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The former and current distribution of the quokka, Setortix brachyurus, was mapped from published and all available unpublished records. At the time of European settlement the quokka was widespread and abundant and its distribution encompassed an area of approximatelyThe former and current distribution of the quokka, Setortix brachyurus, was mapped from published and all available unpublished records. At the time of European settlement the quokka was widespread and abundant and its distribution encompassed an area of approximately 41 200 km2 of south-west Western Australia inclusive of two offshore islands, Bald Island and Rottnest Island. Historical reports indicated an extensive population decline occurred in the 1930s. The decline continued, with a previously undocumented decline apparent in the period from 1980 to 1992. However, this decline may be an artefact of the time scales used for mapping and may well equate with a previously reported decline lor a suite of south -west mammals in the 1970s. By 1992 the quokka´s distribution had been reduced to an area of approximately 17800 km2. An increased awareness of the presence of the quokka on the mainland has resulted in numerous reportings of quokka presence since 1992, has confimled the existence of several populations at the northern extent of the quokka´´s known geographic range and indicated the cmrent, 2005, distribution to be similar to that in 1992. However, survey and population estimates at six of these mainland locations from the northem jarrah forest indicated low abundance. There have been no population estimates elsewhere on the mainland. Two populations have been reported tiom the Swan Coastal Plain, but neither has been confirmed extant. Predation by the introduced fox, Vulpes vulpes, is implicated as a major cause of the quokka´s initial decline, while ongoing predation, habitat destruction and modification through altered tire regimes have contributed to the continued decline. Specific conservation management actions are recommended, namely: (i) Implementing an active adaptive management program in the northern jarrah forest to determine quokka population response to habitat manipulation through the use of fIre, fox baiting and pig control; (ii) Surveying the Stirling fumge and Green Range populations with emphasis placed on determining population size and population genetic structure; (iii) Surveying the reported occurrences from the Swan Coastal Plain, with emphasis on unambiguously determining presence. If confirmed, priority should he directed to assessing population size and determining the management requirements to ensure persistence of the population; (iv) Surveying southem forest and south coast populations to assess quokka population size, the extent of movement between sllbpopulations and assessment of the range of habitat types used by quokkas. The latter should be combined with spatial analyses of known extant populations and suitable and potentially suitable habitat; (v) Determining the role of tire in establishing and maintaining preferred habitat of southern forest and south coast populations; and (vi) Establishing a program to assess the potential effects from management operations.
Total body water increases in pregnancy and while the uterus, placenta, fetus, and amniotic fluid constitute part of this increase, the largest component is in the extracellular water. Fat stores also increase and thus the distribution volumes of all drugs expand, but the major effect is seen in polar drugs which are confined to the extracellular space. Cardiac output and renal function also increase and elimination of polar drugs is acelerated. In contrast, the elimination of lipophilic drugs may be retarded, and the effect on intermediate drugs is variable. Polar drugs cross the placenta slowly and accumulate in amniotic fluid and therefore in the fetal gut lumen. Lipophilic drugs cross the placenta rapidly and their transplacental distribution is dependent on relative maternal and fetal affinity: this is determined largely by protein binding on either side of the placenta. The. fetus and neonate dispose of all drugs less rapidly than adults, the most efficient elimination processes being sulphate conjugation and renal excretion.
A skeletal world revision of the genus is presented to accompany a family account for Flora Malesiana. 82 species are recognised, of which 74 occur in the Malesiana region. Six species are desctibed as new, one species is raised from infraspecific status, and five species are restored from synonymy. Many names are typified for the first time. Three widespread, or locally abundant hybrids are also included. Full descriptions are given for new (6) or recircumscribed (7) species, and emended descriptions of species arc given where necessary (9). Critical notes are given for all the species. Little known and excluded species are discussed. An index to all published species names and an index of exsiccatae is given.
Die vorliegende Arbeit soll einen Beitrag zur Biologie der Honigbiene darstellen. Sie ist zunächst eine biologisch-deskriptive Arbeit. Ich habe die Biene bei ihrer mannigfachen Tätigkeit in freier Natur wie auch in ihrem Stocke beobachtet und habe festzustellen versucht, wie sie sich verhält, wenn ihr Körper mit irgendeinem Schmutzstoff in Berührung kommt. ...
Through the kind assistance of O. G. Lloyd of Cincinnati, Ohio, most of the Australian polypores in our possession have been accurately identified. In the present paper we record our various collections. In doing so, we make use of the excellent keys employed by Lloyd in the following works: "Synopsis of the Genus Hexagona" (Ohio, 1910), "Synopsis of the Stipitate PoIyporoids" (Ohio, 1912), "Synopsis of the Section Apus of the Genus Polyporus" (Ohio, 1915) and "Synopsis of the Genus Fomes" (Ohio, 1915). In addition to recording the plants we have handled, we have included as well all the Australian species embraced in these works. Australian mycologists should thus have available a workable scheme for the identification of most of our firmer polypores. Those who have attempted to work out the species from Cooke´s "Handbook of Australian Fungi", will appreciate the value of Lloyd´s work. We deal first with the Stipitate Polypores, then with Fomes, Polyporus (Apus) and Hexagona.
This synonymic list of the flat bugs (Aradidae) ofthe world enumerates 1,798 species in 211 genera. Names of eight fossil species are given in their original combination in modern genera. The list is introduced by brief discussions of habits, food, ecology and distribution. Many taxonomic innovations are included, as follows: Subfamily Chinamyersiinae is divided into two new tribes, Chinamyersiini and Tretocorini; the subfamily Prosympiestinae is divided into two new tribes, Llaimacorini and Prosympiestini. All currently recognized subgenera are raised to generic rank: Aneurillus, Breviscutaneurus, lralunelus, and Paraneurus from Aneurus; Miraradus and Quilnus from Aradus; Lissaptera and Nesiaptera from Acaraptera; Neoproxius and Nesoproxius from Proxius (see list below for new combinations resulting). Three genus-group names are raised from synonymy: Aneurosoma; Burgeonia and Brachyrhynchus. One genus-group name is reduced to synonymy; Zimera as a junior synonym of Brachyrhynchus. The following new species-genus combinations are made, these mostly resulting from elevation of subgenera to generic status or species transfers. In Aneurillus - borneensis, cetratus, cheesmanae, consimilis, doesbergi, foliaceus, glaberrimus, gracilis, jacobsoni, longicollis, papuasicus, pumilus, superbus; in Aneurosoma - dissimile; in Aneurus - septentrionalis; in Aradus - dignatus; in Arbanatus - asiaticus, loriae; in Brachyrhynchus - affinis, amplicollis, andamanensis, angolensis, armigerus, australis, bergrothi, bergrothianus, bhoutanensis, breuiceps, burmensis, confectus, confusus, consimilis, crenatus, dentipes, discrepans, dispar, duboisi, elegans, exarmatus, funebrus, furcatulus, furcatus, germari, gracilicornis, granos us, hospidus, hoberlandti, horridus, hsiaoi, incisus, incognitus, insignis, intermedius, javanensis, kachenensis, kerzhneri, lindemannae, longicornis, longirostris, luberoensis, luzonicus, machadoi, madagascariensis, mauricii, membranaceus, micronesicus, monedulus, mario, ouerlaeti, parallelus, pauper, philippinensis, piliferus, poriaicolus, projectus, quadridentatus, quadrispinosus, rossi, rugosus, scrupulosus, serratus, similis, solomonensis, spinipes, stolidus, subinermis, subtriangulus, sulcatus, sulcicornis, sumatrensis, taiwanicus, teter, thailandicus, triangulus, tristis, urijdaghi; in Breviscutaneurus - breviscutatus, helenae, madagascariensis, medioscutatus; in Burgeonia - burgeon, dilatatus, froidebisei, intermedius, kormileui, madagascariensis, maynei, paruus, schoutedeni, usingeri; in Chiastoplonia - pusio; in lralunellus - aibonitensis, bergi, bispinosus, boliuianus, carioca, costariquensis, flavomaculatus, ftitzi, gallicus, leptocerus, longicornis, marginalis, monrosi, plaumanni, politus, sahlbergi, simulans, subdipterous, tenuis, westwoodi, wygodzinsky; in Miraradus - foliaceus, himalayensis, mirabilis, oeruendetes; in Neoproxius - amazonicus, carioca, costariquensis, gypsatus, incaicus, lindemannae, magdalenae, nicaraguensis, palliatus, panamensis, personatus, peruuianus, schwarzii; in Nesiaptera - denticulata, gibbosa, ouata, rotundata, tuberculata, zimmermani; in Nesoproxius - angulatus, constrictus, gracilis, hexagonalis, malayensis, minutus, punctulatus, vietnamensis, yoshimotoi; in Neuroctenus - ghesqueri; in Oreossa - insignis; in Quilnus - amurensis, breuirostris, discedens, heidemanni, niger, nigrinus, oregonicus, paruicollis, subsimilis, usingeri. Three new species names are proposed: Brachyrhynchus pauper for the preoccupied Mezira modesta Kormilev, 1972; Mezira uicina for the preoccupied Mezira proxima Kormilev, 1982; and Mezira doesburgi for the preoccupied Mezira surinamensis Kormilev, 1974. Five new species-synonymys are made: Aradus centriguttatus as a junior synonym of Aradus similis; Mezira jacobsoni as a junior synonym of Daulocoris cornigerus; Mezira modesta as a junior synonym of Brachyrhynchus membranaceus; Neuroctenus breuicornis as a junior synonym of Neuroctenus ater; Notoplocaptera malaisei as a junior synonym of Zoroaptera malaisei. Four new emendations of gender endings are proposed for the species name "halaszfyi": Artabanus halaszfyae, Chelysosoma halaszfyae, Ctenoneurus halaszfyae, Mezira halaszfyae.
Da die gesamte Arbeit nur einen vorläufigen Überblick über das bearbeitete Gebiet gibt, können nur wenige Punkte hier herausgegriffen werden. Die Artendichte ist in der Kieler Bucht in der Vegetationszone (= Phytal) am größten, es folgt die Sandregion, am geringsten ist sie in der Schlammzone. Die Tiere des Phytals, der Sandregion und der Schlammregion zeigen in ihrer Organisation wesentliche Unterschiede. Im Sand ist die Mikrofauna stark, die Makrofauna gering entwickelt, in der Schlammregion umgekehrt. Die Verteilung der sessilen, der hemisessilen und der haptischen Tiere mit ihren Haftorganen auf die drei Hauptbiotope wird untersucht. Die Sandregion ist durch Fehlen der sessilen Tiere, Armut an hemisessilen, aber großer Reichtum an haptischen Tieren ausgezeichnet. Die haptischen Tiere des Sandes besitzen besonders Haftröhrchen, Haftpapillen und Haftringe als Haftorgane und diese in großer Zahl und weit über den Körper verteilt. Im Phytal erreichen die sessilen Tiere ihre maximale Arten- und Individuenzahl, in der Schlammregion dominieren die hemisessilen Arten. Die Lokomotion durch Wimperbewegung ist in der Sandregion am reichsten entwickelt (Kriechen auf Wimpern), wird im Phytal geringer und tritt in der Schlammregion ganz zurück. Eine Übersicht über die Ernährungstypen ergibt, daß im groben Sand die Diatomeenflora der Sandoberfläche als wichtigste Nahrungsquelle der Mikrofauna zu betrachten ist. Im Phytal existieren drei Nahrungswege: 1. Ein Weg von den Partikeln des freien Wassers über Mikrophagen zu einer Mikrofauna und Makrofauna ohne Einschaltung der Nährstoffe der Pflanzen des Phytals. Diesem Weg gehören im gesamten Phytal über ein Drittel der Arten an, im Extremfalle (tiefe Fucusregion) weitaus die Mehrzahl. 2. Ein Weg von der epiphytischen Mikroflora zu einer Mikro- und Makrofauna. 3. Ein Weg von den Teilen der Großpflanzen (Laminaria, Fucus, Zostera, Delesseria) zu einer Mikrofauna und Makrofauna. Diesem letzten Nahrungsweg gehören auffallend wenige Tierarten an, relativ am größten ist der Anteil in der Seegras- und der Ulvaregion. Eine Gliederung in Biozoenosen mit besonderer Berücksichtigung der Mikrofauna ergibt für das Benthal, 6 Unterbiozoenosen, 4 davon (die Halammohydra-Biozoenose, die Turbanella-hyalina-B., die Arenicola-B. und die Otoplanen-B.) gehören der Sandregion, 2 (Corbula-B. und Laophonte-horrida-B.) gehören der Schlammregion an. Das Phytal zeigt trotz der starken Biotopunterschiede nur geringe qualitative Unterschiede seiner Fauna, jedoch starke Verschiedenheiten in der Artenzahl, die wohl in erster Linie auf den verschiedenen durchschnittlichen Salzgehalt der Biotope zurückzuführen sind. Die maximale Besiedelungsdichte zeigt die tiefe Fucusregion.
The A. A. present in this paper their studies about the Aspergillus spp. found by them as contaminants of Lab. cultures, chiefly. The species studied are the following: A. allocotus n. sp., A. amstelodami, A. awamori varo hominis n. var., A. candidus, A. fischeri, A. flavus, A. heteromorphus n. sp., A. japonicus, A. niger (two strains), A. ochraceus, A. ochraceo-petaliformis n. sp., A. quadrilineatus, A. repens var. ramos a n. var. A. sclerotiorutn, A. sydowii, A. terreus, A. unguis and A. variecolor var. major n. var.
Sobre Bryozoa do Brasil
(1941)
The specimens which form the basis of the following notes and descriptions were received by the writer from Mr. Ch'i Ho, Asistant Entomologist of Fan Memorial Institute of Biology, who collected thern either in Peiping or Eastern Tomb (40.2 N, 117.0 E), Hopei Province. They belong to nineteen species and are included in fifteen genera. Two of the species are believed to be new to science.
A cladistic analysis is presented of the hawkmoths of the tribe Acherontiini, Morgan´s Sphinx (Xanthopan morganii (Walker», and related genera. The study aims to test the monophyly of tribe Acherontiini; the hypothesis that all taxa with extremely long probosces (some Acherontiini, Meganoton rubescens, Neococytius, Xanthopan) form a monophyletic group, or at least fall within a single reasonably compact clade; and, within this group, to determine whether Xanthopan is more closely related to Acherontiini or to COCytillS and Neococytius. The data set comprises 109 characters derived from adult and immature stage morphology, biology and behaviour. These data were analysed using equal weighting, successive approximations character weighting (SACW) and implied weighting. All weighting schemes agreed on the monophyly of Acherontiini and of a group of genera comprising Amphimoea, Cocytius and Neococytius (the Cocytius group). Several other generic and suprageneric clades were also consistently recovered. However, those hawkmoths with extremely long probosces were never recovered as a monophyletic group. The relationships of Xanthopan were also ambiguous. Equal weighting and SACW placedXanthopan + Meganoton rztbescens (Butler) as sister to the COCytills group, while implied weighting placed Xanthopan as sister to Acherontiini. This latter relationship is based primarily on shared possession of a pilifer/palp hearing organ. Further analyses suggested the two components of this organ were not biologically independent. Downweighting this feature accordingly resulted in all weighting schemes converging on the topology found by equal weighting. Exclusion of the incomplete subset of immature stage data had no effect under implied weighting but equal weighting and SACW now recovered a Neotropical clade comprising Manduca. and the Cocytius group, while Xanthopan was placed with M. rubescens and Panogena. Downweighting the pilifer/palp hearing organ under implied weighting again caused convergence with the equal weighting/SACW results. Thus, the relationships of Xanthopan remain equivocal and further data, particularly from the immature stages, will be required to elucidate its phylogenetic position further.
Geschlechts- und Gattungsunterschiede an Metapodien und Phalangen mitteleuropäischer Wildwiederkäuer
(1968)
Zur Beurteilung der Geschechtsunterschiede und zur Bestimmung der Gattungsunterschiede wurden die Metapodien und Phalangen von im ganzen 258 Exemplaren von Cervus elaphus hippelaphus Erxleben, 1771, Dama dama dama (Linne, 1758), Capreolus capreolus capreolus (Linne, 1758), Rupicapra rupicapra rupicapra (Linne, 1758) und Capra ibex ibex Linne, 1758, ausgewertet. 93 Tiere entfielen auf Capreolus capreolus, von denen aber zur Geschlechtsunterscheidung nur 78 Tiere verwendbar waren; die restlichen 15 Tiere waren ohne Geschlechtsangabe und konnten auch nachträglich nicht bestimmt werden. Weiterhin kamen zur Untersuchung 56 Tiere von Cervus elaphus, 22 von Dama dama, 49 von Rupicapra rupicapra und 38 von Capra ibex (5. Tab. 1).
Was die Geschlechtsunterscheidung betrifft, so gilt mit Ausnahme von Capreolus capreolus die Regel, daß die Metapodien und Phalangen der Weibchen alles in allem länger und stärker sind als die der Männchen. Zur Bestimmung erwies sich die Länge des jeweiligen Knochens - an der Phalanx 3 die diagonale Sohlenlänge - als am besten geeignet. Dabei ließen sich Gesmlechtsunterschiede nicht nur in den Mittelwerten aufzeigen, sondern auch zum Teil in absolut größeren Maßen, wie das bei Dama in der Länge und bei Caprn ibex in der Breite der Fall war (s. Tab. 2-7).
Für die Unterscheidung zwischen den Gattungen waren in erster Linie Gestaltunterschiede von Bedeutung, in zweiter Linie die absoluten Maße und Indices, wovon letztere für sich allein oft schon Gattungsbestimmungen zulassen. Die Unterscheidung der hier behandelten Arten ist nahezu immer möglich, wenn man davon absieht, daß unter Siedlungsabfällen kleine, uncharakteristische Fragmente sein können. Schwierigkeiten können entstehen bei der Unterscheidung von Steinbock- sowie manchen Gemsenknochen von solchen der Gattungen Capra hircus und Ovis ades; auf sie wurde in dieser Arbeit nicht näher eingegangen.
Keys to the hairs of 44 species of southern African Cricetidae and Muridae have been devised for the identification of these species. The keys are based primarily on the cuticular scale patterns and groove characters. Distribution data and descriptions of the hairs are presented with micrographs to assist in identification.
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.
1. Die Feldbeobachtungen der vorliegenden Untersuchung sind in der Zeit vom 10. VII. bis 9. VIII. 1964 in Westspitzbergen in den Gebieten von Isfjorden und Hornsund (Abb. 2) gemacht worden. Die Fjeldheidevegetation wurde auf 58 Probeflächen von je 25 m2 untersucht. 2. Bei der Besprechung der Fjeldheidevegetation wird zunächst der Begriff »Fjeldheide» definiert und mit dem Begriff »Tundra» verglichen. Zugleich wird die Zonität der (oro)arktischen Vegetation erörtert und mit den in Grönland, Fennoskandien und Nowaja Semlja vorgenommen Zoneneinteilungen verglichen. Im Rahmen der Dreizoneneinteilung der (oro)arktischen Vegetationszone werden in Spitzbergen die mittel- und die oberoroarktische Stufe angetroffen. 3. In der untersuchten Fjeldheidevegetation wurden 5 Artengruppen und entsprechend 5 Heidetypen herausgearbeitet: 1. Deflations-, 2. Flechten-, 3. trockene und 4. frische Moosheide sowie 5.Schneebodenstellen. Die Grenze zwischen den Typen und auch zwischen den innerhalb eines jeden Typs anzutreffenden Westküsten- und Binnengebietvarianten sind fliessend. Das Westküstengebiet umfasst die Untersuchungsstellen 1-6, das Binnengebiet (=Innenfjord- und Binnenlandgebiet) die Punkte 7-20. 4. Das Westküstengebiet gehört vorwiegend ins Bereich der metamorphierten, das Binnengebiet wiederum ins Gebiet der nicht metamorphierten Gesteine. Für die Entstehung der die obigen Gebiete charakterisierenden Varianten wird jedoch nach meiner Meinung dem Grossklima die ausschlaggebende Bedeutung beigemessen. Die Westküste ist hygrisch und thermisch ozeanischer als das Binnengebiet (Abb. 6). Dieser Umstand macht sich in der Vegetation auch in den Mangenverhältnissen der Typen geltend: an der Westküste viele Deflationsheiden und SchneebodensteIlen (siehe S. 43). Ferner ist die Höhengrenze der mittelarktischen Stufe an der Westküste tiefer (siehe S. 43). Die Phänologie der Pflanzen lässt an der Westküste Verspätung der Entwicklung erkennen (siehe Tab. 9 und 10). An der Westküste steht die Fjeldheidevegetation auf gröberem Untergrund (siehe Tab. 8), und das Eis reicht weiter herunter als im Binnengebiet. 5. Beim Vergleich der Fjeldheidetypen miteinander wurden Unterschiede in der Dicke des Auftaubodens und in der Phänologie der Pflanzen beobachtet, welche Umstände mit der Dicke der Schneedecke zusammenhängen dürften. Die Dicke des Auftaubodens wird zu den frischen Moosheiden hin geringer und nimmt dann an den SchneebodensteIlen wieder zu (Tab. 8). Die Entwicklung der Pflanzen setzt umso zeitiger ein, je trockener der Typ ist (Tab. 9 und 10). 6. Mit Hilfe der Literatur wird der Versuch gemacht, Vegetationen ausfindig zu machen, die sich mit den Fjeldheidetypen Spitzbergens identifizieren (= Horistisch gleichartig sind; vgL Abb. 11) oder vergleichen lassen (= floristisch andersartig, aber an mehr oder minder gleichartigen Standorten). Zusammenfassend wird hauptsächlich anhand der Literatur ein vorläufiger Vorschlag für die Vegetations gebiete Spitzbergens gemacht (Abb. 10).
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.