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Готові списки джерел за темами / Atlantic - Mediterranean suture zone / Статті в журналах

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Статті в журналах з теми "Atlantic - Mediterranean suture zone"

Автор: Grafiati

Опубліковано: 1 лютого 2023

Оновлено: 31 липня 2025

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1

PRILLO, S., J. MEHAJ, and J. PRILLO. "Other coiling changes in Globoratalia Acostaensis unknown till now in Mediterranean area." Bulletin of the Geological Society of Greece 34, no. 2 (2018): 549. http://dx.doi.org/10.12681/bgsg.17092.

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In this study, all samples from Tortonian to Early Pliocene sediments of Zvernec-Vlora and Kavaja-Durres regions within Peri-Adriatic Foredeep (PAF) of Albania containing Globorotalia acostaensis were studied qualitatively and quantitatively. Based on these analyses resulted that G. acostaensis have changed coiling ratio direction during G. acostaensis and G. obliquus extremus Zone of Tortonian, differently from that known in Mediterranean area up to now. This is not a short time interval, which more exactly is from the first appearance of G. acostaensis to first appearance of G. suterae, at t

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2

Leprêtre, Rémi, Dominique Frizon de Lamotte, Violaine Combier, Oriol Gimeno-Vives, Geoffroy Mohn, and Rémi Eschard. "The Tell-Rif orogenic system (Morocco, Algeria, Tunisia) and the structural heritage of the southern Tethys margin." BSGF - Earth Sciences Bulletin 189, no. 2 (2018): 10. http://dx.doi.org/10.1051/bsgf/2018009.

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The Tell-Rif (Tell in Algeria and Tunisia; Rif in Morocco) is the orogenic system fringing to the south the West Mediterranean basins. This system comprises three major tectonic-palaeogeographic zones from north to south: (1) the internal zones (AlKaPeCa for Alboran, Kabylies, Peloritan, Calabria) originating from the former northern European margin of the Maghrebian Tethys, (2) the “Flyschs zone” regarded as the former cover of the oceanic domain and (3) the external zones, forming the former southern Maghrebian Tethys margin more or less inverted. The Tell-Rif is interpreted as the direct re

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3

Weiss, Ronja, Zeltia Torrecilla, Enrique González-Ortegón, Ana M. González-Tizón, Andrés Martínez-Lage, and Christoph D. Schubart. "Genetic differentiation between Mediterranean and Atlantic populations of the common prawn Palaemon serratus (Crustacea: Palaemonidae) reveals uncommon phylogeographic break." Journal of the Marine Biological Association of the United Kingdom 98, no. 6 (2017): 1425–34. http://dx.doi.org/10.1017/s0025315417000492.

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The Atlantic–Mediterranean transition zone between the Alborán Sea and the Gulf of Cádiz constitutes the most prominent marine geographic barrier in European waters and includes known phylogeographic breaks such as the Strait of Gibraltar and the Almería-Oran Front. A genetic shift in this area has been previously documented for the European littoral shrimp Palaemon elegans. Here we carried out a phylogeographic analysis with the congeneric and sympatric species Palaemon serratus to test for similar intraspecific genetic differentiation and geographic structure. This littoral prawn is distribu

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4

Blanco, G., Y. J. Borrell, M. E. Cagigas, E. Vázquez, and J. A. Sánchez Prado. "Microsatellites-based genetic analysis of the Lophiidae fish in Europe." Marine and Freshwater Research 59, no. 10 (2008): 865. http://dx.doi.org/10.1071/mf08038.

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The anglerfish species Lophius piscatorius and Lophius budegassa are among the most valuable fishes sought after by bottom fisheries in western and southern European waters. It is currently believed that there are two stocks for each of the two species, north and south, which determine their assessment and management. A genetic analysis using eight polymorphic microsatellite markers was carried out on samples collected from western European waters and the south-western Mediterranean Sea. The results strongly suggest that the boundary between northern and southern stocks is not genetically supp

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5

Arntzen, Jan W., Jacob McAtear, Roland Butôt, and Iñigo Martínez-Solano. "A common toad hybrid zone that runs from the Atlantic to the Mediterranean." Amphibia-Reptilia 39, no. 1 (2018): 41–50. http://dx.doi.org/10.1163/15685381-00003145.

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We document the distribution of the common toadBufo bufoand the spined toadB. spinosusat their contact zone across France with data from a mitochondrial DNA RFLP assay, complementing similar work including nuclear markers in the northwest and southeast of France and in Italy. We also reconstruct geographical clines across the species’ contact zone in central France.Bufo bufois found in the north-eastern half of France.Bufo spinosusis found in the south-western complement. The contact zone they form runs from the Atlantic coast near Caen, France, to the Mediterranean coast near Savona, Italy, a

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6

Nofroni, Italo, Walter Renda, and Angelo Vannozzi. "Similar shells in different seas: the case of Atlantic Brachystomia carrozzai (van Aartsen, 1987) and two allied Mediterranean species (Gastropoda: Pyramidellidae)." Bollettino Malacologico 58, no. 1 (2022): 1–13. http://dx.doi.org/10.53559/bollmalacol.2021.19.

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The comparison of shells of Brachystomia carrozzai (van Aartsen, 1987) of Atlantic and Mediterranean origin allowed us to detect slight but constant morphological differences. In particular, Mediterranean specimens, here attributed to Brachystomia pizzinii n. sp., show, with respect to B. carrozzai, a more protruding and widely umbilicated protoconch, and a teleoconch with more convex whorls and clear suture. A further species with distribution limited to the waters of southern Spain, in the literature attributed to B. carrozzai as well, is described here as Brachystomia hispanica n. sp. The l

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7

Varela-Álvarez, Elena, Ana C. Balau, Núria Marbà, Julio Afonso-Carrillo, Carlos M. Duarte, and Ester A. Serrão. "Genetic diversity and biogeographical patterns of Caulerpa prolifera across the Mediterranean and Mediterranean/Atlantic transition zone." Marine Biology 162, no. 3 (2015): 557–69. http://dx.doi.org/10.1007/s00227-014-2605-5.

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8

MIFSUD, C., M. TAVIANI, and S. STOHR. "Remarks on Echinodermata from the South Central Mediterranean Sea based upon collections made during the MARCOS cruise (10 to 20th April, 2007)." Mediterranean Marine Science 10, no. 2 (2009): 63. http://dx.doi.org/10.12681/mms.109.

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The MARCOS cruise, which took place in the South Central Mediterranean Sea on board the RV ‘Urania’, resulted in the collection of 27 species of Echinodermata from shallow to bathyal depths, many from around Malta (the Fisheries Management Zone). The fauna is represented by common to rare taxa already reported from the Mediterranean with the exception of the amphi-Atlantic ophiuroid Ophiotreta valenciennesi rufescens (Koehler, 1896), recorded from the Mediterranean Basin for the first time. Odontaster mediterraneus (von Marenzeller, 1893) and Luidia sarsi Lutken, 1858 are also first records fo

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9

GARCIA RASO, J. E., F. SALMERON, J. BARO, P. MARINA, and P. ABELLO. "The tropical African hermit crab Pagurus mbizi (Crustacea, Decapoda, Paguridae) in the Western Mediterranean Sea: a new alien species or filling gaps in the knowledge of the distribution?" Mediterranean Marine Science 15, no. 1 (2013): 172. http://dx.doi.org/10.12681/mms.530.

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We report the first occurrence in the European Mediterranean Sea of a tropical Atlantic hermit crab, Pagurus mbizi (Forest, 1955), based on the capture of twenty specimens (all sizes and ovigerous females) collected along the northern shores of the Alboran Sea, which proof the existence of a well-established population of this species, and the importance of this geographic area as a transitional and settlement zone for Atlantic species, which makes the Alboran Sea one of the richest marine biodiversity areas in the Mediterranean Sea. Some morphological comparative data with the closely related

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10

Sitjà, Cèlia, Manuel Maldonado, Carlos Farias, and José L. Rueda. "Export of bathyal benthos to the Atlantic through the Mediterranean outflow: Sponges from the mud volcanoes of the Gulf of Cadiz as a case study." Deep Sea Research Part I: Oceanographic Research Papers 163 (July 25, 2020): 103326. https://doi.org/10.1016/j.dsr.2020.103326.

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ABSTRACT The Mediterranean is a semi-enclosed sea, with a narrow natural connection —the Strait of Gibraltar— through its western basin to the North Atlantic. Many studies have investigated how the inflow of North Atlantic Surface water into the Mediterranean shapes the faunal composition and abundance of the shallow-water benthic communities of the Western Mediterranean. However, the reverse effect remains little explored, that is, at what level the relatively deep (>200 m deep) outflow of Mediterranean water (MOW) exports bathyal Mediterranean benthos into the North Atlan

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11

Le Pichon, Xavier, A. M. Celâl Şengör, and Caner İmren. "A new approach to the opening of the eastern Mediterranean Sea and the origin of the Hellenic Subduction Zone. Part 1: The eastern Mediterranean Sea." Canadian Journal of Earth Sciences 56, no. 11 (2019): 1119–43. http://dx.doi.org/10.1139/cjes-2018-0128.

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We identify long transform faults that frame the eastern Mediterranean Sea and that were active during Jurassic and probably the Early Cretaceous, during the opening of the central Atlantic Ocean. We show that the African margin of the eastern Mediterranean Sea is an 1800 km long transform fault that absorbed the Africa/Eurasia Jurassic left-lateral motion during the opening of the central Atlantic. We call this transform fault the Eastern Mediterranean South Transform fault (EMST). We identify two other transform faults that were active simultaneously and framed the eastern Mediterranean Sea

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12

Bellido, Juan J., Juan J. Castillo, Francisco Pinto, et al. "Differential geographical trends for loggerhead turtles stranding dead or alive along the Andalusian coast, southern Spain." Journal of the Marine Biological Association of the United Kingdom 90, no. 2 (2009): 225–31. http://dx.doi.org/10.1017/s0025315409990361.

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Every year, an undetermined number of loggerhead turtles cross the Gibraltar Strait entering and going out of the Mediterranean Sea. An unknown percentage of them strand on the Andalusian beaches, alive or dead, with an unequal distribution along the coast. We found a geographical pattern in the density of strandings, as well as in the proportion of them that were alive and dead. Atlantic areas receive a higher number of strandings, although most of them correspond to dead individuals, especially on the west coast (province of Huelva), whereas on the Mediterranean coast there is less differenc

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13

TASKIN, E. "First report of the North Atlantic myrionematoid brown alga Ulonema rhizophorum Foslie (Phaeophyceae, Chordariaceae) in the Mediterranean Sea." Mediterranean Marine Science 14, no. 1 (2013): 125. http://dx.doi.org/10.12681/mms.330.

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The myrionematoid brown alga Ulonema rhizophorum Foslie (Phaeophyceae, Chordariaceae) is reported for the first time from the Mediterranean Sea. This species was collected growing as an epiphyte on Ulva sp. from the Dardanelles (Sea of Marmara, Turkey) in the midlittoral zone. Ulonema rhizophorum is characterized by downwardly produced rhizoids from the basal system. A key to the Mediterranean related genera of Ulonema is provided.

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14

Thieuleux, F., C. Moulin, F. M. Bréon, F. Maignan, J. Poitou, and D. Tanré. "Remote sensing of aerosols over the oceans using MSG/SEVIRI imagery." Annales Geophysicae 23, no. 12 (2005): 3561–68. http://dx.doi.org/10.5194/angeo-23-3561-2005.

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Abstract. The SEVIRI instrument on board Meteosat Second Generation (MSG) offers new capabilities to monitor aerosol transport over the Atlantic and the Mediterranean at high temporal and spatial resolutions, in particular, Saharan dust from North Africa, biomass-burning aerosols from subtropical Africa and pollution from Europe. An inversion technique was developed to estimate both aerosol optical thickness and Angström coefficients from SEVIRI measurements at 0.63 and 0.81 µm. This method relies on an optimized set of aerosol models to ensure a fast processing of full-resolution MSG images a

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15

Desboeufs, K. V., and G. Cautenet. "Transport and mixing zone of desert dust and sulphate over Tropical Africa and the Atlantic Ocean region." Atmospheric Chemistry and Physics Discussions 5, no. 4 (2005): 5615–44. http://dx.doi.org/10.5194/acpd-5-5615-2005.

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Abstract. The potentiality of dust particles to mix with sulphate over Tropical Africa and the Atlantic Ocean is investigated by combining a meso-scale meteorological model with a dust production model and an SO2 emission database. This mixing process study is based on a qualitative approach where the reactivity of dust is estimated from its calcite content, which is the main mineral known to be reactive with sulphur species. We are presenting a 1-month simulation (January 1993). Our results show that the regions Northern Egypt and Libya (NEL), Western Sahara (WS) and Sahel (S) are the major s

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16

Romero Bujan, Maria Inmaculada, and CARLOS REAL. "Morphometric characterization of Eryngium viviparum (Umbelliferae): description of a new subspecies from the Iberian Peninsula." Phytotaxa 158, no. 3 (2014): 245. http://dx.doi.org/10.11646/phytotaxa.158.3.4.

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Eryngium viviparum is an endemic plant of the Atlantic regions of Europe. Surveys carried out in recent years in the wetlands of northwest Spain have led to the identification of several previously undetected subpopulations of this species in inland areas with markedly Mediterranean bioclimatic characteristics that constitute the southern limit of this species. However, these populations overlap with the distribution of the Iberian endemic E. galioides, similar in size and morphology. We developed a biometric study on herbarium vouchers that has enabled us to identify a new subspecies, subspec

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17

Murphy, J. Brendan, James A. Braid, Cecilio Quesada, Dustin Dahn, Evan Gladney, and Nicolle Dupuis. "An eastern Mediterranean analogue for the Late Palaeozoic evolution of the Pangaean suture zone in SW Iberia." Geological Society, London, Special Publications 424, no. 1 (2015): 241–63. http://dx.doi.org/10.1144/sp424.9.

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18

Tzankov, Tzanko, and Svetla Stankova. "Morphotectonic Nature of the South Moesian Morphostructural Zone." Journal of the Bulgarian Geographical Society 43 (December 3, 2020): 75–77. http://dx.doi.org/10.3897/jbgs.2020.43.12.

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The article represents the author’s contemporary mobility concept about the morphotectonic nature of the South Moesian Morphostructural Zone in North Bulgaria. The mentioned morphounit corresponds with the Moesian Continental Microplate South Margin between Timok River to the west and Kamchia River to the east. The north boundary of the zone coincides with fault bundle system along the Lower Danube River between Timok River Infuse to the west and the town of Cherna Voda to the east and between the towns of Cherna Voda and Constantsa in Nord Dobrudzha. The south boundary of the zone is followin

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19

Tzankov, Tzanko, and Svetla Stankova. "Morphotectonic Nature of the South Moesian Morphostructural Zone." Journal of the Bulgarian Geographical Society 43 (December 3, 2020): 75–77. https://doi.org/10.3897/jbgs.2020.43.12.

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The article represents the author's contemporary mobility concept about the morphotectonic nature of the South Moesian Morphostructural Zone in North Bulgaria. The mentioned morphounit corresponds with the Moesian Continental Microplate South Margin between Timok River to the west and Kamchia River to the east. The north boundary of the zone coincides with fault bundle system along the Lower Danube River between Timok River Infuse to the west and the town of Cherna Voda to the east and between the towns of Cherna Voda and Constantsa in Nord Dobrudzha. The south boundary of the zone is followin

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20

Alberto, Filipe, Sónia Massa, Pablo Manent, et al. "Genetic differentiation and secondary contact zone in the seagrassCymodocea nodosaacross the Mediterranean-Atlantic transition region." Journal of Biogeography 35, no. 7 (2008): 1279–94. http://dx.doi.org/10.1111/j.1365-2699.2007.01876.x.

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21

Cruz-Castán, Roberto, Sámar Saber, David Macías, et al. "A possible new spawning area for Atlantic bluefin tuna (Thunnus thynnus): the first histologic evidence of reproductive activity in the southern Gulf of Mexico." PeerJ 7 (July 3, 2019): e7187. http://dx.doi.org/10.7717/peerj.7187.

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The number of studies of reproductive biology for Atlantic bluefin tuna carried out in the Gulf of Mexico is significantly lower than those undertaken in the Mediterranean Sea. Four spawning areas have been found for the eastern Atlantic bluefin tuna stock in the Mediterranean Sea, so it is not implausible that there is more than one spawning area in the Gulf of Mexico for the western Atlantic bluefin tuna stock. The individuals used in this study were caught as bycatch by the Mexican surface longline fleet between January and April 2015. A total of 63 individuals ranging between 192 and 293 c

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22

Rogerson, Mike, Yuri Dublyansky, Dirk L. Hoffmann, Marc Luetscher, Paul Töchterle, and Christoph Spötl. "Enhanced Mediterranean water cycle explains increased humidity during MIS 3 in North Africa." Climate of the Past 15, no. 5 (2019): 1757–69. http://dx.doi.org/10.5194/cp-15-1757-2019.

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Abstract. We report a new fluid inclusion dataset from northeastern Libyan speleothem SC-06-01, which is the largest speleothem fluid inclusion dataset for North Africa to date. The stalagmite was sampled in Susah Cave, a low-altitude coastal site, in Cyrenaica, on the northern slope of the Jebel Al-Akhdar. Speleothem fluid inclusions from the latest Marine Isotope Stage (MIS) 4 and throughout MIS 3 (∼67 to ∼30 kyr BP) confirm the hypothesis that past humid periods in this region reflect westerly rainfall advected through the Atlantic storm track. However, most of this moisture was sourced fro

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23

Graefe, Ulfert, and Rüdiger M. Schmelz. "Description of Enchytronia pygmaea sp. n. (Enchytraeidae, Clitellata), a very small enchytraeid in European soils." Opuscula Zoologica (Budapest) 48, S2 (2017): 3–10. https://doi.org/10.18348/opzool.2017.S2.3.

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A new and very small European species of terrestrial enchytraeids is described, Enchytronia pygmaea sp. nov. (Enchytraeidae, Oligochaeta). It differs from all enchytraeids known so far in the chaetal pattern: lateral bundles have 2 chaetae from segment II to V, 0 from segment VI to XII–XV, and only 1 chaeta in lateral postclitellar bundles; ventral bundles have 2 chaetae. A further peculiarity is the presence of only 1 pair of preclitellar nephridia. The species must be considered as widespread as it is recorded here from 17 different localities distributed over seven European countries rangin

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24

Almeida, Tiago, Luís F. Rangel, Mónica Sá, Catarina Araújo, Maria João Santos, and Sónia Rocha. "Description of Kentmoseria sirinensis n. sp. and Kentmoseria lusitanica n. comb. (Sirin et al. 2018) (Cnidaria, Myxosporea) from Common Two-Banded Seabream Diplodus vulgaris (Teleostei, Sparidae)." Journal of Marine Science and Engineering 13, no. 8 (2025): 1401. https://doi.org/10.3390/jmse13081401.

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The common two-banded seabream, Diplodus vulgaris, is a commercially important fish in the Mediterranean and eastern Atlantic, yet its myxosporean parasite diversity remains unknown. To address this gap, we conducted a myxosporean survey in D. vulgaris specimens from eastern Atlantic fishing stocks. Myxospores resembling Kentmoseria were observed in the urinary bladder of three specimens. 18S rDNA analyses, however, identified two isolates as Bipteria lusitanica, with the third also showing the highest similarity to this species. Morphological comparison revealed significant overlap between B.

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25

Domínguez-Petit, Rosario, María Rosario Navarro, Marta Cousido-Rocha, et al. "Spatial variability of life-history parameters of the Atlantic chub mackerel (Scomber colias), an expanding species in the northeast Atlantic." Scientia Marina 86, no. 4 (2022): e048. http://dx.doi.org/10.3989/scimar.05296.048.

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Atlantic chub mackerel is a pelagic species present in the Atlantic Ocean that in recent decades has expanded northwards in the eastern Atlantic. Fish samples were collected in scientific surveys and commercial catches between 2011 and 2019. We analysed the geographical variation of the biological parameters (age, length, weight and condition), as well as the length-weight relationship, maturity-at-length and spawning season onset and duration in five geographical areas (from south to north): the Canary Islands, Gulf of Cadiz, western Portuguese coast, northwestern Spanish coast and Cantabrian

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26

HALIL, Houria, and Bouteldja RICHE. "The Mediterranean World and the ‘Turk’ in Shakespeare’s Representation of the British Empire." Arab World English Journal For Translation and Literary Studies 4, no. 4 (2020): 72–83. http://dx.doi.org/10.24093/awejtls/vol4no4.6.

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This research explores Shakespeare’s representation of the so-called British Empire in its contact with other jostling empires, most notably the Ottoman Empire in the Mediterranean. To this end, four of Shakespeare’s Mediterranean plays Othello, the Moor of Venice (1603), The Merchant of Venice (1596), The Tempest (1611), and Cymbeline (1611) are taken understudy. By considering the Postcolonial historicist approach developed by literary scholars such as Stephen Greenblatt and Edward Said, the research argues that the issues of imperial relationships in Shakespeare are not solely centered on t

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27

Dauvin, Jean-Claude, and Denise Bellan-Santini. "Illustrated Key to Ampelisca Species from the North-Eastern Atlantic." Journal of the Marine Biological Association of the United Kingdom 68, no. 4 (1988): 659–76. http://dx.doi.org/10.1017/s0025315400028782.

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The genus Ampelisca comprises more than 150 species and is one of the more important benthic genus of marine amphipods. New species are regularly added (Barnard & Agard 1986; Bellan-Santini & Marques, 1986; Goeke, 1987). Ampelisca are found from the intertidal zone to abyssal depths but most of them live on the continental shelf. In spite of many studies, it is often difficult to distinguish some species which are morphologically similar. In the last ten years, twenty-two species have been described from the north-eastern Atlantic (BellanSantini & Kaïm-Malka, 1977; Bellan-Santini &

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28

Cordey, Fabrice, and Frédéric Quillévéré. "Reassessing the age of Karpathos ophiolite (Dodecanese, Greece): consequences for Aegean correlations and Neotethys evolution." Geological Magazine 157, no. 2 (2019): 263–74. http://dx.doi.org/10.1017/s0016756819000657.

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AbstractWhile the Neogene history of the Eastern Mediterranean region is now fairly well understood, our knowledge of older regional palaeogeographies is less accurate, especially the positions of blocks and nappes constituting the Aegean Islands prior to the Cenozoic. Our study focuses on the ophiolite exposed on the island of Karpathos (Dodecanese), which is located in the Aegean fore-arc at a pivotal position between the ‘western’ and ‘eastern’ ophiolites of the Mediterranean region and where conflicting Late Jurassic and Late Cretaceous ages have led to diverging tectonic and palaeogeograp

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29

Saba, V. S., M. A. M. Friedrichs, D. Antoine, et al. "An evaluation of ocean color model estimates of marine primary productivity in coastal and pelagic regions across the globe." Biogeosciences Discussions 7, no. 5 (2010): 6749–88. http://dx.doi.org/10.5194/bgd-7-6749-2010.

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Abstract. Nearly half of the earth's photosynthetically fixed carbon derives from the oceans. To determine global and region specific rates, we rely on models that estimate marine net primary productivity (NPP) thus it is essential that these models are evaluated to determine their accuracy. Here we assessed the skill of 21 ocean color models by comparing their estimates of depth-integrated NPP to 1156 in situ 14C measurements encompassing ten marine regions including the Sargasso Sea, pelagic North Atlantic, coastal Northeast Atlantic, Black Sea, Mediterranean Sea, Arabian Sea, subtropical No

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30

Saba, V. S., M. A. M. Friedrichs, D. Antoine, et al. "An evaluation of ocean color model estimates of marine primary productivity in coastal and pelagic regions across the globe." Biogeosciences 8, no. 2 (2011): 489–503. http://dx.doi.org/10.5194/bg-8-489-2011.

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Abstract. Nearly half of the earth's photosynthetically fixed carbon derives from the oceans. To determine global and region specific rates, we rely on models that estimate marine net primary productivity (NPP) thus it is essential that these models are evaluated to determine their accuracy. Here we assessed the skill of 21 ocean color models by comparing their estimates of depth-integrated NPP to 1156 in situ 14C measurements encompassing ten marine regions including the Sargasso Sea, pelagic North Atlantic, coastal Northeast Atlantic, Black Sea, Mediterranean Sea, Arabian Sea, subtropical No

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Civitarese, G., M. Gačić, M. Lipizer, and G. L. E. Borzelli. "On the impact of the Bimodal Oscillating System (BiOS) on the biogeochemistry and biology of the Adriatic and Ionian Seas (Eastern Mediterranean)." Biogeosciences Discussions 7, no. 5 (2010): 6971–95. http://dx.doi.org/10.5194/bgd-7-6971-2010.

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Abstract. Analysis of 20-year time-series of the vertically averaged salinity and nutrient data in the South Adriatic shows that the two parameters are subject to strong decadal variability. In addition, nutrient and salinity variations are out of phase. Nutrients in the Ionian and in the Adriatic vary in parallel except that often the nutrient content in the Adriatic is lower than in the Ionian, a fact that has been attributed to primary producer consumption following the winter convective mixing. Horizontal distribution of the nitracline depth in the Ionian suggests that nutrient content in

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Catarino, D., D. Stanković, G. Menezes, and S. Stefanni. "Insights into the genetic structure of the rabbitfish Chimaera monstrosa (Holocephali) across the Atlantic-Mediterranean transition zone." Journal of Fish Biology 91, no. 4 (2017): 1109–22. http://dx.doi.org/10.1111/jfb.13404.

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Ralston, Ian. "Central Gaul at the Roman Conquest: conceptions and misconceptions." Antiquity 62, no. 237 (1988): 786–94. http://dx.doi.org/10.1017/s0003598x00075232.

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Several recent reconstructions of the social and economic development of non-Mediterranean Gaul afterc. 200 BC have argued for the development of complex societies, characterized by the appearance of centralized political entities with urban – or at least urbanizing – communities. The emergence of such ‘Archaic States’ is often considered as having been restricted to a broad zone running eastward from the Atlantic façade through the northern Massif Central to the Swiss plateau. Five certain such states are usually claimed: Bituriges cubi, Aedui, Arverni, Sequani, Helvetii; and three probable:

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Civitarese, G., M. Gačić, M. Lipizer, and G. L. Eusebi Borzelli. "On the impact of the Bimodal Oscillating System (BiOS) on the biogeochemistry and biology of the Adriatic and Ionian Seas (Eastern Mediterranean)." Biogeosciences 7, no. 12 (2010): 3987–97. http://dx.doi.org/10.5194/bg-7-3987-2010.

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Abstract. Analysis of 20-year time-series of the vertically averaged salinity and nutrient data in the Southern Adriatic shows that the two parameters are subject to strong decadal variability. In addition, it is documented that nutrient and salinity variations are out of phase. Nutrients in the Ionian and in the Adriatic vary in parallel except that generally the nutrient content in the Adriatic is lower than in the Ionian, a fact that has been attributed to primary producer consumption following the winter convective mixing. As shown earlier, North Ionian Gyre (NIG) changes its circulation s

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Ramis, C., V. Homar, A. Amengual, R. Romero, and S. Alonso. "Daily precipitation records over mainland Spain and the Balearic Islands." Natural Hazards and Earth System Sciences 13, no. 10 (2013): 2483–91. http://dx.doi.org/10.5194/nhess-13-2483-2013.

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Abstract. Understanding the spatial distribution of extreme precipitations is of major interest in order to improve our knowledge of the climate of a region and its relationship with society. These analyses inevitably require the use of directly observed values to account for the actual extreme amounts rather than analyzed gridded values. A study of daily rainfall extremes observed over mainland Spain and the Balearic Islands is performed by using records from 8135 rain gauge stations from the Spanish Weather Agency (AEMET). Results show that the heaviest daily precipitations have been observe

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Kerr, Andrew, and Richard J. Wardle. "Definition of an Archean – Proterozoic crustal suture by isotopic studies of basement intersections from offshore wells in the southern Labrador Sea." Canadian Journal of Earth Sciences 34, no. 2 (1997): 209–14. http://dx.doi.org/10.1139/e17-017.

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Eight hydrocarbon exploration wells in the southern Labrador Sea penetrated Precambrian basement rocks, adjacent to the course of a Lithoprobe marine seismic reflection survey. The rock types are mostly Early Proterozoic (1870–1800 Ma) calc-alkaline plutonic rocks or their metamorphic derivatives, but one example is a Middle Proterozoic (1270 Ma) anorogenic intrusion. These samples of buried basement document a transition from juvenile Proterozoic crust in the southeast (shown by εNd from +0.8 to +2.2) to ancient Archean crust in the northwest (shown by εNd from −2.7 to −7.0). However, initial

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Tanaka, Yoshifumi. "Reflections on High Seas Marine Protected Areas: A Comparative Analysis of the Mediterranean and the North-East Atlantic Models." Nordic Journal of International Law 81, no. 3 (2012): 295–326. http://dx.doi.org/10.1163/15718107-08103004.

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In 2010, the Contracting-Parties to the Convention for the Protection of the Marine Environment of the North-East Atlantic (OSPAR Convention) created six marine protected areas (MPAs) on the high seas beyond 200 nautical miles with a view to protecting marine biological diversity. This is a significant step toward conservation of biological diversity on the high seas. The creation of high seas MPAs seems to provide a useful insight into the protection of community interests in marine spaces beyond the limits of national jurisdiction. At the same time, however, the creation of MPAs on the high

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Valsecchi, V., M. F. Sanchez Goñi, and L. Londeix. "Vegetation dynamics in the Northeastern Mediterranean region during the past 23 000 yr: insights from a new pollen record from the Sea of Marmara." Climate of the Past 8, no. 6 (2012): 1941–56. http://dx.doi.org/10.5194/cp-8-1941-2012.

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Abstract. High-resolution pollen analysis of core MD01-2430 from the Sea of Marmara (40°47.81' N, 27°43.51' E) allows us to reconstruct the vegetation response to climatic changes during the past 23 cal ka in the Northeastern Mediterranean. Variation in mesic/temperate forest cover indicates major climatic shifts connected to Heinrich Stadial 1, Bölling-Allerød, Younger Dryas and to the onset of the Holocene. Pollen–anthropogenic indicator approach was used to recognize human-induced landscape changes in the Sea of Marmara. The pollen-inferred onset of the Holocene occurs at ca. 11.5 cal ka, i

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Sissingh, W. "Kinematic sequence stratigraphy of the European Cenozoic Rift System and Alpine Foreland Basin: correlation with Mediterranean and Atlantic plate-boundary events." Netherlands Journal of Geosciences 85, no. 2 (2006): 77–129. http://dx.doi.org/10.1017/s0016774600077921.

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AbstractA review of the sequence stratigraphic development of the Tertiary basins of the North and West Alpine Foreland domains shows that their structural and depositional history was episodically affected by brief tectonic phases. These were associated with intermittent deformation events induced by the collisional convergence and compressional coupling of the Apulian and Iberian microplates with the European Plate. The plate kinematics-related episodicity was essentially isochronously recorded in the basin fills of the Alpine Foreland region. These are generally correlative with changes in

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Baldé, Bocar Sabaly, Patrice Brehmer, Saliou Faye, and Penda Diop. "Population Structure, Age and Growth of Sardine (Sardina pilchardus, Walbaum, 1792) in an Upwelling Environment." Fishes 7, no. 4 (2022): 178. http://dx.doi.org/10.3390/fishes7040178.

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Information on the biological parameters of exploited fish stocks facilitates the objective assessment and management of these living resources. The sardine (Sardina pilchardus) is considered as overexploited in northwest Africa. It is a key species of the Canaries current large marine ecosystem (CCLME) of the Atlantic Ocean due to its socioeconomic importance, as well as being a key intermediary species in marine food web. A massive decline in caught fish for Senegal over half a century is also reported (61,648 t in 1994 to 7486 t in 2017). Here, we analyzed the age and growth parameters of s

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Diatta, Samo, Cheikh Waly Diedhiou, Didier Maria Dione, and Soussou Sambou. "Spatial Variation and Trend of Extreme Precipitation in West Africa and Teleconnections with Remote Indices." Atmosphere 11, no. 9 (2020): 999. http://dx.doi.org/10.3390/atmos11090999.

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Extreme precipitation is a great concern for West Africa country, as it has serious consequence on key socio-economic activities. We use high resolution data from the Climate Hazards Group InfraRed Precipitation Stations (CHIRPS) to determine the spatial variability, trend of 8 extreme precipitation indices in West Africa and their relationship to remote indices. Spatial variability of extreme is characterized by maximum precipitation over the orographic regions, and in southern Sahel. The trend analysis shows a decrease of dry condition in Sahel and Sahara, and an increase tendency of wet ind

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Maldonado, Manuel, and Maria-Jesus Uriz. "Biotic Affinities in a Transitional Zone Between the Atlantic and the Mediterranean: A Biogeographical Approach Based on Sponges." Journal of Biogeography 22, no. 1 (1995): 89. http://dx.doi.org/10.2307/2846075.

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Polónia, Amélia, Ana Sofia Ribeiro, and Daniel Lange. "Connected oceans: New pathways in maritime history." International Journal of Maritime History 29, no. 1 (2017): 90–95. http://dx.doi.org/10.1177/0843871416679108.

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The Atlantic, Indian, and Pacific Oceans and the Mediterranean Sea are no longer studied as distinct oceanic regions but interrogated as variegated worlds, interconnected in multiple ways. This Forum explores the various ways in which maritime history has been dealing with this trend. It shows how the notion of oceans as interactive spaces requires maritime historians to look beyond the shoreline by placing the interconnectedness of sea and land at the centre of their analysis. Focusing on littorals and port cities, the five papers in this Forum investigate the sea as zone of cultural encounte

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Escribano, Nora, David Galicia, Arturo H. Ariño, and Carmen Escala. "Mammals in the MZNA Vertebrate Collection of University of Navarra, Spain." ZooKeys 634 (November 21, 2016): 137–50. https://doi.org/10.3897/zookeys.634.10207.

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In this paper five datasets are described that provide information about records of mammals in the Vertebrate Collection of the Museum of Zoology of the University of Navarra (MZNA-VERT). The datasets contain 3,466 records belonging to 20 species of mammals sampled across the transition zone between the Atlantic and Mediterranean biogeographical regions (north Iberian Peninsula). The datasets include both distributional data (georeferenced records) and basic biometric data of most of the vouchered specimens stored in the museum facilities. The samples originated mainly within research projects

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Dauvin, Jean-Claude, and Denise Bellan-Santini. "Biodiversity and the biogeographic relationships of the Amphipoda: Gammaridea on the French coastline." Journal of the Marine Biological Association of the United Kingdom 84, no. 3 (2004): 621–28. http://dx.doi.org/10.1017/s0025315404009658h.

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A recent inventory of the benthic Gammaridea: Amphipoda species on the French continental coastline catalogued 495 species. An analysis of the biodiversity and the biogeographic relationships that exist between the French Amphipoda: Gammaridea, living on the coastline that extends along 10° latitude range in the temperate region between 41° and 51° North and the other gammaridean faunas living in the north-eastern Atlantic has drawn the pattern of diversity in this marine invertebrate group on a large biogeographical scale. Gammaridean amphipods exhibit a latitudinal gradient over the total nu

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Siamak, Mansouri Far. "Geothermal field of the transition area between the Anatolian Plate and the East European Platform." Journal of the Belarusian State University. Geography and Geology, no. 2 (November 29, 2019): 133–48. http://dx.doi.org/10.33581/2521-6740-2019-2-133-148.

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Heat flow data from the Eastern Mediterranean region indicates an extensive province of low heat flow, spreading over the whole basin of the Mediterranean to the east of Crete (Levantine Sea), Cyprus, and Northern Egypt. Surface geology of East Anatolia is complex because of recent active tectonic and volcanic activity. The region is composed of major tectonic units of Pontides, the Anatolid-Tauride Belt and Bitlis Suture Zone, North and East Anatolian faults. Ophiolitic and young volcanic rocks can be observed in many parts of East Anatolia. The Black Sea is surrounded by the Alpine-Himalayan

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Valsecchi, V., M. F. Sanchez Goñi, and L. Londeix. "Vegetation dynamics in the Northeastern Mediterranean region during the past 23 000 yr: insight from a new pollen record from the Sea of Marmara (core MD01-2430)." Climate of the Past Discussions 8, no. 4 (2012): 4183–221. http://dx.doi.org/10.5194/cpd-8-4183-2012.

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Abstract. High-resolution pollen analysis of core MD01-2430 from the Sea of Marmara (40°47.81′ N, 27°43.51′ E) allows us to reconstruct the vegetation response to climatic changes during the past 23 cal ka in the Northeastern Mediterranean. Variation in mesic/temperate forest cover indicates major climatic shifts connected to Heinrich Stadial 1, Bölling-Allerød, Younger Dryas and to the onset of the Holocene. Pollen-anthropogenic indicator approach was used to recognize human-induced landscape changes in the Sea of Marmara. The pollen-inferred onset of the Holocene occurs at ca. 11.5 cal ka, i

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Argyriadis, Ion. "The superposed orogenesis of the alpine-mediterranean edifice." Boletín Geológico y Minero 127, no. 2-3 (2016): 593–612. http://dx.doi.org/10.21701/bolgeomin.127.2-3.020.

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The circum-Mediterranean chains must be considered as the result of two distinct orogenies. The apparent unity of the present structure is of formal order, due to the latest deformations. Since the Hercynian time there have been two periods of paroxysmal deformation; the younger fits the definition of the alpine orogeny; the older occurred during the Cretaceous and may correspond to the first great convergent relative drift of the Eurasiatic and African blocks. The Cretaceous or Mesogean orogeny is independent from the Alpine orogeny stricto sensu (Oligo-Miocene) and cannot be considered as it

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Rivera-González, Mª Carmen, and Pedro M. Sánchez-Castillo. "Diatomeas planctónicas del litoral de Andalucía (España). Planktonic diatoms from the coast of Andalusia (Spain)." Acta Botanica Malacitana 36 (December 1, 2011): 5–31. http://dx.doi.org/10.24310/abm.v36i1.2787.

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Español. Se estudian un total de 206 taxones identificados durante el estudio del ciclo anual realizado en las costas de Andalucía a lo largo del año 2000. Destacan, entre las diatomeas céntricas, la subclase Coscinodiscophycidae con 27 taxones y la subclase Chaetocerotophycidae con 28. Entre las pennadas destaca la clase Bacillariophyceae con 76 species. Los géneros que mostraron un mayor número de taxones fueron Chaetoceros, Thalassiosira y Rhizosolenia en el grupo de diatomeas céntricas, mientras que entre las pennadas destacaron los géneros Lyrella, Gyrosigma y Pseudonitzschia. Respecto a

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Testa, Giovanni, Mathieu Dever, Mara Freilich, et al. "Turbulent erosion of a subducting intrusion in the Western Mediterranean Sea." Ocean Science 21, no. 3 (2025): 989–1002. https://doi.org/10.5194/os-21-989-2025.

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Abstract. Frontal zones within the Western Alboran Gyre (WAG) are characterized by a density gradient resulting from the convergence of Atlantic and Mediterranean waters. Subduction along isopycnals at the WAG periphery can play a crucial role in upper-ocean ventilation and influences its stratification and biogeochemical cycles. In 2019, physical parameters (comprising temperature, salinity, turbulent kinetic energy dissipation rates) and biogeochemical data (oxygen and chlorophyll a) profiles were collected in transects along the northern edge of the WAG. Several intrusions of subducted wate

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