Results of n-alkane biomarker analyses and paleoclimate reconstruction

The current study presents quantitative reconstructions of tree cover, annual precipitation and mean July temperature derived from the pollen record from Lake Billyakh (65°17'N, 126°47'E, 340 m above sea level) spanning the last ca. 50 kyr. The reconstruction of tree cover suggests presence of woody plants through the entire analyzed time interval, although trees played only a minor role in the vegetation around Lake Billyakh prior to 14 kyr BP (<5%). This result corroborates low percentages of tree pollen and low scores of the cold deciduous forest biome in the PG1755 record from Lake Billyakh. The reconstructed values of the mean temperature of the warmest month ~8-10 °C do not support larch forest or woodland around Lake Billyakh during the coldest phase of the last glacial between ~32 and ~15 kyr BP. However, modern cases from northern Siberia, ca. 750 km north of Lake Billyakh, demonstrate that individual larch plants can grow within shrub and grass tundra landscape in very low mean July temperatures of about 8 °C. This makes plausible our hypothesis that the western and southern foreland of the Verkhoyansk Mountains could provide enough moist and warm microhabitats and allow individual larch specimens to survive climatic extremes of the last glacial. Reconstructed mean values of precipitation are about 270 mm/yr during the last glacial interval. This value is almost 100 mm higher than modern averages reported for the extreme-continental north-eastern Siberia east of Lake Billyakh, where larch-dominated cold deciduous forest grows at present. This suggests that last glacial environments around Lake Billyakh were never too dry for larch to grow and that the summer warmth was the main factor, which limited tree growth during the last glacial interval. The n-alkane analysis of the Siberian plants presented in this study demonstrates rather complex alkane distribution patterns, which challenge the interpretation of the fossil records. In particular, extremely low n-alkane concentrations in the leaves of local coniferous trees and shrubs suggest that their contribution to the litter and therefore to the fossil lake sediments might be not high enough for tracing the Quaternary history of the needleleaved taxa using the n-alkane biomarker method.

Mecanismos implicados en las etapas iniciales de infección en la cancrosis de los cítricos provocada por Xanthomonas citri subsp. citri

La cancrosis o chancro bacteriano de los cítricos (CBC) causada por Xanthomonas citri subsp. citri (Xcc) y X. fuscans subsp. aurantifolii, afecta a un gran número de especies dentro de la familia de las rutáceas, especialmente cítricos. Esta enfermedad produce graves pérdidas económicas allí donde está presente, principalmente porque la comercialización de cítricos desde las zonas afectadas hacía zonas libres de cancrosis, está sujeta a fuertes medidas cuarentenarias. La cancrosis se encuentra distribuida a nivel mundial pero no se ha localizado ni en la Unión Europea ni en ningún área del Mediterráneo. Se han descrito tres tipos de cancrosis en función de la gama de huésped y de las características fenotípicas y genotípicas de las bacterias que las producen. La más extendida es la cancrosis tipo A producida por Xcc, dentro de la cual se distinguen los subtipos Aw y A*, originarios de Florida y Sudeste Asiático, respectivamente, que de forma natural solo son capaces de producir enfermedad en lima mejicana. En este trabajo se presentan estudios sobre mecanismos implicados en las primeras etapas de la infección, como la quimiotaxis y formación de biopelículas, en la cancrosis de los cítricos. La quimiotaxis es el proceso por el cual las bacterias se dirigen hacia zonas favorables para su supervivencia y desarrollo. Los perfiles quimiotácticos obtenidos frente a distintas fuentes de carbono, así como los estudios en relación al contenido de proteínas aceptoras de grupos metilo (MCPs), permitieron agrupar a las cepas de Xanthomonas estudiadas en este trabajo, de acuerdo a la enfermedad producida y a su gama de huésped. Todas las cepas mostraron quimiotaxis positiva frente a extractos de hoja y apoplasto de diferentes especies, sin embargo, Xcc 306, X. alfalfae subsp. citrumelonis (Xac) y X. campestris pv. campestris (Xc) manifestaron respuestas más específicas frente a extractos de apoplasto de hojas de naranjo dulce, lima y col china, respectivamente. Dicho resultado nos permite asociar el mecanismo de quimiotaxis con la capacidad de las cepas de Xanthomonas para colonizar estos huéspedes de forma específica. Las cepas estudiadas fueron capaces de realizar movimiento tipo swimming, twitching y sliding en distintos medios, siendo el movimiento swimming el único en el que se encontraron diferencias entre las cepas de Xcc con distinta gama de huésped. En este trabajo se ha estudiado además la formación de biopelículas en superficies bióticas y abióticas, un mecanismo importante tanto para la supervivencia en superficie vegetal como para el desarrollo de la infección. Las cepas de Xanthomonas estudiadas fueron capaces de formar biopelículas in vitro, siendo mayor en un medio que simula el apoplasto y que contiene una baja concentración de nutrientes en comparación con medios que contenían alta concentración de nutrientes. La formación de biopelículas en superficie vegetal se encontró relacionada, en las cepas patógenas de cítricos, con la capacidad para infectar un tejido o huésped determinado. Se han caracterizado algunos de los componentes de la matriz extracelular producida por Xcc, que compone hasta un 90% de las bipoelículas. Entre ellos destaca el ADN extracelular, que tiene un papel como adhesina en las primeras etapas de formación de biopelículas y estructural en biopelículas maduras. Además, se han identificado el pilus tipo IV como componente importante en las biopelículas, que también participa en motilidad. Finalmente, se han realizado estudios sobre la expresión de genes implicados en motilidad bacteriana y formación de biopelículas que han confirmado las diferencias existentes entre cepas de Xcc de amplia y limitada gama de huésped, así como el papel que juegan elementos como el pilus tipo IV o el flagelo en estos procesos. ABSTRACT Xanthomonas citri subsp. citri (Xcc) and X. fuscans subsp. aurantifolii are the causal agents of Citrus Bacterial Canker (CBC) which is one of the most important citrus diseases. CBC affects all Citrus species as well as other species from Rutaceae family. CBC produces strong economic losses; furthermore the commercialization of plants and fruits is restricted from infested to citrus canker free areas. The disease is worldwide distributed in tropical and subtropical areas, however it is not present in the European Union. Three types of CBC have been described according to the host range and phenotypic and genotypic characteristics. CBC type A caused by Xcc is he widest distributed. Within CBC A type two subtypes Aw and A* were described from Florida and Iran respectively, both infecting only Mexican lime. Herein mechanisms connected to early events in the citrus bacterial canker disease such as chemotaxis and biofilm formation, were studied. Chemotaxis allows bacteria to move towards the more suitable environments for its survival, host colonization and infection. Studies performed on citrus pathogenic Xanthomonas and X. campestris pv. campestris (Xc), a crucifer pathogen, have shown different chemotactic profiles towards carbon compound as well as different MCPs profile, which clustered strains according to host range and disease caused. Every strain showed positive chemotaxis toward leaf extracts and apoplastic fluids from sweet orange, Mexican lime and Chinese cabbage leaves. However, a more specific response was found for strains Xcc 306, X. alfalfae subsp. citrumelonis and Xc towards sweet orange, Mexican lime and Chinese cabbage apoplastic fluids, respectively. These results relate chemotaxis with the higher ability of those strains to specifically colonize their proper host. Xanthomonas strains studied were able to perform swimming, sliding and twitching motilities. The ability to swim was variable among CBC strains and seemed related to host range. Biofilm formation is an important virulence factor for Xcc because it allows a better survival onto the plant surface as well as facilitates the infection process. The studied Xanthomonas strains were able to form biofilm in vitro, on both nutrient rich and apoplast mimicking media, furthermore the biofilm formation by all the strains was higher in the apoplast mimicking media. The ability to form biofilm in planta by Xcc and Xac strains was dependent of the host and the tissue colonized. The wide host range CBC strain was able to form biofilm onto several citrus leaves and fruits, however the limited host range CBC strain produced biofilm solely onto Mexican lime leaves and fruits. Furthermore Xac strain, which solely infects leaves of young plants, was not able to develop biofilms on fruits. Some components of the extracellular matrix produced by Xcc strains have been characterized. Extracellular DNA acted as an adhesin at the very early stages of biofilm formation and as structural component of mature biofilm for citrus pathogenic Xanthomonas. Furthermore type IV pilus has been identified as a component of the extracellular matrix in biofilm and motility. Transcriptional studies of genes related with biofilm formation and motility have confirmed the differential behavior found among wide and limited host range CBC strains as well as the role of type IV pili and flagellum on those processes.

An ethnopharmacological and historical analysis of “Dictamnus”, a European traditional herbal medicine

Ethnopharmacological relevance and background: “Dictamnus” was a popular name for a group of medicinal herbaceous plant species of the Rutaceae and Lamiaceae, which since the 4th century have been used for gynaecological problems and other illnesses BCE and still appear in numerous ethnobotanical records. Aims: This research has as four overarching aims: Determining the historical evolution of medical preparations labelled “Dictamnus” and the different factors affecting this long-standing herbal tradition. Deciphering and differentiating those medicinal uses of “Dictamnus” which strictly correspond to Dictamnus (Rutaceae), from those of Origanum dictamnus and other Lamiaceae species. Quantitatively assessing the dependence from herbal books, and pharmaceutical tradition, of modern Dictamnus ethnobotanical records. Determining whether differences between Western and Eastern Europe exist with regards to the Dictamnus albus uses in ethnopharmacology and ethnomedicine. Methods: An exhaustive review of herbals, classical pharmacopoeias, ethnobotanical and ethnopharmacological literature was conducted. Systematic analysis of uses reported which were standardized according to International Classification of Diseases – 10 and multivariate analysis using factorial, hierarchical and neighbour joining methods was undertaken. Results and discussion: The popular concept “Dictamnus” includes Origanum dictamnus L., Ballota pseudodictamnus (L.) Benth. and B. acetabulosa (L.) Benth. (Lamiaceae), as well as Dictamnus albus L. and D. hispanicus Webb ex Willk. (Rutaceae), with 86 different types of uses. Between 1000 and 1700 CE numerous complex preparations with “Dictamnus” were used in the treatment of 35 different pathologies. On biogeographical grounds the widespread D. albus is a far more likely prototypical “Dictamnus” than the Cretan endemic Origanum dictamnus. However both form integral parts of the “Dictamnus” complex. Evidence exists for a sufficiently long and coherent tradition for D. albus and D. hispanicus, use to treat 47 different categories of diseases. Conclusions: This approach is a model for understanding the cultural history of plants and their role as resources for health care. “Dictamnus” shows how transmission of traditional knowledge about materia medica, over 26 centuries, represents remarkable levels of development and innovation. All this lead us to call attention to D. albus and D. hispanicus which are highly promising as potential herbal drug leads. The next steps of research should be to systematically analyse phytochemical, pharmacological and clinical evidence and to develop safety, pharmacology and toxicology profiles of the traditional preparations.

Pollen analysis of surface sediments from the Gulf of Guinea and offshore NW-Africa

The areas of marine pollen deposition are related to the pollen source areas by aeolian and fluvial transport regimes, whereas wind transport is much more important than river transport. Pollen distribution patterns of Pinus, Artemisia, Chenopodiaceae-Amaranthaceae, and Asteraceae Tubuliflorae trace atmospheric transport by the northeast trades. Pollen transport by the African Easterly Jet is reflected in the pollen distribution patterns of Chenopodiaceae-Amaranthaceae, Asteraceae Tubuliflorae, and Mitracarpus. Grass pollen distribution registers the latitudinal extension of Sahel, savannas and dry open forests. Marine pollen distribution patterns of Combretaceae-Melastomataceae, Alchornea, and Elaeis reflect the extension of wooded grasslands and transitional forests. Pollen from the Guinean-Congolian/Zambezian forest and from the Sudanian/Guinean vegetation zones mark the northernmost extension of the tropical rain forest. Rhizophora pollen in marine sediments traces the distribution of mangrove swamps. Only near the continent, pollen of Rhizophora, Mitracarpus, Chenopodiaceae-Amaranthaceae, and pollen from the Sudanian and Guinean vegetation zones are transported by the Upwelling Under Current and the Equatorial Under Current, where those currents act as bottom currents. The distribution of pollen in marine sediments, reflecting the position of major climatic zones (desert, dry tropics, humid tropics), can be used in tracing climatic changes in the past.

The late Pliocene pollen record of ODP Site 108-658 off Cape Blanc, Atlantic Ocean

A 200 m long marine pollen record from ODP Site 658 (21°N, 19°W) reveals cyclic fluctuations in vegetation and continental climate in northwestern Africa from 3.7 to 1.7 Ma. These cycles parallel oxygen isotope stages. Prior to 3.5 Ma, the distribution of tropical forests and mangrove swamps reached Cape Blanc, 5°N of the present distribution. Between 3.5 and 2.6 Ma, forests occurred at this latitude during irregular intervals and nearly disappeared afterwards. Likewise, a Saharan paleoriver flowed continuously until isotope Stage 134 (3.35 Ma). When river discharge ceased, wind transport of pollen grains prevailed over fluvial transport. Pollen indicators of trade winds gradually increased between 3.3 and 2.5 Ma. A strong aridification of the climate of northwestern Africa occurred during isotope Stage 130 (3.26 Ma). Afterwards, humid conditions reestablised followed by another aridification around 2.7 Ma. Repetitive latitudinal shifts of vegetation zones ranging from wooded savanna to desert flora dominated for the first time between between 2.6 and 2.4 Ma as a response to the glacial stages 104, 100 and 98. Although climatic conditions, recorded in the Pliocene, were not as dry as those of the middle and Late Pleistocene, latitudinal vegetation shifts near the end of the Pliocene resembled those of the interglacial-glacial cycles of the Brunhes chron.