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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.