Microsatellite in Aeschynomene falcata (Leguminosae): diversity, cross-amplification, and chromosome localization

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Addizioni organocatalitiche asimmetriche di 1,3-dicarbonili a orto-chinoni metidi. Un nuovo metodo per la sintesi di 3,4-diidrocumarine e 4h-cromeni otticamente attivi

Questa tesi descrive lo sviluppo di una nuova metodologia che prevede l’utilizzo degli orto-chinoni metidi (o-QMs) in reazioni organocatalitiche asimmetriche. A causa della loro elevata instabilità e reattività, gli o-QMs sono stati impiegati in trasformazioni di sintesi asimmetrica solo di recente. Il metodo sviluppato prevede l’utilizzo di catalizzatori bifunzionali in grado di promuovere la generazione in situ degli intermedi reattivi a partire dai rispettivi 2-solfonilalchil fenoli, tramite eliminazione di acido solfinico. L’utilizzo di condizioni blandamente basiche sia per generare gli o-QMs che per l’attivazione dei partner nucleofili, risulta innovativo e permette non solo di ovviare all’intrinseca instabilità di questi intermedi, ma anche di impiegarli efficacemente in reazioni organocatalitiche con una varietà di nucleofili, come, ad esempio, l’acido di Meldrum, il malononitrile e vari composti 1,3 dicarbonilici. Le reazioni catalitiche portano alla formazione di 3,4-diidrocumarine, 4H-cromeni e xantenoni enantioarricchiti. Alcuni di questi composti sono dei precursori sintetici di composti naturali o sintetici biologicamente attivi e per avvalorare questa metodologia sono state proposte le sintesi formali di tre composti di interesse biologico: la (R)-tolterodina (il principio attivo del farmaco antimuscarinico Detrol®), (S)-4-metossidalbergione (allergene della Dalbergia Nigra) and SB-209670 / SB-217242 (due potenti antagonisti dell’endotelina).

Early Oligocene continental climate ofthe Paleogene Basin in Hungary and Slovenia

This paper concentrates on the Early Oligocene palaeoclimate of the southern part of Eastern and Central Europe and gives a detailed climatological analysis, combined with leaf-morphological studies and modelling of the palaeoatmospheric CO2 level using stomatal and d13 C data. Climate data are calculated using the Coexistence Approach for Kiscellian floras of the Palaeogene Basin (Hungary and Slovenia) and coeval assemblages from Central and Southeastern Europe. Potential microclimatic or habitat variations are considered using morphometric analysis of fossil leaves from Hungarian, Slovenian and Italian floras. Reconstruction of CO2 is performed by applying a recently introduced mechanistic model. Results of climate analysis indicate distinct latitudinal and longitudinal climate patterns for various variables which agree well with reconstructed palaeogeography and vegetation. Calculated climate variables in general suggest a warm and frost-free climate with low seasonal variation of temperature. A difference in temperature parameters is recorded between localities from Central and Southeastern Europe, manifested mainly in the mean temperature of the coldest month. Results of morphometric analysis suggest microclimatic or habitat difference among studied floras. Extending the scarce information available on atmospheric CO2 levels during the Oligocene, we provide data for a well-defined time-interval. Reconstructed atmospheric CO2 levels agree well with threshold values for Antarctic ice sheet growth suggested by recent modelling studies. The successful application of the mechanistic model for the reconstruction of atmospheric CO2 levels raises new possibitities for future climate inference from macro-flora studies.

AMS radiocarbon dates and pollen analysis of ODP Hole 175-1078C

ODP Site 1078 situated under the coast of Angola provides the first record of the vegetation history for Angola. The upper 11 m of the core covers the past 30 thousand years, which has been analysed palynologically in decadal to centennial resolution. Alkenone sea surface temperature estimates were analysed in centennial resolution. We studied sea surface temperatures and vegetation development during full glacial, deglacial, and interglacial conditions. During the glacial the vegetation in Angola was very open consisting of grass and heath lands, deserts and semi-deserts, which suggests a cool and dry climate. A change to warmer and more humid conditions is indicated by forest expansion starting in step with the earliest temperature rise in Antarctica, 22 thousand years ago. We infer that around the period of Heinrich Event 1, a northward excursion of the Angola Benguela Front and the Congo Air Boundary resulted in cool sea surface temperatures but rain forest remained present in the northern lowlands of Angola. Rain forest and dry forest area increase 15 thousand years ago. During the Holocene, dry forests and Miombo woodlands expanded. Also in Angola globally recognised climate changes at 8 thousand and 4 thousand years ago had an impact on the vegetation. During the past 2 thousand years, savannah vegetation became dominant.

Early - Late Miocene palaeoclimate data and palaefloras of 48 samples from Southern China

Southern China, especially Yunnan, has undergone high tectonic activity caused by the uplift of Himalayan Mountains during the Neogene, which led to a fast changing palaeogeography. Previous study shows that Southern China has been influenced by the Asian Monsoon since at least the Early Miocene. However, it is yet not well understood how intense the Miocene monsoon system was. In the present study, 63 fossil floras of 16 localities from Southern China are compiled and evaluated for obtaining available information concerning floristic composition, stratigraphic age, sedimentology, etc. Based on such reliable information, selected mega- and micro-floras have been analysed with the coexistence approach to obtain quantitative palaeoclimate data. Visualization of climate results in maps shows a distinct spatial differentiation in Southern China during the Miocene. Higher seasonalities of temperature and precipitation occur in the north and south parts of Southern China, respectively. During the Miocene, most regions of Southern China and Europe were both warm and humid. Central Eurasia was likely to be an arid center, which gradually spread westward and eastward. Our data provide information about Miocene climate patterns in Southern China and about the evolution of these patterns throughout the Miocene, and is also crucial to unravel and understand the climatic signals of global cooling and tectonic uplift.

Distribution of pollen and spores in sediments of ODP Hole 175-1078C

The distribution of pollen in marine sediments is used to record vegetation change on the continent. Generally, a good latitudinal correspondence exists between the distribution patterns of pollen in the marine surface sediments and the occurrence of the source plants on the adjacent continent. To investigate land-sea interactions during deglaciation, we compare proxies for continental (pollen assemblages) and marine conditions (alkenone-derived sea surface temperatures) of two high-resolution, radiocarbon-dated sedimentary records from the tropical southeast Atlantic. The southern site is located West of the Cunene River mouth; the northern site is located West of the Angolan Huambe Mountains. It is inferred that the vegetation in Angola developed from Afroalpine and open savannah during the last Glacial maximum (LGM) via Afromontane Podocarpus forest during Heinrich Event 1 (H1), to an early increase of lowland forest after 14.5 ka. The vegetation record indicates dry and cold conditions during the LGM, cool and wet conditions during H1 and a gradual rise in temperature starting well before the Younger Dryas (YD) period. Terrestrial and oceanic climate developments seem largely running parallel, in contrast to the situation ca. 5° further South, where marine and terrestrial developments diverge during the YD. The cool and wet conditions in tropical West Africa, South of the equator, during H1 suggest that low-latitude insolation variation is more important than the slowdown of the thermohaline circulation for the climate in tropical Africa.

Late Miocene palaeoflora and palaeoclimate of Lincang (China)

The Miocene Lincang leaf assemblage is used in this paper as proxy data to reconstruct the palaeoclimate of southwestern Yunnan (SW China) and the evolution of monsoon intensity. Three quantitative methods were chosen for this reconstruction, i.e. Leaf Margin Analysis (LMA), Climate Leaf Analysis Multivariate Program (CLAMP), and the Coexistence Approach (CA). These methods, however, yield inconsistent results, particularly for the precipitation, as also shown in European and other East Asian Cenozoic floras. The wide range of the reconstructed climatic parameters includes the Mean Annual Temperature (MAT) of 18.5-24.7 °C and the Mean Annual Precipitation (MAP) of 1213-3711 mm. Compared with the modern Lincang climate (MAT, 17.3 °C; MAP, 1178.7 mm), the Miocene climate is slightly warmer, wetter and has a higher temperature seasonality. A detailed comparison on the palaeoclimatic variables with the coeval Late Miocene Xiaolongtan flora from the eastern part of Yunnan allows us to investigate the development and interactions of both South Asian and East Asian monsoons during the Late Miocene in southwest China, now under strong influence of these monsoon systems. Our results suggest that the monsoon climate has already been established in southwest Yunnan during the Late Miocene. Furthermore, our results support that both Southeast Asian and East Asian monsoons co-occurred in Yunnan during the Late Miocene.

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