The use of Open Reading frame ESTs (ORESTES) for analysis of the honey bee transcriptome

Abstract Background The ongoing efforts to sequence the honey bee genome require additional initiatives to define its transcriptome. Towards this end, we employed the Open Reading frame ESTs (ORESTES) strategy to generate profiles for the life cycle of Apis mellifera workers. Results Of the 5,021 ORESTES, 35.2% matched with previously deposited Apis ESTs. The analysis of the remaining sequences defined a set of putative orthologs whose majority had their best-match hits with Anopheles and Drosophila genes. CAP3 assembly of the Apis ORESTES with the already existing 15,500 Apis ESTs generated 3,408 contigs. BLASTX comparison of these contigs with protein sets of organisms representing distinct phylogenetic clades revealed a total of 1,629 contigs that Apis mellifera shares with different taxa. Most (41%) represent genes that are in common to all taxa, another 21% are shared between metazoans (Bilateria), and 16% are shared only within the Insecta clade. A set of 23 putative genes presented a best match with human genes, many of which encode factors related to cell signaling/signal transduction. 1,779 contigs (52%) did not match any known sequence. Applying a correction factor deduced from a parallel analysis performed with Drosophila melanogaster ORESTES, we estimate that approximately half of these no-match ESTs contigs (22%) should represent Apis-specific genes. Conclusions The versatile and cost-efficient ORESTES approach produced minilibraries for honey bee life cycle stages. Such information on central gene regions contributes to genome annotation and also lends itself to cross-transcriptome comparisons to reveal evolutionary trends in insect genomes.

Differences in diversity, structure, and variability between intertidal and subtidal meiofaunal assemblages

[EN] Meiofaunal assemblages from intertidal and shallow subtidal seabeds were studied at two sites (one dominated by volcanic sands and the other by organogenic sands) at Tenerife (Canary Islands, NE Atlantic Ocean) throughout an entire year (May 2000?April 2001). Specifically, we aimed (i) to test for differences in diversity, structure, and stability between intertidal and subtidal meiofaunal assemblages, and (ii) to determine if differences in the meiofaunal assemblage structure may be explained by environmental factors (granulometric composition, availability of organic matter, and carbonate content in sediments). A total of 103,763 meiofaunal individuals were collected, including 203 species from 19 taxonomic groups (Acari, Amphipoda, Cnidaria, Copepoda, Echinodermata, Gastrotricha, Isopoda, Insecta, Kinorrhyncha, Misidacea, Nematoda, Nemertini, Oligochaeta, Ostracoda, Polychaeta, Priapulida, Sipuncula, Tanaidacea, and Turbellaria). Nematodes were the most abundant taxonomic group. Species diversity was higher in the subtidal than in the intertidal zone at both sites, as a result of the larger dominance of a few species in the intertidal zone. The meiofaunal assemblage structure was different between tidal levels at both sites, the intertidal presenting greater temporal variability (multivariate dispersion) in the meiofaunal assemblage structure than the subtidal. Sediment grain size, here quantified by the different granulometric fractions, explained the variability in meiofaunal assemblage structure to a greater extent than the percentage of carbonates, a variable linked to sediment origin. This study revealed differences in diversity, assemblage structure, and variability between intertidal and subtidal meiofauna.

Revision der paläarktischen Arten der Gattung Lygus Hahn (Heteroptera, Miridae)

Als Ergebnis der Revision der Gattung Lygus Hahn (Heteroptera, Miridae, Insecta) wurden die fünf neuen Arten beschrieben: L. sibiricus Aglyamzyanov, 1990, L. orientis Aglyamzyanov, 1994, L. izyaslavi Aglyamzyanov, 1994, L. monticola Aglyamzyanov, 1994 und L. martensi Aglyamzyanov, 2003. Die vier Speziessnamen wurden synonymisiert: L. dracunculi Josifov, 1992, L. alashanensis Qi, 1993, L. renati Schwartz, 1998 (L. elegans Aglyamzyanov, 1994) = L. poluensis (Wagner, 1967) und L. kerzhneri Qi, 1993 = L. punctatus (Zetterstedt, 1838). Artstatus von L. israelensis Linnavuori, 1962 wurde wiederhergestellt. Nach aktuellen Angaben wurden in der Paläarktis 19 Lygus-Arten festgestellt: L. discrepans Reuter, 1906; L. gemellatus (Herrich-Schaeffer, 1835); L. hsiaoi Zheng & Yu, 1992; L. israelensis Linnavuori, 1962; L. italicus Wagner, 1950; L. izyaslavi Aglyamzyanov, 1994; L. maritimus Wagner, 1949; L. martensi Aglyamzyanov, 2003; L. monticola Aglyamzyanov, 1994; L. orientis Aglyamzyanov, 1994; L. pachycnemis Reuter, 1879; L. paradiscrepans Zheng & Yu, 1992; L. poluensis (Wagner, 1967); L. pratensis (Linnaeus, 1758); L. punctatus (Zetterstedt, 1838); L. rugulipennis Poppius, 1911; L. sibiricus Aglyamzyanov, 1990; L. tibetanus Zheng & Yu, 1992 und L. wagneri Remane, 1955. Es wurden die diagnostischen Merkmale analysiert, eine Bestimmungstabelle erstellt und die Areale der Verbreitung der einigen Arten präzisiert.

Early steps in ventral nerve cord development in chelicerates and myriapods and formation of brain compartments in spiders

The central point of this work is the investigation of neurogenesis in chelicerates and myriapods. By comparing decisive mechanisms in neurogenesis in the four arthropod groups (Chelicerata, Crustacea, Insecta, Myriapoda) I was able to show which of these mechanisms are conserved and which developmental modules have diverged. Thereby two processes of embryonic development of the central nervous system were brought into focus. On the one hand I studied early neurogenesis in the ventral nerve cord of the spiders Cupiennius salei and Achaearanea tepidariorum and the millipede Glomeris marginata and on the other hand the development of the brain in Cupiennius salei.rnWhile the nervous system of insects and crustaceans is formed by the progeny of single neural stem cells (neuroblasts), in chelicerates and myriapods whole groups of cells adopt the neural cell fate and give rise to the ventral nerve cord after their invagination. The detailed comparison of the positions and the number of the neural precursor groups within the neuromeres in chelicerates and myriapods showed that the pattern is almost identical which suggests that the neural precursors groups in these arthropod groups are homologous. This pattern is also very similar to the neuroblast pattern in insects. This raises the question if the mechanisms that confer regional identity to the neural precursors is conserved in arthropods although the mode of neural precursor formation is different. The analysis of the functions and expression patterns of genes which are known to be involved in this mechanism in Drosophila melanogaster showed that neural patterning is highly conserved in arthropods. But I also discovered differences in early neurogenesis which reflect modifications and adaptations in the development of the nervous systems in the different arthropod groups.rnThe embryonic development of the brain in chelicerates which was investigated for the first time in this work shows similarities but also some modifications to insects. In vertebrates and arthropods the adult brain is composed of distinct centres with different functions. Investigating how these centres, which are organised in smaller compartments, develop during embryogenesis was part of this work. By tracing the morphogenetic movements and analysing marker gene expressions I could show the formation of the visual brain centres from the single-layered precheliceral neuroectoderm. The optic ganglia, the mushroom bodies and the arcuate body (central body) are formed by large invaginations in the peripheral precheliceral neuroectoderm. This epithelium itself contains neural precursor groups which are assigned to the respective centres and thereby build the three-dimensional optical centres. The single neural precursor groups are distinguishable during this process leading to the assumption that they carry positional information which might subdivide the individual brain centres into smaller functional compartments.rn

Funktionsaufklärung von Atmungsproteinen in Insekten

Globine sind kleine globuläre Proteine mit nahezu ubiquitärem Vorkommen in allen Tiergruppen. Sie weisen eine typische Sandwichstruktur auf, die in der Regel aus acht α-Helices mit einer zentralen prosthetischen Häm-Gruppe besteht und die Proteine zur Bindung gasförmiger Liganden befähigt. Die Funktionen der Globine reichen von O2-Transport und – Speicherung, über eine Beteiligung bei der Entgiftung reaktiver Sauerstoff- und Stickstoffspezies bis hin zu sensorischen physiologischen Aufgaben. Innerhalb der Klasse der Insekten schien das Vorhandensein von Globinen zunächst auf Insekten mit offensichtlich hypoxischen Habitaten beschränkt zu sein. Die Entdeckung des Globins glob1 in Drosophila melanogaster deutete jedoch eine sehr viel weitere Verbreitung der Globine in Insekten an, die sich durch die Identifizierung von Globingenen in einer Vielzahl von normoxisch lebenden Insekten, wie z.B. Apis mellifera oder Aedes aegypti bestätigte. D. melanogaster besitzt drei Globine, glob1, glob2 und glob3. Glob1 ist eng mit anderen intrazellulären Insektenglobinen verwandt, was zu der Annahme führte, dass es sich bei glob1 um das ursprüngliche und bei glob2 und glob3 um abgeleitete D. melanogaster Globine handelt. Glob1 wird in allen Entwicklungsstadien exprimiert, wobei die Hauptexpressionsorte der Fettkörper und das Tracheensystem sind. Die Transkription des glob1 startet von zwei alternativen Promotoren (Promotor I und II), wodurch in Kombination mit alternativem Splicing vier Transkriptvarianten (Isoform A-D) entstehen, deren Translation jedoch in einer Proteinvariante (glob1) resultiert. Hypoxische Bedingungen führen zu einer vermutlich HIF (=‚hypoxia-inducible factor‘) -vermittelten Abnahme der glob1 Genexpression, wohingegen Hyperoxie eine leichte Zunahme der glob1 mRNA Menge bewirkt. Der mithilfe des UAS/Gal4- Systems erzeugte, RNAi-vermittelte glob1 Knockdown führt zu einer schlechteren Überlebensrate adulter Fliegen unter hypoxischen Bedingungen, einer verkürzten Erholungszeit nach hypoxischem Stupor in Weibchen sowie zu einer erhöhten Resistenz gegenüber dem ROS (=‘reactive oxygen species‘) -generierenden Herbizid Paraquat in Larven und adulten Weibchen. Diese Beobachtungen sprechen für eine Funktion des Drosophila glob1 innerhalb der O2-Versorgung. Unter hyperoxischen Bedingungen hingegen wurde kein Unterschied zwischen Fliegen mit wildtypischer und manipulierter glob1-Expression festgestellt, wodurch eine Beteiligung des glob1 bei der Entgiftung reaktiver Sauerstoffspezies als mögliche Funktion vorerst ausscheidet. Bei glob2 und glob3 handelt es sich um duplizierte Gene. Auf phylogenetischen Rekonstruktionen basierend konnte die Entstehung der Globin-Duplikate auf ein Duplikationsereignis vor der Radiation des Subgenus Sophophora vor mindestens 40 Millionen Jahren zurückgeführt werden. Die durchgeführten Analysen zur molekularen Sequenzevolution der Globin-Duplikate deuten darauf hin, dass glob2 und glob3 nach der Duplikation eine Kombination aus Sub- und Neo-Funktionalisierungsprozessen durchlaufen haben. Glob2 und glob3 zeigen eine deckungsgleiche mRNA Expression, die auf die männliche Keimbahn beschränkt ist. Aufgrund des hohen Konservierungsgrads der für die Häm- und O2-Bindung essentiellen Aminosäuren kann von der Funktionalität beider Proteine ausgegangen werden. Die streng auf die männliche Keimbahn begrenzte Expression von glob2 und glob3 deutet auf eine Rolle der Globin-Duplikate innerhalb der Spermatogenese hin, die möglicherweise in einem Schutz der Spermatogenese vor oxidativem Stress besteht. Auch eine Beteiligung beim korrekten Ablauf der Spermien-Individualisierung, beispielsweise durch Regulation von Apoptoseprozessen wäre denkbar.

Response of chironomid assemblages to environmental change during the early Late-glacial at Gerzensee, Switzerland

Prior to ca. 14,660 yr BP, during the early Late-glacial (Oldest Dryas), larval assemblages of Chironomidae (Insecta: Diptera) in Gerzensee, Switzerland, were dominated by cold stenothermic taxa as well as by taxa typical of subalpine lakes today. This was the coldest period of the entire sequence. After ca. 14,660 yr BP, in the Late Glacial Interstadial (Bølling–Allerød), a temperature increase is recorded by a sharp rise in the oxygen-isotope ratio in lake marl and by an increase in the organic-matter content of the sediments. Changes in the chironomid fauna then are consistent with rising temperatures. This warming trend is interrupted between 14,070 and 13,940 yr BP, coinciding with the GI-1d cold oscillation, but the change in the chironomid assemblage is more consistent with a response to increasing lake depth and density of aquatic macrophytes than falling temperature. A rise in cold-adapted chironomid taxa between 13,840 and 13,710 yr BP suggests that summer air temperatures may have declined. Changes in the chironomid assemblage after 13,710 yr BP suggest a decline in submerged macrophytes coupled with a rise in lake productivity and summer temperature, although the latter is not reflected in the oxygen-isotope record. This suggests that there may have been increasing seasonality during this period when summer temperatures were rising, driven by rising summer insolation, and winters becoming cooler, which is largely reflected in the oxygen-isotope record. A decline in thermophilic chironomids and a rise in cold-adapted taxa after 13,180 yr BP suggest a response to cooling at the beginning of the Gerzensee Oscillation.

Mesozooplankton size data from the fjord branch Kapisigdlit located in the Godthaabsfjord system, West Greenland, 2010

Sampling was conducted from March 24 to August 5 2010, in the fjord branch Kapisigdlit located in the inner part of the Godthåbsfjord system, West Greenland. The vessel "Lille Masik" was used during all cruises except on June 17-18 where sampling was done from RV Dana (National Institute for Aquatic Resources, Denmark). A total of 15 cruises (of 1-2 days duration) 7-10 days apart was carried out along a transect composed of 6 stations (St.), spanning the length of the 26 km long fjord branch. St. 1 was located at the mouth of the fjord branch and St. 6 was located at the end of the fjord branch, in the middle of a shallower inner creek . St. 1-4 was covering deeper parts of the fjord, and St. 5 was located on the slope leading up to the shallow inner creek. Mesozooplankton was sampled by vertical net tows using a Hydrobios Multinet (type Mini) equipped with a flow meter and 50 µm mesh nets or a WP-2 net 50 µm mesh size equipped with a non-filtering cod-end. Sampling was conducted at various times of day at the different stations. The nets were hauled with a speed of 0.2-0.3 m s**-1 from 100, 75 and 50 m depth to the surface at St. 2 + 4, 5 and 6, respectively. The content was immediately preserved in buffered formalin (4% final concentration). All samples were analyzed in the Plankton sorting and identification center in Szczecin (www.nmfri.gdynia.pl). Samples containing high numbers of zooplankton were split into subsamples. All copepods and other zooplankton were identified down to lowest possible taxonomic level (approx. 400 per sample), length measured and counted. Copepods were sorted into development stages (nauplii stage 1 - copepodite stage 6) using morphological features and sizes, and up to 10 individuals of each stage was length measured.

Uso de trampas "Barber" para determinar la diversidad de coleópteros epígeos asociados al cultivo de maní (Arachis hypogaea L.). Córdoba, Argentina

El objetivo fue estudiar la diversidad de coleópteros epígeos en el cultivo de maní, su composición taxonómica y su hábito alimenticio, a fin de aportar conocimientos acerca de especies potencialmente dañinas o benéficas al cultivo. Durante las campañas agrícolas 2004/05, 2005/06 y 2006/07 se colocaron 10 trampas Barber en un lote de maní ubicado en la localidad de Olaeta (Córdoba, Argentina). Se instalaron siguiendo un diseño en "X" dentro del lote en el momento de la siembra del cultivo y se dejaron hasta la cosecha. La colecta se realizó con una frecuencia semanal y el material fue identificado y cuantificado. Se determinó la frecuencia y constancia de cada especie colectada y la riqueza de especies fue calculada a través del Índice de diversidad de Simpson. Se registraron 10 familias y dentro de ellas 19 géneros/especies: los individuos fitófagos representaron entre el 66 y el 71%; los predadores entre el 18 y el 27% y los coprófagos entre el 2 y el 16% en los tres ciclos estudiados. La mayor diversidad (0,80-0,82) se obtuvo entre mediados de diciembre y principios de enero. Las especies fitófagas que se encontraron podrían comportarse como plagas para el cultivo.

Biología de la psychidosmicra Brethesi Blanchard : enemigo natural del "bicho del cesto" común, Oiketicus Kirbyi Guild

La finalidad de este trabajo fué determinar las especies parásitas e hiperparásitas del "bicho del cesto" común, Oiketicus Kirbyi Guild, en Mendoza, a fin de obtener supervivencia de la que se encuentra en mayor número e intensidad. Como resultado de estas investigaciones se comprobó que el calcídido Psychidosmicra Brethesi Blanchard constituye un eficáz enemigo específico del psíquico, llegándose a la conclusión que debe preservarse dicho material por el método de aislamiento en su época oportuna, permitiendo esto incrementar las poblaciones por dispersión artificial y atenuar la acción del factor hiperparasitismo.

Mesozooplankton abundance data from the fjord branch Kapisigdlit located in the Godthaabsfjord system, West Greenland, 2010

Sampling was conducted from March 24 to August 5 2010, in the fjord branch Kapisigdlit located in the inner part of the Godthåbsfjord system, West Greenland. The vessel "Lille Masik" was used during all cruises except on June 17-18 where sampling was done from RV Dana (National Institute for Aquatic Resources, Denmark). A total of 15 cruises (of 1-2 days duration) 7-10 days apart was carried out along a transect composed of 6 stations (St.), spanning the length of the 26 km long fjord branch. St. 1 was located at the mouth of the fjord branch and St. 6 was located at the end of the fjord branch, in the middle of a shallower inner creek . St. 1-4 was covering deeper parts of the fjord, and St. 5 was located on the slope leading up to the shallow inner creek. Mesozooplankton was sampled by vertical net tows using a Hydrobios Multinet (type Mini) equipped with a flow meter and 50 µm mesh nets or a WP-2 net 50 µm mesh size equipped with a non-filtering cod-end. Sampling was conducted at various times of day at the different stations. The nets were hauled with a speed of 0.2-0.3 m s**-1 from 100, 75 and 50 m depth to the surface at St. 2 + 4, 5 and 6, respectively. The content was immediately preserved in buffered formalin (4% final concentration). All samples were analyzed in the Plankton sorting and identification center in Szczecin (www.nmfri.gdynia.pl). Samples containing high numbers of zooplankton were split into subsamples. All copepods and other zooplankton were identified down to lowest possible taxonomic level (approx. 400 per sample), length measured and counted. Copepods were sorted into development stages (nauplii stage 1 - copepodite stage 6) using morphological features and sizes, and up to 10 individuals of each stage was length measured.

Determination of ages and fossil Coleoptera fauna from eight sites in the London region

These data sets report the fossil beetle assemblages identified from the Mesolithic to Late Bronze Age at eight sites in the London region. All but one of the study sites are within 2 km of the modern course of the Thames. The sites produced 128 faunal assemblages that yielded 218 identified species in 41 families of Coleoptera (beetles).  Beetle faunas of Mesolithic age indicate extensive wetlands near the Thames, bordered by rich deciduous woodlands. The proportion of woodland species declined in the Neolithic, apparently because of the expansion of wetlands, rather than because of human activities. The Early Bronze Age faunas contained a greater proportion of coniferous woodland and aquatic (standing water) species. An increase in the dung beetle fauna indicates the presence of sheep, cattle and horses, and various beetles associated with crop lands demonstrate the local rise of agriculture, albeit several centuries after the beginnings of farming in other regions of Britain. Late Bronze Age faunas show the continued development of agriculture and animal husbandry along the lower Thames. About 33% of the total identified beetle fauna from the London area sites have limited modern distributions or are extinct in the U.K. Some of these species are associated with the dead wood found in primeval forests; others are wetland species whose habitat has been severely reduced in recent centuries. The third group is stream-dwelling beetles that require clean, clear waters and river bottoms.

Benthic foraminifera extinctions in the Cenozoic record

In the late Pliocene-middle Pleistocene a group of 95 species of elongate, cylindrical, deep-sea (lower bathyal-abyssal) benthic foraminifera became extinct. This Extinction Group (Ext. Gp), belonging to three families (all the Stilostomellidae and Pleurostomellidae, some of the Nodosariidae), was a major component (20-70%) of deep-sea foraminiferal assemblages in the middle Cenozoic and subsequently declined in abundance and species richness before finally disappearing almost completely during the mid-Pleistocene Climatic Transition (MPT). So what caused these declines and extinction? In this study 127 Ext. Gp species are identified from eight Cenozoic bathyal and abyssal sequences in the North Atlantic and equatorial Pacific Oceans. Most species are long-ranging with 80% originating in the Eocene or earlier. The greatest abundance and diversity of the Ext. Gp was in the warm oceanic conditions of the middle Eocene-early Oligocene. The group was subjected to significant changes in the composition of the faunal dominants and slightly enhanced species turnover during and soon after the rapid Eocene-Oligocene cooling event. Declines in the relative abundance and flux of the Ext. Gp, together with enhanced species loss, occurred during middle-late Miocene cooling, particularly at abyssal sites. The overall number of Ext. Gp species present began declining earlier at mid abyssal depths (in middle Miocene) than at upper abyssal (in late Pliocene-early Pleistocene) and then lower bathyal depths (in MPT). By far the most significant Ext. Gp declines in abundance and species loss occurred during the more severe glacial stages of the late Pliocene-middle Pleistocene. Clearly, the decline and extinction of this group of deep-sea foraminifera was related to the function of their specialized apertures and the stepwise cooling of global climate and deep water. We infer that the apertural modifications may be related to the method of food collection or processing, and that the extinctions may have resulted from the decline or loss of their specific phytoplankton or prokaryote food source, that was more directly impacted than the foraminifera by the cooling temperatures.

Pliocene/Pleistocene benthic foraminiferal abundances from six drilling cores

Twenty percent (19 genera, 95 species) of cosmopolitan, deep-sea (500-4000 m), benthic foraminiferal species became extinct during the late Pliocene-Middle Pleistocene (3-0.12 Ma), with the peak of extinctions (76 species) occurring during the mid-Pleistocene Climate Transition (MPT, 1.2-0.55 Ma). One whole family (Stilostomellidae, 30 species) was wiped out, and a second (Pleurostomellidae, 29 species) was decimated with just one species possibly surviving through to the present. Our studies at 21 deep-sea core sites show widespread pulsed declines in abundance and diversity of the extinction group species during more extreme glacials, with partial interglacial recoveries. These declines started in the late Pliocene in southern sourced deep water masses (Antarctic Bottom Water, Circumpolar Deep Water) and extending into intermediate waters (Antarctic Intermediate Water, North Atlantic Deep Water) in the MPT, with the youngest declines in sites farthest downstream from high-latitude source areas for intermediate waters. We infer that the unusual apertural types that were targeted by this extinction period were adaptations for a specific kind of food source and that it was probably the demise of this microbial food that resulted in the foraminiferal extinctions. We hypothesize that it may have been increased cold and oxygenation of the southern sourced deep water masses that impacted on this deep water microbial food source during major late Pliocene and Early Pleistocene glacials when Antarctic ice was substantially expanded. The food source in intermediate water was not impacted until major glacials in the MPT when there were significant expansion of polar sea ice in both hemispheres and major changes in the source areas, temperature, and oxygenation of global intermediate waters.