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.

The Global Plankton Database: an inventory and data from the Former Soviet Union expeditions

At present time, there is a lack of knowledge on the interannual climate-related variability of zooplankton communities of the tropical Atlantic, central Mediterranean Sea, Caspian Sea, and Aral Sea, due to the absence of appropriate databases. In the mid latitudes, the North Atlantic Oscillation (NAO) is the dominant mode of atmospheric fluctuations over eastern North America, the northern Atlantic Ocean and Europe. Therefore, one of the issues that need to be addressed through data synthesis is the evaluation of interannual patterns in species abundance and species diversity over these regions in regard to the NAO. The database has been used to investigate the ecological role of the NAO in interannual variations of mesozooplankton abundance and biomass along the zonal array of the NAO influence. Basic approach to the proposed research involved: (1) development of co-operation between experts and data holders in Ukraine, Russia, Kazakhstan, Azerbaijan, UK, and USA to rescue and compile the oceanographic data sets and release them on CD-ROM, (2) organization and compilation of a database based on FSU cruises to the above regions, (3) analysis of the basin-scale interannual variability of the zooplankton species abundance, biomass, and species diversity.

Discarge compilation from The Global River Discharge (RivDIS) Project

The Global River Discharge (RivDIS) data set contains monthly discharge measurements for 1018 stations located throughout the world. The period of record varies widely from station to station, with a mean of 21.5 years. These data were digitized from published UNESCO archives by Charles Voromarty, Balaze Fekete, and B.A. Tucker of the Complex Systems Research Center (CSRC) at the University of New Hampshire. River discharge is typically measured through the use of a rating curve that relates local water level height to discharge. This rating curve is used to estimate discharge from the observed water level. The rating curves are periodically rechecked and recalibrated through on-site measurement of discharge and river stage.

La construcción del espacio litoral. Una aproximación desde el marco legal

A lo largo del siglo XIX, y coincidiendo con la disminución de su valor estratégico militar, el litoral resurge como fuente de recursos económicos y productivos y como elemento de ocio y disfrute personal. Es también por estas fechas cuando vuelve a recuperarse el concepto de dominio público marítimo terrestre ya recogido por el derecho romano y las Partidas del Rey Alfonso X ?el Sabio?. La Ley de Aguas de 1866, que regula tanto las aguas terrestres como las marinas, incluye dentro del dominio público marítimo las costas, o fronteras marítimas, el mar litoral y las playas. Desde ese momento y hasta el día de hoy la costa queda integrada dentro del dominio público marítimo terrestre, cuya definición y delimitación se va perfilando hasta la redacción y aprobación del texto legislativo vigente en la actualidad: la Ley 22/1988, de 28 de julio, de Costas. Sin embargo, el concepto de dominio público está vinculado al Interés General que es interpretado según las necesidades socioeconómicas y políticas de cada momento. La identificación en exclusividad entre Interés General y desarrollo económico en algunos periodos de la historia reciente es una de las principales causas de la degradación actual del litoral: construcción masiva de puertos sin tener en cuenta su ubicación con respecto al funcionamiento físico de la costa, reconocimiento de los derechos privados en la Ley de Puertos de 1880 que autorizó la construcción de viviendas y hoteles dentro de terrenos ganados al mar, la subvención a la desecación de marismas a través de la aplicación de la llamada Ley Cambó, el fomento del turismo de masas desde la política pública (Ley 197/1963, de 28 de diciembre, sobre Centros y Zonas de Interés Turístico Nacional), etc. En este sentido, la explotación del litoral como recurso económico ha llegado a poner en juego el propio equilibrio del sistema físico y natural, con la consecuente afección sobre las actividades económicas y los usos que en él se desarrollan. Con objeto de evitar los riesgos que provoca dicha desestabilización sobre el sistema físico, las políticas en costas han ido encaminadas en su mayoría a la construcción de obras públicas que no son capaces de detener la inercia del sistema ni, por tanto, el riesgo sobre lo que se pretende proteger. El reparto competencial sobre la franja litoral que limita la gestión estatal al DPMT y reconoce la soberanía de las Comunidades Autónomas y Ayuntamientos en las zonas de servidumbre, no ha ayudado a la diversificación de herramientas para la ordenación y gestión del litoral, lo que ha provocado visiones y formas de hacer encontradas dentro de un mismo territorio continuo, como si las decisiones que se toman en la franja de 500 metros mar adentro no influyesen en el estado del DPMT A través de la evolución del concepto de DPMT y espacio litoral en el marco legal, la presente ponencia trata de hacer una aproximación histórica sobre la construcción del espacio urbano en el litoral, evaluando la adecuación de las herramientas urbanísticas para la intervención dentro de dicho espacio dentro del contexto de los nuevos retos de dicho espacio, con especial atención a la gestión integrada de las zonas costeras y a los nuevos riesgos derivados del cambio climático.

Principales maderas tropicales utilizadas en España: Características, tecnología y aplicaciones

Se describen las características de las principales maderas tropicales con uso en España. La descripción incluye el nombre científico, sinonimias, nombres vulgares, su distribución en el mundo y en España, la descripción del fuste y de las trozas, con sus defectos más característicos, la descripción de la madera, sus características físicas, mecánicas, resistentes y durables. También se incluye sus aspectos tecnológicos, en el sentido de indicar que aspectos deben considerarse a la hora de trabajar estas maderas. Por último se indican los usos más comunes de las distintas maderas, las ventajas e inconvenientes frente a otras maderas Las especies principales que se describen son las siguientes: Algarrobo blanco, Prosopis alba, Grisebach Andiroba, Carapa guianensis, Aubl. Balsamo, Myroxylon balsamun, Harms. Sandwith. Barba jolote, Pithecolobium arboreum (L), Urban. Bubinga, Guibourtia tessmanii Caoba, Swietenia macrophylla, King. Cedro, Cedrela odorata, L. Cenizaro, Pithecellobium saman, (Jacq.) Benth Chinchon, Guarea grandiflora, A. DC. Cocobolo, Dalbergia retusa, Hemsl Cristobal, Platysmicium polystachyum Elondo o tali, Erythrophleum ivorensis Espavé, Anacardium excelsum, Skeels Gonzalo Alves, Astronium graveolens, Jacquin. Guayabillo, Terminalia lucida, Hoff. Guapaque, Dialium guianense, (Aubl.) Sandwith. Guayacán, Guaiacum sanctum, L. Huesito Homalium racemosum, Jacq. Ipe, Tabebuia guayacan, Hemsl. Iroko, Milicia excelsa Sim Jatoba, Hymenaea courbaril L. Machiche, Lonchocarpus castilloi, Standley. Manil, Symphonia globulifera, L. Marupa, Simarouba glauca, DC. Melina, Gmelina arborea, Roxb. Mongoy, Guibourtia ehie J. Léonard Nance, Byrsonima crassifolia (L.), H.B.K. Nazareno, Peltogyne purpurea Nispero, Manilkara zapota, (L.) Van royen. Palo blanco, Cybitax donnell- smith , Seibert. Pino amarillo, Erblichia odorata Piojo, Tapirira guianensis, Aubl. Quaruba, Vochysia guatemalensis, Donnell Smith Quira, Platysmicium pinnatum. Redondo, Magnolia yoroconte, Dandy. Rosul, Dalbergia tucurensis, Donn-Smith. Sande, Brossimiun ssp San juan areno, Ilex ssp. Saqui-saqui, Bombacopsis quinatum, (Jacq.) Dugand Santa maría, Calophyllum brasílíense Camb. Sapelly, Entandrophragma cylindricum Sprague Tamboril, Enterolobium cyclocarpum, Gris Teca, Tectona grandis, L.F.. Ukola, Tieghemella africana Ururucana, Hieronyma alchorneoides, Allem

Homospermidine synthase, the first pathway-specific enzyme of pyrrolizidine alkaloid biosynthesis, evolved from deoxyhypusine synthase

Pyrrolizidine alkaloids are preformed plant defense compounds with sporadic phylogenetic distribution. They are thought to have evolved in response to the selective pressure of herbivory. The first pathway-specific intermediate of these alkaloids is the rare polyamine homospermidine, which is synthesized by homospermidine synthase (HSS). The HSS gene from Senecio vernalis was cloned and shown to be derived from the deoxyhypusine synthase (DHS) gene, which is highly conserved among all eukaryotes and archaebacteria. DHS catalyzes the first step in the activation of translation initiation factor 5A (eIF5A), which is essential for eukaryotic cell proliferation and which acts as a cofactor of the HIV-1 Rev regulatory protein. Sequence comparison provides direct evidence for the evolutionary recruitment of an essential gene of primary metabolism (DHS) for the origin of the committing step (HSS) in the biosynthesis of pyrrolizidine alkaloids.

Poems copied by James Diman, ca. 1730-1733

Small pamphlet-sized notebook containing handwritten transcriptions of three poems copied by James Diman, likely in the early 1730s. The notebook contains "The Catholic Remedy. to ye Tune of To all you Ladies, not at land &c.," "Father Ab--y's Will. Col. Sweeper Camb: Dec. 1731," and "The Poet's Lamentation for ye Loss of his cat, w'ch he used to call his Muse" copied from the London Magazine, November 1733. The "Catholic Remedy" begins "You Peope who desire to mend / your Desperate Estate..." and includes the note, "Made upon A--D--'s goving over to take orders. The note refers to the voyage of Addington Davenport (Harvard AB 1719) to England join the priesthood of the Church of England in 1730. "Father Ab--y's Will" begins "To my dear Wife, / My joy and Life..." and was a humorous poem published in 1731 after the death of Harvard College Sweeper Matthew Abdy, and attributed to Jonathan Seccombe (Harvard AB 1728). The "Poet's Lamentation" begins "Oppress'd with Grief, in heavy strains I mourn..." and was written by Joseph Green (Harvard AB 1726) as a parody of a psalm composed by Mather Byles (Harvard AB 1725). Pages 10-12, holding part of "Father Ab--y's Will" are missing, and pages 13-15 are no longer attached to the item.

Plant species, biomass and environmental characteristics of relevés along the North America Arctic bioclimate gradient

Question: How do interactions between the physical environment and biotic properties of vegetation influence the formation of small patterned-ground features along the Arctic bioclimate gradient? Location: At 68° to 78°N: six locations along the Dalton Highway in arctic Alaska and three in Canada (Banks Island, Prince Patrick Island and Ellef Ringnes Island). Methods: We analysed floristic and structural vegetation, biomass and abiotic data (soil chemical and physical parameters, the n-factor [a soil thermal index] and spectral information [NDVI, LAI]) on 147 microhabitat releves of zonalpatterned-ground features. Using mapping, table analysis (JUICE) and ordination techniques (NMDS). Results: Table analysis using JUICE and the phi-coefficient to identify diagnostic species revealed clear groups of diagnostic plant taxa in four of the five zonal vegetation complexes. Plant communities and zonal complexes were generally well separated in the NMDS ordination. The Alaska and Canada communities were spatially separated in the ordination because of different glacial histories and location in separate floristic provinces, but there was no single controlling environmental gradient. Vegetation structure, particularly that of bryophytes and total biomass, strongly affected thermal properties of the soils. Patterned-ground complexes with the largest thermal differential between the patterned-ground features and the surrounding vegetation exhibited the clearest patterned-ground morphologies.

Erysiphella aggregata; Erysiphaceae

Erysiphella aggregata f. vernalis Peck. f. vernalis Thum.