Dinoflagellate and other palynomorph abundance in sediments from ODP Leg 189 sites

At Ocean Drilling Program (ODP) Leg 189 Sites 1170-1172, the climatologically critical Eocene-Oligocene (E-O) transition is barren of any calcareous microfossils but contains rich marine organic walled dinoflagellate cyst (dinocyst) and diatom assemblages, suitable for detailed biostratigraphic and paleoenvironmental analysis. The resulting first-ever integrated dinocyst/diatom magnetostratigraphy allows confident correlation of the E-O interval between all Leg 189 sites, including Site 1168. Our correlations indicate that the (deep) opening of the Tasmanian Gateway occurred quasi-synchronously throughout the Tasmanian region, starting at ~35.5 Ma. At Sites 1170-1172, quantitatively, three distinct dinocyst assemblages may be distinguished that reflect the relatively rapid and pronounced stepwise environmental changes associated with the E-O transition in the Tasmanian region, from a pro-deltaic setting to a deep marine pelagic setting. Moreover, synchronous with the deepening of the gateway, at the southern and eastern Sites 1170-1172, typical endemic Antarctic assemblages were replaced by more cosmopolitan dinocyst communities. In marked contrast, at Site 1168 off western Tasmania, endemic Antarctic taxa are virtually absent during the E-O transition. At Sites 1170-1172, the endemic Antarctic dinocyst assemblage (Transantarctic Flora) drastically changes into a more cosmopolitan assemblage at ~35.5 Ma, with a more offshore character, reflecting the arrival of different oceanographic and environmental conditions associated with the deepening of the Tasmanian Gateway. In turn, this assemblage grades at ~34 Ma into one more typical for even more offshore and/or upwelling conditions at Site 1172. In slightly younger deposits at all sites, organic microfossils are virtually absent, reflecting winnowing and oxidation, indicative of a next step of oceanographic development. This phase may be dated as close to the Oceanic Anoxic (Oi)-1 18O (Antarctic glaciation) event (~33.3 Ma). In a single productive sample from the earliest Oligocene the northern Site 1172, a relatively warm-water cosmopolitan assemblage has been recovered. This aspect contrasts findings from coeval deposits from the Ross Sea, where endemic Antarctic species remain dominant. Somewhere between the paleogeographic positions of Site 1172 and the Ross Sea, a strong differentiation of surface waters occurred in the earliest Oligocene, possibly reflecting the onset of the Antarctic Circumpolar Current.

Differences into HT and HTO concentrations in air into the Western Mediterranean Basin and Continental Europe and Safety Related Issues.

Real time Tritium concentrations in air in two chemical forms, HT and HTO, coming from an ITER-like fusion reactor as source were coupled the European Centre Medium Range Weather Forecast (ECMWF) numerical model with the Lagrangian Atmospheric-particle dispersion model FLEXPART. This tool was analyzed in nominal tritium discharge operational reference and selected incidental conditions affecting the Western Mediterranean Basin during 45 days during summer 2010 together with surface “wind observations” or weather data based in real hourly observations of wind direction and velocity providing a real approximation of the tritium behavior after the release to the atmosphere from a fusion reactor. From comparison with NORMTRI - a code using climatologically sequences as input - over the same area, the real time results have demonstrated an apparent overestimation of the corresponding climatologically sequence of Tritium concentrations in air outputs, at several distances from the reactor. For this purpose two development patterns were established. The first one was following a cyclonic circulation over the Mediterranean Sea and the second one was based on the plume delivered over the Interior of the Iberian Peninsula and Continental Europe by another stabilized circulation corresponding to a High Pressure System. One of the important remaining activities defined then, was the qualification tool. In order to validate the model of ECMWF/FLEXPART we have developed of a new complete data base of tritium concentrations for the months from November 2010 to March 2011 and defined a new set of four patterns of HT transport in air, in each case using real boundary conditions: stationary to the North, stationary to the South, fast and very fast displacement. Finally the differences corresponding to those four early patterns (each one in assessments 1 and 2) has been analyzed in terms of the tuning of safety related issues and taking into account the primary phase o- - f tritium modeling, from its discharge to the atmosphere to the deposition on the ground, will affect to the complete tritium environmental pathway altering the chronic dose by absorption, reemission and ingestion both from elemental tritium, HT and from the oxide of tritium, HTO

Validation of real time dispersion of Tritium clouds over the Western Mediterranean Basin in different assesments

Real time Tritium concentrations in air coming from an ITER-like reactor as source were coupled the European Centre Medium Range Weather Forecast (ECMWF) numerical model with the lagrangian atmospheric dispersion model FLEXPART. This tool ECMWF/FLEXPART was analyzed in normal operating conditions in the Western Mediterranean Basin during 45 days at summer 2010. From comparison with NORMTRI plumes over Western Mediterranean Basin the real time results have demonstrated an overestimation of the corresponding climatologically sequence Tritium concentrations in air outputs, at several distances from the reactor. For these purpose two clouds development patterns were established. The first one was following a cyclonic circulation over the Mediterranean Sea and the second one was based in the cloud delivered over the Interior of the Iberian Peninsula by another stabilized circulation corresponding to a High. One of the important remaining activities defined then, was the tool qualification. The aim of this paper is to present the ECMWF/FLEXPART products confronted with Tritium concentration in air data. For this purpose a database to develop and validate ECMWF/FLEXPART tritium in both assessments has been selected from a NORMTRI run. Similarities and differences, underestimation and overestimation with NORMTRI will allowfor refinement in some features of ECMWF/FLEXPART

Contribución al conocimiento de los macrohongos en la provincia de Tambopata -Madre de Dios, Perú

El presente trabajo de investigación es una contribución al conocimiento científico de los macrohongos de los Phyllum Ascomycetos y Basidiomycetos en el departamento amazónico Madre de Dios (Perú), investigación desarrollada en la región durante los años 2006 al 2014. Durante estos años se han recorrido las trochas de investigación dentro de las 6 áreas, seleccionadas según su grado de intervención antrópica, recolectando y fotografiando todos los carpóforos que en ellas se encontraban. Así mismo se ha realizado una revisión bibliografía exhaustiva para poder identificar a estas especies de los Phylum Basidiomycetos y Ascomycetos, fotografiando las esporas en los casos que esto fue posible. Las muestras fueron recolectadas en 6 áreas con diferentes grados de intervención humana, para poder determinar si se encontraba diferencia significativa en la composición de especies de Macrohongos entre ellas. Así mismo se consideró el tipo de bosque donde se encontraba la muestra y el sustrato donde se desarrollaba. Las muestras fueron buscadas y recolectadas en las dos épocas del año (seca y lluviosa), para saber si este factor climatológico era determinante y afectaba el número de carpóforos encontrados. Se han identificado completamente 70 especies pertenecientes a 25 familias, siendo la familia Xylariaceae la más representativa para el Phyllum Ascomycetos y la familia Polyporaceae para el caso del Phyllum basidiomycetos, resultando cinco especies nuevos registros para el Perú. De las especies identificadas 23 son de interés comestible, 13 son de interés medicinal, 2 de interés mágico religioso, 2 tóxicas, 2 micorrizógenas y de 30 especies no se conocen sus usos para la ciencia. Así mismo se identificó a 6 especies promisorias (géneros Auricularia sp. y Pleurotus sp.) para el cultivo con fines alimentarios de autoconsumo y la posible comercialización a pequeña y gran escala, puesto que estas especies promisorias transforman los residuos lignocelulosicos en alimento. Se ha confeccionado una guía de campo para la identificación de los macrohongos, sus usos y recomendaciones para su consumo, con lo cual queda abierta otra puerta de nuestra biodiversidad al interés científico, gastronómico y turístico. ABSTRACT This investigation is a contribution to the scientific knowledge of the Phyllum Ascomycetos and Basidiomycetos mushrooms in the Amazonian department Madre de Dios (Peru). The study was carried out from 2006 till 2014, during which forest study paths were crossed in six areas were all types of found carpophores were collected and photographed. In order to identify the Phylum Basidiomycetos and Ascomycetos species, an intensive biographical review was carried out and photographs were taken from the spores in case it was possible to assist the identification. Samples were collected in six areas with different human intervention and forest types so that any significant difference in the species´ composition could be analyzed between these different zones and between the species specific area. The samples were searched and collected during two different seasons (dry and rainy season) to analyze if this climatologically factor affects the number of found species. In total 70 species were completely identified, belonging to 25 families. The most representative families were the Xylariaceae for the Phyllum Ascomycetos and the Polyporaceae in the case of the Phyllum Basidiomycetos. Of all the identified species, 23 are considered edible, thirteen are identified as medicinal, and two are known for psychedelic and religious practices, two are toxic, two are mycorrhizal species and of 30 species the use is unknown to science. Five species are newly registered for Peru, Moreover, six species of the Auricularia sp. and Pleurotus sp. gender were identified as promising species for cultivation to serve auto consumption and possibly small and large scale commercialization. These species transform lignocelular waste in food. Part of this study was the development of a field guide to identify mushrooms and which can be used to open doors to our biodiversity for multiple interests such as scientific, gastronomy, and tourism.

Granulometry, calcium carbonate content and radiocarbon ages of soil profiles obtained in Quinghai Province, northeast Tibet

Colluvial deposits consisting of silts and loams were detected in several climatologically different areas of NE Tibet (3200-3700 m a.s.l.). Layering, distinct organic content and low content of coarse matter as well as location in the relief revealed an origin from low-energy slope erosion (hillwash). Underlying and intercalated paleosols were classified as Chernozems, Phaeozems, Regosols and Fluvisols. Fifteen radiocarbon datings predominant on charcoal from both colluvial layers and paleosols yielded ages between 8988 ± 66 and 3512 ± 56 uncal BP. Natural or anthropogenic factors could have been the triggers of the erosional processes derived. It remains unclear which reason was mainly responsible, due to controversial paleoclimatic and geomorphic records as well as insufficient archaeological knowledge from this region. Determinations of charcoal and fossil wood revealed the Holocene occurrence of tree species (spruce, juniper) for areas which nowadays have no trees or only few forest islands. Thus large areas of NE Tibet which are at present steppes and alpine pastures were forested in the past.

Multiple solutions and numerical analysis to the dynamic and stationary models coupling a delayed energy balance model involving latent heat and discontinuous albedo with a deep ocean

We study a climatologically important interaction of two of the main components of the geophysical system by adding an energy balance model for the averaged atmospheric temperature as dynamic boundary condition to a diagnostic ocean model having an additional spatial dimension. In this work, we give deeper insight than previous papers in the literature, mainly with respect to the 1990 pioneering model by Watts and Morantine. We are taking into consideration the latent heat for the two phase ocean as well as a possible delayed term. Non-uniqueness for the initial boundary value problem, uniqueness under a non-degeneracy condition and the existence of multiple stationary solutions are proved here. These multiplicity results suggest that an S-shaped bifurcation diagram should be expected to occur in this class of models generalizing previous energy balance models. The numerical method applied to the model is based on a finite volume scheme with nonlinear weighted essentially non-oscillatory reconstruction and Runge–Kutta total variation diminishing for time integration.