Seed beetles (Coleoptera: Bruchidae) associated with Acacia cornigera (L.) Willd., with description of a new species of Acanthoscelides Schilsky

Presented herein is a key to identify species of Bruchidae associated with Acacia cornigera (L.). For each species, host records, distributions and bionomics are given. A new species of Acanthoscelides Schilsky is described and figured; Acanthoscelides sauli Romero, Cruz, and Kingsolver

Soil Rotifers new to Hungary from the floodplain Gemenc (Duna-Dráva National Park, Hungary)

In summer and autumn 2010, we collected soil samples from the Gemenc floodplain of the Danube (Duna-Dráva National Park) from places with different flood regimes and vegetation cover and examined them for rotifers. We found a total of 31 species; 14 of them are new to the Hungarian fauna. The Hungarian occurrence of 8 further species is confirmed based on their first detailed data from the country. The genus Wierzejskiella Wiszniewski, 1934 is also new for Hungary. This study provides additional support to the conclusion that floodplains of large rivers have a diverse and sensitive biota

5. Wochenbericht MSM01/3

Maria S. Merian Cruise 1 leg 3 Last report: 10. 05. - 18. 05. 2006 Der 3. Fahrtabschnitt der 1. Reise des neuesten deutschen Forschungsschiffes Maria S. Merian führt in die Schlammvulkanprovinz des Golf von Cadiz. Hier sollen Untersuchungen von biogeochemischen Stoffumsätzen, Fluid- und Gas-Flüssen an spezifischen Ökosystemen wie anoxischen Lebensgemeinschaften und azooxanthellaten Steinkorallen durchgeführt werden. Die Fahrt, die in 2 Unterabschnitte geteilt ist, beginnt in Kiel gefolgt von einem Zwischenstopp in Cadiz (Spanien) und endet in Lissabon (Portugal). MSM- 1/3 ist eine multidisziplinäre Expedition mit biologischen, geologischen und hydrographischen Fragestellungen. Ein Teil der Untersuchungen wird im Rahmen des „Geotechnologien” Programms des BMBF und der DFG für den Schwerpunkt „Methan im Geo-/Biosystem” durch das am IFM-GEOMAR koordinierte und für das ebenfalls hier schwerpunktmäßig angesiedelte Programm COMET (Controls on methane fluxes and their climatic relevance in marine gas hydrate-bearing environments) durchgeführt. Ein weiterer Teil der Ausfahrt dient den Untersuchungen im Rahmen des FP-6 Programms der EU HERMES (Hotspot Ecosystem Research on the Margins of European Seas). Aus dem HERMES-Programm nehmen 6 Partner teil. Beide Forschungsvorhaben sind sehr umfangreich und in ihrer Thematik komplex. Es gibt neben der geographischen Orientierung auf das Gebiet des Golf von Cadiz eine Vielzahl von inhaltlichen, personellen und logistischen Verbindungen zwischen beiden Programmen. Golf von Cadiz: Geologischer Hintergrund Die Region des Golf von Cadiz hat eine sehr komplexe geologische Geschichte. Sie ist seit der Trias durch mehrere tektonische Phasen mit Extension, Kompression und Lateralverschiebungen gekennzeichnet. Während des Mesozoikums und frühen Känozoikums bildeten sich in diesem Gebiet Bruchzonen mit Halbgraben-Strukturen und Karbonatplattformen. Im Torton verlagerte sich der Gibraltar-Bogen nach Westen. Dadurch wurde der Golf von Cadiz zu einem Forearc-Becken, in das Olistostrome (Rutschmassen) hineinglitten. In diesem Ablagerungsmilieu, das sonst für Akkretionskeile charakteristisch ist, wurden die Sedimente des südiberischen und nordafrikanischen Kontinentalrandes der damaligen Tethys stark deformiert. Die Olistostrom-Bildung war im oberen Miozän beendet. Gleichzeitig nahm die Subsidenz des Gebietes zu, und es kam zur Ausbildung von mächtigen Abfolgen progradierender und aggradierender Vorschüttfächer. Die geodynamische Interpretation dieser tektonisch sehr komplexen Region ist bis heute kontrovers. Der Gibraltarbogen liegt am östlichen Ausläufer der Azoren-Gibraltar Transformstörung, die als transpressionelle Grenze der iberischen und afrikanischen Platte gesehen wird. Die NW-SE gerichtete Konvergenz dieser beiden Platten zeigt sehr langsame Relativbewegungen von nur 4 mm pro Jahr. Die Ergebnisse neuester geophysikalischer Untersuchungen weisen jedoch darauf hin, dass auch eine ostwärtige Subduktion unter den Gibraltar-Bogen die gegensätzlichen Beobachtungen tektonischer Phänomene aus dem Riffgebirge und der Bethischen Kordillere erklären kann. Eine westwärts gerichtete Gegenrotation erzeugt Krustendehnung und damit Subsidenz in der Alboran See, während die damit verbundene westwärtige Verlagerung des Gibraltar-Bogens eine kompressionelle Deformation des Atlantis-Akkretionskeiles bewirkt. Es ist zu erwarten, dass die aktive Subduktion im Golf von Cadiz einen starken Einfluss auf das natürliche Gefahrenpotential dieser Region ausübt. Sie muss beispielsweise als Ursache für das große Erdbeben von 1755 gesehen werden (Stärke 8.5), durch das und den nachfolgenden Tsunami schwere Schäden in Lissabon und im angrenzenden Küstengebiet des Golf von Cadiz verursacht wurden. Diese historischen Ereignisse sind ein gewichtiger Grund dafür, dass der Golf von Cadiz eine Schlüsselregion für Europäische Forschungsaktivitäten und instrumenteller Langzeitbeobachtungen im Rahmen der EU-Programme ESONET, HERMES und EuroSEIZE bildet. Aus den Ergebnissen verschiedener Expeditionen ergeben sich viele Hinweise auf weit verbreitete Fluidaustritte, Karbonatmounds mit Tiefwasserkorallen (Lophelia-Skelette), Kohlenwasserstoff-Gasaustritte und Schlammdiapirismus am portugiesischen, spanischen und marokkanischen Kontinentalrand des Golf von Cadiz. Diese Phänomene wurden als Indikatoren für die weit verbreitete Existenz von gasübersättigten Sedimenten und der Migration von Fluiden diffusiv durch die Sedimente oder advektiv entlang von tektonischen Störungen interpretiert

Cryptic species in a well-known habitat: applying taxonomics to the amphipod genus Epimeria (Crustacea, Peracarida)

Taxonomy plays a central role in biological sciences. It provides a communication system for scientists as it aims to enable correct identification of the studied organisms. As a consequence, species descriptions should seek to include as much available information as possible at species level to follow an integrative concept of ‘taxonomics’. Here, we describe the cryptic species Epimeria frankei sp. nov. from the North Sea, and also redescribe its sister species, Epimeria cornigera. The morphological information obtained is substantiated by DNA barcodes and complete nuclear 18S rRNA gene sequences. In addition, we provide, for the first time, full mitochondrial genome data as part of a metazoan species description for a holotype, as well as the neotype. This study represents the first successful implementation of the recently proposed concept of taxonomics, using data from highthroughput technologies for integrative taxonomic studies, allowing the highest level of confidence for both biodiversity and ecological research

Efecto de diferentes dietas sobre la regeneración tisular en "Dendrophyllia cornigera" (Lamarck, 1816)

[Resumen] Dendrophyllia cornigera (Lamarck, 1816) es una especie de coral escleractinio de agua fría que se encuentra a profundidades de (30-) 200-800 m. Al tratarse de una especie ahermatípica, la heterotrofía es su principal vía de captación de energía. Por otro lado, posee la capacidad de regenerar el tejido vivo que recubre su esqueleto. Esta capacidad es vital para la integridad y supervivencia de las colonias. En este trabajo, se estudió el efecto de diferentes tipos de dieta (Artemia salina adulta congelada, caballa, mejillón y pienso) sobre la capacidad de regeneración tisular en D. cornigera. Para ello, se puso en marcha una instalación acuariológica donde se dotó al material biológico de las condiciones necesarias para su mantenimiento. La capacidad de regeneración tisular se estudió mediante el cálculo de la Tasa de Regeneración Tisular (expresada en mm2/día), que mostró diferencias significativas entre los diferentes grupos de dieta (p=0.001). Por otro lado, se representó la Superficie Regenerada de cada tipo de dieta frente al tiempo transcurrido. Por último, se realizó un seguimiento fotográfico de las colonias para obtener un registro visual de la capacidad de regeneración tisular. Los resultados mostraron que la dieta compuesta de Artemia salina adulta congelada fue la que arrojó valores más elevados de Tasa de Regeneración Tisular, así como una recuperación de superficie más rápida que el resto de dietas. Este estudio supone un acercamiento a las técnicas que pueden ser empleadas para la recuperación de corales de agua fría en ambientes controlados.[Abstract] Dendrophyllia cornigera (Lamarck, 1816) is a scleractinian, cold-water coral species that can be found in depths from (30-) 200-800 m. As it is an ahermatipic species, heterotrophy is its main mechanism of energy intake. On the other hand, it has the capacity to regenerate the living tissue that covers its skeleton. This capacity is vital for the integrity and survival of the colonies. In this essay, the effect that different diets (frozen adult Artemia salina, mackerel, mussel and feed) could cause on the capacity of tissue regeneration in D. cornigera was studied. For that purpose, an aquariologic system was set up, where the biological material was provided with all the necessary conditions for its maintenance. The capacity of tissue regeneration was analyzed via Tissue Regeneration Rate (mm2/day), which showed significant differences between the different groups (p=0.001). Besides, Regenerated Surface of each diet group vs time was represented. Lastly, a photographic monitoring of the colonies was made to obtain a visual register of the capacity of tissue regeneration. The results showed that the diet consisted of frozen adult Artemia salina generated the highest values of Tissue Regeneration Rate, additionally to create the fastest regeneration of surface. This study means an approach to the techniques that can be used to recover cold-water corals in controlled environmentsTraballo fin de mestrado (UDC.CIE). Bioloxía mariña Curso 2014/201

Nomina dubia and faunistic issues with New Zealand spiders(Araneae)

Attempts to clarify the identity of obscure New Zealand spider taxa have lead to the conclusion that six species are best treated as nomina dubia [Philodromus rubrofrontus Urquhart 1891 (Philodromidae); Dictyna urquhartii Roewer 1951, (Dictynidae); Linyphia albiapiata Urquhart 1891, Linyphia cruenta Urquhart 1891, Linyphia multicolor Urquhart 1891, Linyphia pellos Urquhart 1891 (Linyphiidae)]. Four species currently listed in Araneus Clerck 1757 (Araneidae) are re-affirmed as synonyms [Araneus lineaacutus (Urquhart 1887) = Zealaranea crassa (Walckenaer 1842), Araneus powelli (Urquhart 1894) = Novaranea laevigata (Urquhart 1891), Araneus sublutius (Urquhart 1892b) = Zealaranea trinotata (Urquhart 1890), Araneus ventricosellus (Roewer 1942) = Eriophora heroine (L. Koch 1871)]. An old record of Araneus brisbanae (L. Koch 1867b) (Araneidae) from New Zealand is a misidentification of Eriophora decorosa Urquhart 1894. The family Philodromidae, the genera Dictyna Sundevall 1833 (Dictynidae) and Linyphia Latreille 1804 (Linyphiidae), as well as Tharpyna munda L. Koch 1875 (Thomisidae) and Araneus brisbanae (Araneidae) are absent from New Zealand

New paleoenvironmental insights on the Miocene condensed phosphatic layer of Salento (southern Italy) unlocked by the coral-mollusc fossil archive

From the Late Oligocene to the Late Miocene, the central Mediterranean area was characterized by the extensive deposition of phosphate-rich sediments. They are usually represented by 10 to 20-cm-thick hardgrounds made of phosphatic and glauconitic sediments containing a rich macrofossil association. This study represents the first thorough investigation of the biotic assemblage of Mediterranean phosphorites aimed at collecting new information on the environmental factors controlling their deposition. The Serravallian/Tortonian phosphatic deposits of the Salento Peninsula (“Aturia level”) have been selected for the abundance of fossil remains and special attention is given to the coral–mollusc association. Two different facies have been recognized: a basal coral rudstone that includes most of the macrofossils, superimposed by a detrital rudstone made of thin layers mainly composed of phosphatic fragments. These two facies are separated by a phosphatic crust several millimeters in thickness. The coral assemblage contains at least 17 azooxanthellate taxa belonging to four families, while the molluscs are represented by a rich gastropod fauna (26 species), associated with bivalves (18 species) and cephalopods (two species). Four distinct depositional phases have been recognized, with the coral rudstone representing the key-facies to reconstruct the onset of the “Aturia level” and the original environment of its fossil content. The composition of the coral–mollusc association has been reliably compared with present-day analog taxa, suggesting the occurrence of a heterogeneous seafloor formed by rocky substrates and accumulations of soft sediment, at around 100–350-m water depth, and under the influence of moderate-to-strong bottom currents rich in nutrients and resuspended organic matter

Calcification is not the Achilles' heel of cold-water corals in an acidifying ocean.

Ocean acidification is thought to be a major threat to coral reefs: laboratory evidence and CO2 seep research has shown adverse effects on many coral species, although a few are resilient. There are concerns that cold-water corals are even more vulnerable as they live in areas where aragonite saturation (Ωara ) is lower than in the tropics and is falling rapidly due to CO2 emissions. Here, we provide laboratory evidence that net (gross calcification minus dissolution) and gross calcification rates of three common cold-water corals, Caryophyllia smithii, Dendrophyllia cornigera, and Desmophyllum dianthus, are not affected by pCO2 levels expected for 2100 (pCO2  1058 μatm, Ωara 1.29), and nor are the rates of skeletal dissolution in D. dianthus. We transplanted D. dianthus to 350 m depth (pHT 8.02; pCO2  448 μatm, Ωara 2.58) and to a 3 m depth CO2 seep in oligotrophic waters (pHT 7.35; pCO2  2879 μatm, Ωara 0.76) and found that the transplants calcified at the same rates regardless of the pCO2 confirming their resilience to acidification, but at significantly lower rates than corals that were fed in aquaria. Our combination of field and laboratory evidence suggests that ocean acidification will not disrupt cold-water coral calcification although falling aragonite levels may affect other organismal physiological and/or reef community processes

Cold-Water Corals and Anthropogenic Impacts in La Fonera Submarine Canyon Head, Northwestern Mediterranean Sea

We assess the occurrence and extent of cold-water coral (CWC) species Madrepora oculata and Dendrophyllia cornigera, as well as gorgonian red coral Corallium rubrum, in La Fonera canyon head (Northwestern Mediterranean Sea), as well as human impacts taking place in their habitats. Occurrence is assessed based on Remotely Operated Vehicle (ROV) video imaging. Terrain classification techniques are applied to high-resolution swath bathymetric data to obtain semi-automatic interpretative maps to identify the relationship between coral distribution patterns and canyon environments. A total of 21 ROV immersions were carried out in different canyon environments at depths ranging between 79 and 401 m. Large, healthy colonies of M. oculata occur on abrupt, protected, often overhanging, rocky sections of the canyon walls, especially in Illa Negra branch. D. cornigera is sparser and evenly distributed at depth, on relatively low sloping areas, in rocky but also partially sedimented areas. C. rubrum is most frequent between 100 and 160 m on highly sloping rocky areas. The probable extent of CWC habitats is quantified by applying a maximum entropy model to predict habitat suitability: 0.36 km2 yield M. oculata occurrence probabilities over 70%. Similar predictive models have been produced for D. cornigera and C. rubrum. All ROV transects document either the presence of litter on the seafloor or pervasive trawling marks. Nets and longlines are imaged entangled on coral colonies. Coral rubble is observed at the foot of impacted colonies. Some colonies are partially covered by sediment that could be the result of the resuspension generated by bottom trawling on neighbouring fishing grounds, which has been demonstrated to be responsible of daily increases in sediment fluxes within the canyon. The characteristics of the CWC community in La Fonera canyon are indicative that it withstands high environmental stress of both natural and human origin

Diversity of active constituents in Cichorium endivia and Cynara cornigera extracts

The present study attempts to explore the phytochemical constituents of different extracts from Cynara cornigera and Cichorium endivia plant materials. The two species studied are native in Egypt. Five different solvents, viz., aqueous, methylene chloride, petroleum ether, ethyl acetate, and n-butanol were used. Phytochemical analysis revealed the presence of phenols, flavonoids, sterols (stigmasterol and beta-sitosterol), terpenes (α-amyrin, ursolic and oleanolic acid), and hydrocarbons (n-alkane), the latter found in low amount. The ethyl acetate and water extracts of C. cornigera root showed lower mass fractions of phenolic compounds ranged from 20 to 81 g/100 g, and higher amounts in ethyl acetate extract of the inflorescences and butanol extract of the root where values ranged from 195 to 399 g/100 g. The β-sitosterol and stigmasterol were present in all plant extracts. Oleanolic and ursolic acids were detected in roots, leaves and inflorescences of C. cornigera and in C. endivia shoot. The ethyl acetate extracts from C. cornigera leaf and inflorescence attained higher chemical diversity than the other extracts. Alternatively, sterols and triterpenes were the major constituents. The high chemical diversity of active constituents justifies the future potential use of the two species at commercial level