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Journal articles on the topic 'Alborán'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 May 2024

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1

De la Rosa Álamos, Julio, María Altamirano, and Marianela Zanolla. "Checklist of benthic marine Cyanoprokariota of Chafarinas Islands (Alboran Sea, Western Mediterranean). Catálogo de cianoprocariotas bentónicas marinas de las Islas Chafarinas (Mar de Alborán, Mediterráneo Occidental)." Acta Botanica Malacitana 38 (December 1, 2013): 182–86. http://dx.doi.org/10.24310/abm.v38i0.2619.

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Catálogo de cianoprocariotas bentónicas marinas de las Islas Chafarinas (Mar de Alborán, Mediterráneo Occidental) Keywords: Chafarinas Islands, Cyanoprokariota, marine algae, Alboran Sea. Palabras clave: Islas Chafarinas, Cyanoprokariotas, algas marinas, Mar de Alborán.

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ABDELLAOUI, BENYOUNES, FEDERICO FALCINI, TARIK BAIBAI, KARIM KARIM HILMI, OMAR ETTAHIRI, ROSALIA SANTOLERI, RACHIDA HOUSSA, HASSAN NHHALA, HASSAN ER-RAIOUI, and LAILA OUKHATTAR. "Spatial pattern of sea surface temperature and chlorophyll-a trends in relation to hydrodynamic processes in the Alborán Sea." Mediterranean Marine Science 25, no. 1 (March 22, 2024): 136–50. http://dx.doi.org/10.12681/mms.30268.

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Environmental conditions such as temperature, planktonic biomass, and ocean currents play an important role in the development and distribution of marine species. This work aims to estimate, in a high spatial resolution, the actual trends of sea surface temperature (SST) and chlorophyll-a concentration (Chl-a) and to assess the relationship with the local hydrodynamic conditions in the Alborán Sea. To investigate these objectives, time series of SST and Chl-a of satellite sensor data were analyzed during 20 years from January 2001 to December 2020, using the Seasonal-Trend-Loess (STL) decomposition method and the Mann-Kendall seasonality test. The results, obtained with a 95% of confidence, showed that the Alborán Sea basin is subject to sea surface warming evaluated at 0.027 ± 0.008 ° C per year, related to the warming of the Atlantic water mass, which contributes to a decrease of productivity evaluated at -0.0024 ± 0.0003 μg /l per year of Chl-a concentration. These trends are not homogeneous over the entire basin area but show a large regional variation between different parts of the Alborán Sea due to the hydrodynamic process of the Atlantic Jet - Western Alboran Gyre system (AJ-WAG), which is more active especially in summer/autumn seasons and contribute largely to these changes by mixing the waters of the Atlantic Ocean and the Mediterranean Sea.

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3

Meléndez-Vallejo, María José, Pedro Torres, Fernando González-Valderrama, Ana Giráldez, María González, José Luís Pérez-Gil, José Miguel Serna-Quintero, Jesús Acosta, and José Carlos Báez. "First record of intersexuality gonad anomaly in Trachurus mediterraneus (Steindachner, 1868) from Alboran Sea." Anales de Biología, no. 39 (May 15, 2017): 89–92. http://dx.doi.org/10.6018/analesbio.39.09.

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El objetivo principal de este trabajo es dar a conocer el primer registro de una anomalía intersexual gonadal de Trachurus mediterraneus desde el mar de Alborán (Mediterráneo occidental). Este espécimen es el primer registro de intersexualidad para un jurel en el mundo. The main aim of this paper is report the first cited of an intersexual gonadal anomaly of Trachurus mediterraneus from the Alboran Sea (Western Mediterranean). This specimen is the first record of intersexuality in horse mackerel in the world.

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Blanca, Gabriel, Miguel Cueto, and Victor N. Suárez-Santiago. "Sobre Anacyclus alboranensis Esteve Chueca & Varo (Asteraceae, Anthemidae)." Acta Botanica Malacitana 34 (December 1, 2009): 257–60. http://dx.doi.org/10.24310/abm.v34i0.6884.

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About Anacyclus alboranensis Esteve Chueca & Varo (Asteraceae, Anthemideae)Palabras clave. Anacyclus, nomenclatura, tipificación, isla de Alborán, Almería, España.Key words. Anacyclus, nomenclature, typification, Alborán island, Almería, Spain.

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Pérez García, Francisco J., Miguel Cueto, María L. Jiménez Sánchez, Juan A. Garrido, Fabián Martínez Hernández, José M. Medina Cazorla, María L. Rodríguez-Tamayo, Ana J. Sola, and Juan F. Mota. "Contribución al conocimiento de la flora de Andalucía: citas novedosas e interesantes de la provincia de Almería." Acta Botanica Malacitana 28 (January 1, 2003): 233–37. http://dx.doi.org/10.24310/abm.v28i0.7290.

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Contribution to the knowledge about Andalusian flora: new and interesting cites of the Almería province.Palabras clave. Corología, Isla de Alborán, sureste ibérico, xenófitas.Key words. Corology, Alborán Island, South-Eastern Iberian Peninsula, xenophytes.

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García-Lafuente, Jesús, Cristina Naranjo, Simone Sammartino, José C. Sánchez-Garrido, and Javier Delgado. "The Mediterranean outflow in the Strait of Gibraltar and its connection with upstream conditions in the Alborán Sea." Ocean Science 13, no. 2 (March 24, 2017): 195–207. http://dx.doi.org/10.5194/os-13-195-2017.

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Abstract. The present study addresses the hypothesis that the Western Alborán Gyre in the Alborán Sea (the westernmost Mediterranean basin adjacent to the Strait of Gibraltar) influences the composition of the outflow through the Strait of Gibraltar. The process invoked is that strong and well-developed gyres help to evacuate the Western Mediterranean Deep Water from the Alborán basin, thus increasing its presence in the outflow, whereas weak gyres facilitate the outflow of Levantine and other intermediate waters. To this aim, in situ observations collected at the Camarinal (the main) and Espartel (the westernmost) sills of the strait have been analysed along with altimetry data, which were employed to obtain a proxy of the strength of the gyre. An encouraging correlation of the expected sign was observed between the time series of potential temperature at the Espartel Sill, which is shown to keep information on the outflow composition, and the proxy of the Western Alborán Gyre, suggesting the correctness of the hypothesis, although the weakness of the involved signals does not allow for drawing definitive conclusions.

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7

Lyamani, H., A. Valenzuela, D. Perez-Ramirez, C. Toledano, M. J. Granados-Muñoz, F. J. Olmo, and L. Alados-Arboledas. "Aerosol properties over the western Mediterranean Basin: temporal and spatial variability." Atmospheric Chemistry and Physics Discussions 14, no. 15 (August 21, 2014): 21523–64. http://dx.doi.org/10.5194/acpd-14-21523-2014.

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Abstract. This study focuses on the analysis of AERONET aerosol data obtained over Alborán Island (35.95° N, 3.01° W, 15 m a.s.l.) in the western Mediterranean from July 2011 to January 2012. Additional aerosol data from three nearest AERONET stations and the Maritime Aerosol Network (MAN) were also analyzed in order to investigate the aerosol temporal and spatial variations over this scarcely explored region. Aerosol load over Alborán was significantly larger than that reported for open oceanic areas not affected by long-range transport. High aerosol loads over Alborán were mainly associated with desert dust transport from North Africa and occasional advection of anthropogenic fine particles from Italy. The fine particle load observed over Alborán was surprisingly similar to that obtained over the other three nearest AERONET stations in spite of the large differences in local aerosol sources. The results from MAN acquired over the Mediterranean Sea, Black Sea and Atlantic Ocean from July to November 2011 revealed a pronounced predominance of fine particles during the cruise period. Alborán was significantly less influenced by anthropogenic particles than the Black Sea and central and eastern Mediterranean regions during the cruise period. Finally, the longer AERONET dataset from Málaga (36.71° N, 4.4° W, 40 m a.s.l.), port city in southern Spain, shows that no significant changes in columnar aerosol loads since the European Directive on ship emissions was implemented in 2010 were observed over this site.

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8

Rodríguez Martínez, Jaime. "Oceanografía del Mar de Alborán." Aldaba, no. 13 (January 1, 1989): 71. http://dx.doi.org/10.5944/aldaba.13.1989.20149.

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9

Abelló, Pere, Aina Carbonell, and Pedro Torres. "Biogeography of epibenthic crustaceans on the shelf and upper slope off the Iberian Peninsula Mediterranean coasts: implications for the establishment of natural management areas." Scientia Marina 66, S2 (June 30, 2002): 183. http://dx.doi.org/10.3989/scimar.2002.66s2183.

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The patterns of occurrence and bathymetric distribution of epibenthic crustaceans on the continental shelf and upper slope down to a depth of 800 m are analysed based on data gathered during six demersal trawl surveys performed annually in spring along the Mediterranean coasts of the Iberian Peninsula (from the Straits of Gibraltar to Cape Creus) between 1994 and 1999. A total of 598 valid hauls has been studied providing a total of 108 species of decapods, two stomatopods, one euphausiid, one mysid and one isopod. The study area has been subdivided into seven sectors according to their geomorphological characteristics, and the patterns of occurrence and abundance by depth have been analysed separately for each of the sectors. Detailed data on bathymetric distribution are presented for each species. Two main biogeographical areas can be discerned along the study area, which can approximately be separated at Palos Cape: the Alborán Sea to the southwest, and the northwestern Mediterranean (Levantine and Catalan Seas) northwest of Palos Cape. The continental shelf in the Alborán Sea (the most western area of the Mediterranean) is extremely narrow whereas it is much wider in the northwestern Mediterranean. The influence of Atlantic waters entering the Mediterranean is particularly strong in the Alborán Sea which shows a particularly high species richness of Atlantic affinity. Within the context of the western Mediterranean Sea, the Alborán Sea region shows important faunistic characteristics such that it might be considered as a possible separate natural management area for demersal fisheries.

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10

Lyamani, H., A. Valenzuela, D. Perez-Ramirez, C. Toledano, M. J. Granados-Muñoz, F. J. Olmo, and L. Alados-Arboledas. "Aerosol properties over the western Mediterranean basin: temporal and spatial variability." Atmospheric Chemistry and Physics 15, no. 5 (March 5, 2015): 2473–86. http://dx.doi.org/10.5194/acp-15-2473-2015.

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Abstract. This study focuses on the analysis of Aerosol Robotic Network (AERONET) aerosol data obtained over Alborán Island (35.90° N, 3.03° W, 15 m a.s.l.) in the western Mediterranean from July 2011 to January 2012. Additional aerosol data from the three nearest AERONET stations (Málaga, Oujda and Palma de Mallorca) and the Maritime Aerosol Network (MAN) were also analyzed in order to investigate the temporal and spatial variations of aerosol over this scarcely explored region. High aerosol loads over Alborán were mainly associated with desert dust transport from North Africa and occasional advection of anthropogenic fine particles from central European urban-industrial areas. The fine particle load observed over Alborán was surprisingly similar to that obtained over the other three nearest AERONET stations, suggesting homogeneous spatial distribution of fine particle loads over the four studied sites in spite of the large differences in local sources. The results from MAN acquired over the Mediterranean Sea, Black Sea and Atlantic Ocean from July to November 2011 revealed a pronounced predominance of fine particles during the cruise period.

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11

Conde, Francisco, and Antonio Flores-Moya. "Nuevas adiciones al conocimiento de las macroalgas marinas de la isla de Alborán (Mediterráneo Occidental)." Acta Botanica Malacitana 25 (December 1, 2000): 180–84. http://dx.doi.org/10.24310/abm.v25i0.8484.

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12

Morales Lomas, Francisco. "Reseña de AA. VV. (2020): Mar de Alborán. Antología de la poesía contemporánea andaluza y marroquí." Analecta Malacitana. Revista de la sección de Filología de la Facultad de Filosofía y Letras 41 (July 24, 2021): 321–25. http://dx.doi.org/10.24310/analecta.v41i.13071.

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13

Casimiro-Soriguer Solanas, Federico, Noelia Hidalgo Triana, Manuel Zafra, and Andrés Vicente Pérez Latorre. "Nuevas citas de interés para la flora vascular terrestre del litoral ibérico del mar de Alborán (Andalucía, España)." Acta Botanica Malacitana 47 (March 24, 2022): 77–81. http://dx.doi.org/10.24310/abm.v47i.14240.

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14

Muñoz, A., M. Ballesteros, I. Montoya, J. Rivera, J. Acosta, and E. Uchupi. "Alborán Basin, southern Spain—Part I: Geomorphology." Marine and Petroleum Geology 25, no. 1 (January 2008): 59–73. http://dx.doi.org/10.1016/j.marpetgeo.2007.05.003.

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15

Serrano, M. A., M. Díez-Minguito, M. Ortega-Sánchez, and M. A. Losada. "Continental shelf waves on the Alborán sea." Continental Shelf Research 111 (December 2015): 1–8. http://dx.doi.org/10.1016/j.csr.2015.11.004.

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16

Altamirano, María, Julio De la Rosa, Monia Flagella, and Marianela Zanolla. "Contributions to the benthic marine flora of Chafarinas Islands (Alboran Sea, Western Mediterranean). Contribuciones a la flora marina bentónica de las Islas Chafarinas (Mar de Alborán, Mediterráneo Occidental)." Acta Botanica Malacitana 38 (December 1, 2013): 187–91. http://dx.doi.org/10.24310/abm.v38i0.2614.

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Contribuciones a la flora marina bentónica de las Islas Chafarinas (Mar de Alborán, Mediterráneo Occidental)Key words. Chafarinas Islands, geographical distribution, Mediterranean Sea, seaweeds.Palabras clave. Islas Chafarinas, corología, macroalgas marinas, Mediterráneo.

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Altamirano, María, Julio De la Rosa, Marianela Zanolla, Virginia Souza-Egipsy, and Javier Díaz. "New records for the benthic marine flora of Chafarinas Islands (Alboran Sea, western Mediterranean). Nuevas citas para la flora bentónica marina de las Islas Chafarinas (Mar de Alborán, Mediterráneo occidental)." Acta Botanica Malacitana 35 (December 1, 2010): 165–67. http://dx.doi.org/10.24310/abm.v35i0.2861.

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Nuevas citas para la ﬂ ora bentónica marina de las Islas Chafarinas (Mar de Alborán, Mediterráneo occidental) Keywords. Chafarinas Islands, geographical distribution, Mediterranean Sea, seaweeds. Palabras clave. Islas Chafarinas, corología, macroalgas marinas, Mediterráneo.

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18

Reina-Hervás, J. A., J. E. García Raso, and M. E. Manjón-Cabeza. "First record of Sphoeroides spengleri (Osteichthyes: Tetraodontidae) in the Mediterranean Sea." Journal of the Marine Biological Association of the United Kingdom 84, no. 5 (October 2004): 1089–90. http://dx.doi.org/10.1017/s0025315404010495h.

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The capture of a specimen of Sphoeroides spengleri (Osteichthyes: Tetraodontidae), 17 December 2000 and 29·7 mm total length, from the Málaga coast (Alborán Sea, western Mediterranean) represents the first record of a new alien species for Mediterranean waters.

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Fernandez de Puelles, Maria Luz, Magdalena Gazá, Miguel Cabanellas-Reboredo, and Todd D. O’Brien. "Decadal Trends in the Zooplankton Community of the Western Mediterranean." Water 15, no. 24 (December 13, 2023): 4267. http://dx.doi.org/10.3390/w15244267.

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Decadal trends in the zooplankton community were seasonally investigated in multiple monitoring transects of the western Mediterranean Sea during a period of increasing and record-high water temperatures. The transition area around the Baleares archipelago can be separated into two regions: the Alborán Sea and the Balearic Sea. Differences were found in the abundance and structure of the dominant zooplankton groups: the cladocerans and copepods. The highest zooplankton abundances were found during the stratified summer season, when cladoceran numbers peaked. However, copepods were more abundant during the winter. A marked seasonality was found in all groups and the dominant taxa: 114 species of copepods and 5 species of cladocerans were identified, but less than 8 species of copepods and 2 species of cladocerans dominated the populations. During the 2007–2017 study, warm and salty waters were observed in the Balearic Sea. In the Alborán Sea, cool and fresh waters were observed, along with a decline in chlorophyll. Irregular group and species trends were observed in both regions, exhibiting both increases and decreases depending on region and season. Trends differed, often oppositely, for the Alborán versus the Balearic Sea, with the transition region between them mirroring one or the other, switching with the seasons. The most dominant species, including Penilia avirostris and Clausocalanus arcuicornis, but also Evadne spinifera, C. lividus, C. furcatus, Paracalanus parvus, Acartia clausi, Centropages typicus, Subeucalanus monachus, and Calanus helgolandicus, are proposed as biological tracers to be used in further studies on climate and zooplankton community changes in the western Mediterranean Sea.

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Vélez-Belchı́, P., M. Vargas-Yáñez, and J. Tintoré. "Observation of a western Alborán gyre migration event." Progress in Oceanography 66, no. 2-4 (August 2005): 190–210. http://dx.doi.org/10.1016/j.pocean.2004.09.006.

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21

Periáñez, R. "Modelling radioactivity dispersion in the Alborán Sea, western Mediterranean." Radioprotection 44, no. 5 (2009): 5–10. http://dx.doi.org/10.1051/radiopro/20095008.

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Tintoré, Joaquín, Damià Gomis, Sergio Alonso, and Gregorio Parrilla. "Mesoscale Dynamics and Vertical Motion in the Alborán Sea." Journal of Physical Oceanography 21, no. 6 (June 1991): 811–23. http://dx.doi.org/10.1175/1520-0485(1991)021<0811:mdavmi>2.0.co;2.

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Periáñez, R. "Modelling surface radioactive spill dispersion in the Alborán Sea." Journal of Environmental Radioactivity 90, no. 1 (January 2006): 48–67. http://dx.doi.org/10.1016/j.jenvrad.2006.06.009.

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Peñas de Giles, Julio, Jesús Del Río Sánchez, Luis Sánchez Tocino, and Antonio De la Linde Rubio. "Primera cita de la especie invasora Caulerpa cylindracea Sonder en las islas Chafarinas (África del Norte)." Acta Botanica Malacitana 45 (May 13, 2020): 157–59. http://dx.doi.org/10.24310/abm.v45i.6781.

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Las Islas Chafarinas constituyen una importante área de biodiversidad en el Mar de Alborán (Mediterráneo occidental) que se encuentra bajo protección. Presentamos un nuevo registro de presencia de Caulerpa cylindracea para las islas, un taxón invasor agresivo y de rápida expansión introducido en el mar Mediterráneo hace unos años. Alertamos sobre una posible invasión en esta importante reserva marina.

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Cartes, Joan E., Pere Abelló, and Pedro Torres. "The occurrence of Hymenopenaeus debilis (Decapoda: Aristeidae: Solenocerinae) in Mediterranean waters: a case of pseudopopulations of Atlantic origin?" Journal of the Marine Biological Association of the United Kingdom 80, no. 3 (June 2000): 549–50. http://dx.doi.org/10.1017/s0025315400002277.

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The occurrence of the aristeid shrimp Hymenopenaeus debilis in the Mediterranean Sea is reported from two individuals collected in the Alborán Sea and off Eivissa (western Mediterranean) from depths of 668-679 and 1109-1140 m, respectively. Comments on the origin of the populations and biogeography of the species are related to the Mediterranean pseudopopulations hypothesis.

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Cartes, Joan E., Pere Abelló, Domènec Lloris, Aina Carbonell, Pedro Torres, Francesc Maynou, and Luis Gil de Sola. "Feeding guilds of western Mediterranean demersal fish and crustaceans: an analysis based in a spring survey." Scientia Marina 66, S2 (June 30, 2002): 209. http://dx.doi.org/10.3989/scimar.2002.66s2209.

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The MEDITS-99 sampling was performed along all the Iberian Peninsula coasts of the western Mediterranean (from the Alborán Sea to Cape Creus) in a space-scale of 1000 Km N-S, at depths ranging between 27-790 m. Fish and decapod crustaceans were dominant in the megafaunal compartment sampled by trawling. Based on both the fish and the decapod crustacean compositions, a comparison of trophic guilds has been attempted, with fish and decapods classified as: 1) migrator macroplankton feeders (mM), 2) non-migrator macroplankton feeders (nmM), 3) nektobenthos-suprabenthos feeders (NS), 4) epibenthos feeders (Epib), 5) large detritus-scavengers (Sca), 6) infaunal feeders (Inf), 7) deposit feeders (Dep) and 8) small detritivorous feeders (Det). Multivariate techniques showed the following differences in the trophodynamics of the megafaunal assemblages along the coasts of the Iberian Peninsula: 1) crustaceans (mainly decapods) have different trophic structures on the shelf and on the slope; 2) on the slope, fish exhibited more clear changes as a function of the geographical gradient than crustaceans; and 3) trophodynamics of bathyal fish showed some geographic variations between the Alborán Sea, the Catalano-Balearic Basin, and the Algerian Basin (Vera Gulf and Alicante sectors), with a progressive north-south increase in planktophagous species.

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Camiñas, Juan Antonio, José Carlos Báez, Enrique Ayllón, Adolfo Marco, Luis Hernández-Sastre, María Isabel López, Helena Moreno, et al. "Conservation status of sea turtles in Spain (review of the period 2013-2018)." Anales de Biología, no. 43 (December 15, 2021): 175–98. http://dx.doi.org/10.6018/analesbio.43.17.

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El presente documento revisa la situación y aporta nuevos datos para las tortugas marinas en España durante el periodo 2013-2018. Se revisa el estado de conservación para el periodo 2013-2018 en cada una de las demarcaciones marítimas españolas: Levante –Baleares y Estrecho-Alborán para el Mediterráneo, y Noratlántica, Sudatlántica y Macaronesia en aguas del océano Atlántico. Se incluyen análisis de tendencias, las presiones y amenazas que afectan a cada especie y bibliografía actualizada. Para Caretta caretta, se recopila la información de los nidos en las costas mediterráneas españolas desde 2013 hasta 2018 y los movimientos de juveniles nacidos en España, tras su liberación. This document reviews the situation and provides new data for sea turtles in Spain during the period 2013-2018. The conservation status for such period is reviewed in each of the Spanish maritime demarcations: Levante -Baleares and Estrecho-Alborán for the Mediterranean, and Noratlántica, Sudatlántica and Macaronesia in waters of the Atlantic Ocean. Analysis of trends, pressures and threats that affect each species and updated bibliography are included. For Caretta caretta, information is collected on nests on the Spanish Mediterranean coasts from 2013 to 2018 and the movements of juveniles born in Spain, after their release.

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Coleman, David. "Of Corsairs, Converts and Renegades: Forms and Functions of Coastal Raiding on Both Sides of the Far Western Mediterranean, 1490-1540." Medieval Encounters 19, no. 1-2 (2013): 167–92. http://dx.doi.org/10.1163/15700674-12342128.

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Abstract Historians have long debated whether or not the cultures of the Mediterranean constitute a singular unit of geo-historical analysis. The Alborán Sea—the Mediterranean’s far western corner that narrowly separates the Iberian Peninsula from Africa’s northwestern shore—has long been an important “frontier” zone in which arguments for and against Mediterranean unity are put to the test. This essay contends that endemic practices of corsair activity and coastal raiding played analogous functions on both sides of this “frontier” in the late fifteenth and early sixteenth centuries. While the fact of systematized conflict in the form of raids lends some support to the notion of an enduring “clash of civilizations,” the parallel forms and functions of such raiding within the societies from which the corsairs came argue at least as persuasively for a significant degree of fundamental similarity and continuity. The Alborán corsairs along both coasts, for instance, typically received patronage and organizational aid from local and regional elites, and their raiding activities proved central to both economies. On both sides of the frontier, moreover, the world of the corsairs allowed a surprising degree of mobility and participation to converts and renegades of Muslim, Jewish and Christian origin alike.

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González Donoso, José María, Isabel María González Padilla, and Paul Palmqvist. "Contribución al conocimiento de la paleoceanografía del Mar de Alborán (Mediterráneo Occidental) mediante el estudio de los foraminíferos planctónicos de un testigo de sondeo." Spanish Journal of Palaeontology 6, no. 2 (August 11, 2022): 191. http://dx.doi.org/10.7203/sjp.25060.

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Se estudia la fauna de foraminíferos planctónicos de un sondeo en materiales cuaternarios localizado en el mar de Alborán (Mediterráneo occidental), los más antiguos de los cuales alcanzan una edad algo superior a los 10.500 a. A. P. La inspección visual, el análisis de grupos y el análisis factorial en modo Q permiten establecer la existencia de tres grupos de especies. El primero, que incluye Globorotalia inflata (d'Orbigny), Globigerina bulloides d'Orbigny y Globorotalia truncatulinoides d'Orbigny, es un tanto artificial. El segundo integra Neogloboquadrina pachyderma (Ehrenberg), Neogloboquadrina dutertrei (d'Orbigny), las formas intermedias entre N. pachyderma y N. dutertrei, y Globigerina quinqueloba Natland. El tercero esta formado por Globigerinoides ruber (d'Orbigny). Los resultados de las funciones de transferencia y los diagramas TS permiten inferir un cambio paleoceanográfco, consistente en un aumento, con dos oscilaciones importantes, de la temperatura y la salinidad de las aguas superficiales del mar de Alborán durante el intervalo de tiempo comprendido entre 10.500 y 7.000 a. A. P. Ahora bien, algunos de los cambios en la abundancia relativa de las especies más importantes no son siempre correlativos con estos cambios paleoceanográficos y para explicarlos se debe tener en cuenta la intervención de otros factores, tales como la productividad y la estratificación de las aguas.

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ZECK, H. P., and M. J. WHITEHOUSE. "Pre-eruptional magmatic zircon, Neogene Alborán volcanic province, SE Spain." Journal of the Geological Society 159, no. 4 (July 2002): 343–46. http://dx.doi.org/10.1144/0016-764901-117.

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31

Sammartino, M., A. Di Cicco, S. Marullo, and R. Santoleri. "Spatio-temporal variability of micro-, nano- and pico-phytoplankton in the Mediterranean Sea from satellite ocean colour data of SeaWiFS." Ocean Science 11, no. 5 (September 25, 2015): 759–78. http://dx.doi.org/10.5194/os-11-759-2015.

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Abstract. The seasonal and year-to-year variability of the phytoplankton size class (PSC) spatial distribution has been examined in the Mediterranean Sea by using the entire time series of Sea-viewing Wide Field-of-view Sensor (SeaWiFS) space observations (1998–2010). Daily maps of PSCs have been determined using an empirical model based on a synoptic relationship between surface chlorophyll a and diagnostic pigments referred to different taxonomic groups. The analysis of micro-, nano- and pico-phytoplankton satellite time series (1998–2010) describes, quantitatively, the algal assemblage structure over the basin and reveals that the main contribution to chlorophyll a in most of the Mediterranean Sea comes from the pico-phytoplankton component, especially in nutrient-poor environments. Regions with different and peculiar features are the Northwestern Mediterranean Sea, the Alborán Sea and several coastal areas, such as the North Adriatic Sea. In these areas, local interactions between physical and biological components modulate the composition of the three phytoplankton size classes. It results that, during the spring bloom season, micro-phytoplankton dominates in areas of intense vertical winter mixing and deep/intermediate water formation, while in coastal areas micro-phytoplankton dominates in all seasons because of the nutrient supply from the terrestrial inputs. In the Alborán Sea, where the Atlantic inflow modulates the nutrient availability, any predominance of one class over the other two has been observed. The nano-phytoplankton component instead remains widespread over the entire basin along the year, and its contribution to chlorophyll a is of the order of 30–40 %. The largest inter-annual signal occurs in the Northwestern Mediterranean Sea, driven by the year-to-year variation in intensity and extension of the spring bloom, followed by the Alborán Sea, in which the inter-annual variability is strongly modulated by the Atlantic inflow. In absence of sufficient in situ data of community composition, the satellite-based analysis demonstrated that pico-, nano- and micro-phytoplankton classes often coexist. The predominance of one group over the other ones is strongly dependent on the physical and biological processes occurring at the mesoscale. These processes directly influence the nutrient and light availability, which are the principal forcing for the algae growth.

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32

Salvo Tierra, Enrique, Ignacio José Melero-Jiménez, José García-Sánchez, José Carlos Báez, and Antonio Flores-Moya. "Biogeografía analítica de la pteridoflora del Arco de Alborán: Consecuencias para su status de protección." Acta Botanica Malacitana 45 (June 28, 2020): 47–65. http://dx.doi.org/10.24310/abm.v45i.7743.

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Se ha analizado la pteridoflora del Arco de Alborán mediante la aplicación de índices pteridoflorísticos y su correlación con variables ambientales. Asimismo se han realizado análisis de agrupamiento de taxones para definir corotipos y de componentes principales para delimitar unidades pteridogeográficas. Con todos estos datos se realiza un análisis de conservación de taxones amenazados y se valora desde un punto de vista territorial la posible declaración del área de estudio con alguna figura de protección especial.

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33

Salvo Tierra, Enrique, Ignacio José Melero-Jiménez, José García-Sánchez, José Carlos Báez, and Antonio Flores-Moya. "Biogeografía analítica de la pteridoflora del Arco de Alborán: Consecuencias para su status de protección." Acta Botanica Malacitana 45 (June 28, 2020): 47–65. http://dx.doi.org/10.24310/abm.v45i.7743.

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Se ha analizado la pteridoflora del Arco de Alborán mediante la aplicación de índices pteridoflorísticos y su correlación con variables ambientales. Asimismo se han realizado análisis de agrupamiento de taxones para definir corotipos y de componentes principales para delimitar unidades pteridogeográficas. Con todos estos datos se realiza un análisis de conservación de taxones amenazados y se valora desde un punto de vista territorial la posible declaración del área de estudio con alguna figura de protección especial.

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34

CASTELLÓ, JOSÉ. "The genus Limnoria (Limnoriidae, Isopoda, Crustacea) in Europe, including a key to species." Zootaxa 2968, no. 1 (July 18, 2011): 1. http://dx.doi.org/10.11646/zootaxa.2968.1.1.

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A new species of Limnoria inhabiting seaweed from the Alborán Island (western Mediterranean) is described. This is the seventh record of the genus from European coasts. L. turae n. sp. is mainly distinguished by the unique dorsal sculpture of its pleotelson, with 3 pairs of longitudinal carina without puncta, and the absence of the mandibular rasp. L. carinata is redescribed from a neotype. A key to European species is provided, and two comparative tables of the European species are included.

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35

Morales, J., I. Serrano, A. Jabaloy, J. Galindo-Zaldívar, D. Zhao, F. Torcal, F. Vidal, and F. González Lodeiro. "Active continental subduction beneath the Betic Cordillera and the Alborán Sea." Geology 27, no. 8 (1999): 735. http://dx.doi.org/10.1130/0091-7613(1999)027<0735:acsbtb>2.3.co;2.

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36

Serrano, M. A., M. Díez-Minguito, A. Valle-Levinson, and M. Ortega-Sánchez. "Circulation in a Short, Microtidal Submarine Canyon in the Alborán Sea." Journal of Coastal Research 95, sp1 (May 26, 2020): 1531. http://dx.doi.org/10.2112/si95-295.1.

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37

Vargas-Yáñez, Manuel, Teodoro Ramírez, Dolores Cortés, Marta Sebastián, and Francisco Plaza. "Warming trends in the continental shelf of Málaga Bay (ALBORÁN SEA)." Geophysical Research Letters 29, no. 22 (November 2002): 39–1. http://dx.doi.org/10.1029/2002gl015306.

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38

Fletcher, W. J., M. F. Sanchez Goñi, O. Peyron, and I. Dormoy. "Abrupt climate changes of the last deglaciation detected in a western Mediterranean forest record." Climate of the Past Discussions 5, no. 1 (January 20, 2009): 203–35. http://dx.doi.org/10.5194/cpd-5-203-2009.

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Abstract. Evidence for abrupt changes in western Mediterranean climate between 20 and 6 cal ka BP is examined in marine core MD95-2043 (Alborán Sea), using pollen data for temperate Mediterranean forest development and pollen-based climate reconstructions using the modern analogue technique (MAT) for annual precipitation (Pann) and mean temperatures of the coldest and warmest months (MTCO and MTWA). Major climatic shifts with parallel temperature and precipitation changes occurred at the onsets of Heinrich Event 1 (equivalent to the Oldest Dryas), the Bölling-Allerød (BA), and the Younger Dryas (YD). Multi-centennial-scale oscillations in forest development related to regional precipitation (Pann) variability occurred throughout the BA, YD, and early Holocene, with drier atmospheric conditions in phase with Lateglacial events of high-latitude cooling including GI-1d (Older Dryas), GI-1b (Intra-Allerød Cold Period) and GS-1 (YD), and during Holocene events associated with high-latitude cooling, meltwater pulses and N. Atlantic ice-rafting (events at 11.4, 10.1, 9.3, 8.2 and 7.4 cal ka BP). The forest record also indicates multi-centennial variability within the YD interval and multiple Preboreal climate oscillations. A possible climatic mechanism for the recurrence of dry intervals and an opposed regional precipitation pattern with respect to western-central Europe relates to the dynamics of the jet stream and the prevalence of atmospheric blocking highs. Comparison of radiocarbon and ice-core ages for well-defined climatic transitions in the forest record suggests possible enhancement of marine reservoir ages in the Alborán Sea by ~200 years (surface water age ~600 years) during the Lateglacial.

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Booth-Rea, G., C. R. Ranero, J. M. Martínez-Martínez, and I. Grevemeyer. "Crustal types and Tertiary tectonic evolution of the Alborán sea, western Mediterranean." Geochemistry, Geophysics, Geosystems 8, no. 10 (October 2007): n/a. http://dx.doi.org/10.1029/2007gc001639.

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40

Duggen, S., K. Hoernle, A. Klügel, J. Geldmacher, M. Thirlwall, F. Hauff, D. Lowry, and N. Oates. "Geochemical zonation of the Miocene Alborán Basin volcanism (westernmost Mediterranean): geodynamic implications." Contributions to Mineralogy and Petrology 156, no. 5 (April 20, 2008): 577–93. http://dx.doi.org/10.1007/s00410-008-0302-4.

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41

Paracuellos, Mariano, and Diego Jerez. "A comparison of two seabird communities on opposite coasts of the Alborán Sea (western Mediterranean)." Scientia Marina 67, S2 (July 30, 2003): 117–23. http://dx.doi.org/10.3989/scimar.2003.67s2117.

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42

PRADO, AINHOA, and GUILLERMO SAN MARTÍN. "Syllidae (Annelida) from the Alborán Sea (Western Mediterranean), with the description of a new species of Paraehlersia San Martín, 2003." Zootaxa 5437, no. 1 (April 11, 2024): 87–104. http://dx.doi.org/10.11646/zootaxa.5437.1.5.

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A list of 35 species of Syllidae (Annelida) is reported from sublittoral bottoms (from 42 to 169 m) in the Alborán Sea (Western Mediterranean), together with the description of a new species (Paraehelersia pamelae n. sp.), including original drawings and SEM photos. The new species is characterized by its small size, compound chaetae of posterior segments with short, bidentate falcigers, with both teeth similar, the proximal tooth only slightly longer than the distal one, long spiniger-like chaetae all along body, and dorsal simple chaetae distally bifid. Finally, we compare this new species with all previously known species of Paraehlersia and provide a dichotomous key.

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43

Renault, L., T. Oguz, A. Pascual, G. Vizoso, and J. Tintore. "Surface circulation in the Alborán Sea (western Mediterranean) inferred from remotely sensed data." Journal of Geophysical Research: Oceans 117, no. C8 (August 2012): n/a. http://dx.doi.org/10.1029/2011jc007659.

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44

Sicard, Michaël, Rubén Barragan, François Dulac, Lucas Alados-Arboledas, and Marc Mallet. "Aerosol optical, microphysical and radiative properties at regional background insular sites in the western Mediterranean." Atmospheric Chemistry and Physics 16, no. 18 (September 28, 2016): 12177–203. http://dx.doi.org/10.5194/acp-16-12177-2016.

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Abstract. In the framework of the ChArMEx (the Chemistry-Aerosol Mediterranean Experiment; http://charmex.lsce.ipsl.fr/) program, the seasonal variability of the aerosol optical, microphysical and radiative properties derived from AERONET (Aerosol Robotic Network; http://aeronet.gsfc.nasa.gov/) is examined in two regional background insular sites in the western Mediterranean Basin: Ersa (Corsica Island, France) and Palma de Mallorca (Mallorca Island, Spain). A third site, Alborán (Alborán Island, Spain), with only a few months of data is considered for examining possible northeast–southwest (NE–SW) gradients of the aforementioned aerosol properties. The AERONET dataset is exclusively composed of level 2.0 inversion products available during the 5-year period 2011–2015. AERONET solar radiative fluxes are compared with ground- and satellite-based flux measurements. To the best of our knowledge this is the first time that AERONET fluxes are compared with measurements at the top of the atmosphere. Strong events (with an aerosol optical depth at 440 nm greater than 0.4) of long-range transport aerosols, one of the main drivers of the observed annual cycles and NE–SW gradients, are (1) mineral dust outbreaks predominant in spring and summer in the north and in summer in the south and (2) European pollution episodes predominant in autumn. A NE–SW gradient exists in the western Mediterranean Basin for the aerosol optical depth and especially its coarse-mode fraction, which all together produces a similar gradient for the aerosol direct radiative forcing. The aerosol fine mode is rather homogeneously distributed. Absorption properties are quite variable because of the many and different sources of anthropogenic particles in and around the western Mediterranean Basin: North African and European urban areas, the Iberian and Italian peninsulas, most forest fires and ship emissions. As a result, the aerosol direct forcing efficiency, more dependent to absorption than the absolute forcing, has no marked gradient.

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Cesare, B., and M. T. Gómez-Pugnaire. "Crustal melting in the alborán domain: constraints from xenoliths of the Neogene Volcanic Province." Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy 26, no. 4-5 (April 2001): 255–60. http://dx.doi.org/10.1016/s1464-1895(01)00053-9.

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46

Periáñez, R. "Chemical and oil spill rapid response modelling in the Strait of Gibraltar–Alborán Sea." Ecological Modelling 207, no. 2-4 (October 2007): 210–22. http://dx.doi.org/10.1016/j.ecolmodel.2007.04.033.

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47

Werner, Francisco E., Alán Cantos-Figuerola, and Gregorio Parrilla. "A Sensitivity Study of Reduced-Gravity Channel Flows with Application to the Alborán Sea." Journal of Physical Oceanography 18, no. 2 (February 1988): 373–83. http://dx.doi.org/10.1175/1520-0485(1988)018<0373:assorg>2.0.co;2.

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Periáñez, R. "A modelling study on 137Cs and 239,240Pu behaviour in the Alborán Sea, western Mediterranean." Journal of Environmental Radioactivity 99, no. 4 (April 2008): 694–715. http://dx.doi.org/10.1016/j.jenvrad.2007.09.011.

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Periáñez, R. "Models for radioactivity dispersion assessments in Andalusian coastal waters: Gulf of Cádiz and Alborán Sea." Radioprotection 44, no. 5 (2009): 17–22. http://dx.doi.org/10.1051/radiopro/20095010.

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Navarro, Gabriel, Águeda Vázquez, Diego Macías, Miguel Bruno, and Javier Ruiz. "Understanding the patterns of biological response to physical forcing in the Alborán Sea (western Mediterranean)." Geophysical Research Letters 38, no. 23 (December 2011): n/a. http://dx.doi.org/10.1029/2011gl049708.

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