Characterisation of Sierra Morena citrus blossom honey (Citrus sp)

2010 ◽  
Vol 45 (10) ◽  
pp. 2008-2015 ◽  
Author(s):  
Inmaculada Rodriguez ◽  
Serrano Salud ◽  
Galán Hortensia ◽  
Ubera José Luis ◽  
Manuela Jodral
Keyword(s):  
2010 ◽  
Vol 6 (3) ◽  
Author(s):  
José María Gil-Sánchez ◽  
Miguel Angel Simón ◽  
Rafael Cadenas ◽  
José Bueno ◽  
Manuel Moral ◽  
...  

2007 ◽  
Vol 81 (4) ◽  
pp. 377-380 ◽  
Author(s):  
Javier Millán ◽  
Joan Carles Casanova

AbstractFive critically endangered Iberian lynxes (Lynx pardinus) and 35 other sympatric carnivores (19 feral catsFelis catus, 12 Egyptian mongoosesHerpestes ichneumon, and 4 common genetsGenetta genetta) were analysed for helminths in Sierra Morena and Doñana area (southern Spain).Ancylostoma tubaeforme, which was believed to be harmful for lynx cubs according to a previous study, was present in the only lynx and in 53% of cats analysed in Doñana (80% in adult cats). Other species shared in both areas wereToxocara cati(1 lynx, 31% of cats),Joyeuxiella pasqualei(1 lynx, 21% of cats) andMesocestoidessp. (2 lynxes, 5% of cats). Only one mongoose was parasitized, harbouring larvae of two acantocephalan species not previously reported in the Iberian peninsula (Centrorhynchus(Sphaerirostris)lanceaandCentrorhynchus(Longirostris)undulatus). Feral cats may be a reservoir for hookworms and other helminths affecting the Iberian lynx. In contrast, mongooses and genets may not play a role in the epidemiology of these species.


Author(s):  
J. H. Collins
Keyword(s):  

The great pyrites masses of the Sierra Morena, of which those worked at Rio Tinto are by far the most extensive, may be briefly described as contact deposits, which differ from such as are ordinarily met with only in size; and from ordinary fissure veins only in the circumstance that the cavities in which the minerals occur are bounded by dissimilar rocks.


Sendebar ◽  
2021 ◽  
Vol 32 ◽  
pp. 48-64
Author(s):  
Adolfo Hamer Flores

En la segunda mitad del siglo XVIII, impulsada por el gobierno ilustrado de Carlos III, se puso en marcha en el sur de la Península Ibérica una experiencia de colonización agraria en la que se empleó, fundamentalmente, a familias procedentes de Centroeuropa. Estos individuos, en los momentos iniciales, solo hablaban sus lenguas maternas (alemán, francés e italiano, sobre todo) por lo que la figura del intérprete de lenguas fue imprescindible para facilitar la comunicación. Sin embargo, esta función, al igual que aquellos que la desempeñaron, no ha sido estudiada hasta ahora; de ahí que nuestro objetivo en este trabajo consista en aproximarnos a la figura del intérprete en esas nuevas poblaciones durante sus primeros años de existencia.


2002 ◽  
Vol 27 ◽  
pp. 189-228 ◽  
Author(s):  
Andrés V. Pérez Latorre ◽  
Patricia Navas ◽  
David Navas ◽  
Yolanda Gil ◽  
Baltasar Cabezudo

RESUMEN. Datos sobre la flora y vegetación de la cuenca del río Guadiamar (Sevilla-Huelva, España). Sc ha realizado un estudio florístico, fitocenológico y fitogeográfico de la cuenca hidrográfica del río Guadiamar (Sevilla-Huelva, Andalucía, España). Bioclimáticamente domina en la cuenca el piso termomecliterráneo (con un reducto mesomediterráneo al NW) y el ombrotipo subhúmedo (seco al S). Se propone una sectorización fitogeográfica para la cuenca a un nivel inferior al de sector y resaltando el papel de conector de la cuenca del Guadiamar entre la provincia Luso-Extremadurense (Sierra Morena) y la Tingitano-Onubo-Algarviense (arenales y marismas). Como resultado sobre la flora, se presenta un conjunto de especies de interés por estar protegidas, por su escasez en la cuenca, en Andalucía Occidental, o por indicar determinados ecosistemas frágiles o singulares. Respecto a la vegetación, el territorio presenta una gran diversidad de asociaciones y comunidades (96), algunas de ellas son novedades sintaxonómicas: Imperato cylindricae-Scirpetum holoschoeni, Cisto salvifolii-Ulicetum australis lavanduletosum sampaianae, Malcomio trilobae-Hytnenocarpetum hamosi loeflingietosunz baeticae, Ornithopi isthmocarpi-Anthoxantetum ovati y vulpietosum alopecuroris, Ranunculo peltati-Callitrichetum brutiae y Ranunculo hederacei-Callitrichetum stagnalis. Además se lectotipifican Polypogono monspeliensis-Ranunculetum scelerati y Scolymo maculati-Sylibetum mariani. Se han catalogado 13 series de vegetación, 5 de tipo climatófilo, dominadas por fagáceas (Quercus suber y Quercus rotundtfolia) con faci aciones de Pious pinea, Olea europaea var. sylvestris o Quercus broteroi, y 8 de tipo edafohidrófi lo (caracterizadas respectivamente por Populus alba, Fraxinus angustifolia, Ulmus minor, Alnus glutinosa, Salix pedicellata, Nerium oleander, Tamariz gallica y Securinega tinctorea). Así mismo, aparecen complejos edafogénicos (mosaicos) de vegetación halófila en Entremuros (Parque Natural de Doñana) y de vegetación dulceacuícola por toda la cuenca. La vegetación permanente edafoxerófila corresponde a Genistetum polyanthi. Se presentan un esquema sintaxonómico, tablas fitosociológicas de novedades y un mapa de las series de vegetación.Palabras clave. Flora, vegetación, Fitogeografía, río Guadiamar, Sevilla, Huelva, Andalucía, España.SUMMARY. Flora and vegetation in the basin of the Guadiamar river (Seville-Huelva, Spain). We have carried out a floristical, phytocoenological and phytogeographical study about the Guadiamar river basin (Seville-Huelva, Andalusia, Spain). Thermo-mediterranean bioclimatic belt (appearing a little meso-mediterranean belt area towards NW) and sub humid ombro-type (dry towards S) characterises the basin. It is proposed a phytogeographical scheme under sector level for the Guadiamar basin. Stands out the corridor role of the Guadiamar river between the phytogeographical provinces Luso-Extremadurense (Sierra Morena) and Tingitano-Onubo- Algarviense (sandy lands and marshes). A group of species are highlighted as a result of being protected, rare in the basin or in Western Andalusia or because of living in fragile or singular ecosystems. Regarding the vegetation, a high diversity of plant communities has been found (96), some of them are new syntaxa or combinations: Impercaocylindricae-Scirpetumholoschoeni, Cisto salvifolii-Ulicetum australis lavanduletosum sampaianae, Malcomio trilobae- flymenocarpetum hamosi loeflingietosum baeticae, Ornithopi istlunocarpi-Anthoxantetum ovati and vulpietosutn alopecuroris, Ranunculo peltati-Callitrichetum brutiae, Ranunculo hederacei- Callitrichetum stagnalis. Two syntaxa are lectotypified here: Polypogono tnonspeliensis- Ranunculetum scelerati and Scolymo niaculati-Sylibetum mariani. 13 vegetation series have been recorded: 5 climactic, characterised by Quercus sober and Quercus rotundifolia showing variants with Pious pinea, Olea sylvestris or Quercus broteroi. 8 series are linked to riverside biotopes and respectively characterised by Populus alba, Fraxinus angustifolia, Ulmus minor, Alnus glutinosa, Salix pee/ice//ala, Nerium oleander, Tamarix gal lica and Securinega tinctorea. Halophytic vegetation (mosaics) is located in Entremuros near the Doilana marshes and also wetlands with hydrophilic vegetation are spread all over the basin. Soil-xeric permanent vegetation is represented by Genistetum polyanthi. A syntaxonomical scheme, phytosociological tables and one map of the vegetation series are also included.Key words. Flora, vegetation, Phytogeography, Guadiamar river basin, Seville, Huelva, Andalusia, Spain.


2019 ◽  
Vol 45 ◽  
pp. 138-153
Author(s):  
Luis Arboledas-Martínez ◽  
Eva Alarcón-García

Researchers have traditionally paid little attention to mining by Bronze Age communities in the south-east of the Iberian Peninsula. This has changed recently due to the identification of new mineral exploitations from this period during the archaeo-mining surveys carried out in the Rumblar and Jándula valleys in the Sierra Morena Mountains between 2009-2014, as well as the excavation of the José Martín Palacios mine (Baños de la Encina, Jaén). The analysis of the archaeological evidence and the archaeometric results reveal the importance of mining and metallurgical activities undertaken by the communities that inhabited the region between 2200 and 900 cal. BC, when it became one of the most important copper and silver production centers during the Late Prehistory of south-eastern Iberia.


2015 ◽  
Vol 43 ◽  
pp. 1-15 ◽  
Author(s):  
Antonia Paniza Cabrera

This paper tracks the evolution of the area covered by the dehesa in Sierra Morena from the mid 20th century to the present day, in an attempt to identify those areas in which traditional land uses still hold sway and others in which new land uses are appearing in relation to emerging business activities. These new uses have brought about an important transformation in the landscape of the dehesa, which in some areas is being replaced by other more profitable forms of land use, in particular with olive groves. In many areas where the dehesa still exists, livestock farming has been replaced by hunting, which has led to internal changes in the structure of the dehesa with an increase in scrubland. Another emerging land use is tourism-related activities, which many farmers now use to complement their income from livestock and which help preserve the traditional landscape of the dehesa.


1991 ◽  
Vol 17 (0) ◽  
pp. 37 ◽  
Author(s):  
J. Rodríguez Vidal ◽  
L. Cáceres Puro ◽  
A. Rodríguez Ramírez
Keyword(s):  

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