amongst all the prosobranchs. A difficulty arises at this point in relation to the number of species which have been described. Many neogastropods are not intertidal in occurrence. Their capture is dependent upon dredging, a method which can often do no more than sample a few isolated spots on the ocean bed. Many species have been described on the basis of these samples without any real knowledge of the variation whjch may affect populations. It seems, indeed, probable that many of these are no more than local varieties, especially when it is remembered that the anatomy of many is very imperfectly known. We have, therefore, been conservative in nomenclature and tended to use broad generic groupings where others might have used narrower ones. The latter may be right, but it is prernature to be sure of this.
The cirripeds sampled by the N. O. Jean Charcot from the Azores region include thirty-four species: twenty lepadomorphs, eight verrucomorphs and six balanomorphs. Among these are two new species: Arcoscalpellum eponkos n.sp. and Tesseropora arnoldi n.sp. and several little known species. The family Verrucidae is revised, and a key to the genera is included. Verruca and Metaverruca are rediagnosed, two new genera are proposed: Newmaniuerruca n.g. and Costatoverruca n.g. A list of recent species of Verrucidae is provided, reported with keys to all of the species. Forty-five species of cirripeds are reported from the Azores region, of which one third are endemic.
Linnaeus as an evolutionist
(1909)