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Journal articles on the topic 'Sphalérite – France – Ariège (France)'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Kennedy, W. James, Michel Bilotte, and Michel Hansotte. "Cenomanian ammonites from Pech de Foix (Ariège, France)." Geobios 29, no. 3 (January 1996): 307–18. http://dx.doi.org/10.1016/s0016-6995(96)80031-3.

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2

James Kennedy, W., Michel Hansotte, Michel Bilotte, and Jacqueline Burnett. "Ammonites and Nannofossils from the Campanian of Nalzen (Ariège, France)." Geobios 25, no. 2 (January 1992): 263–78. http://dx.doi.org/10.1016/s0016-6995(06)80404-3.

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3

Dalmat, Yann-Mickael. "Brève : Masques en non-tissé made in France : capitale Ariège." Option/Bio 32, no. 629-630 (March 2021): 6. http://dx.doi.org/10.1016/s0992-5945(21)00031-3.

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4

Géraud, Manon, Julien Flament, Alice Hunt, Guillaume Sarah, Eddy Foy, and Florian Téreygeol. "Les céramiques métallurgiques de Castel-Minier (Ariège, France) xiiie-xve siècle." ArchéoSciences, no. 43 (December 30, 2019): 83–95. http://dx.doi.org/10.4000/archeosciences.6317.

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5

Wargny, M., M. Tourdjman, P. Soler, P. Chauvin, M. Gouali, and D. Mouly. "Épidémie de shigellose lors d’un festival musical, Ariège, France, juillet 2013." Revue d'Épidémiologie et de Santé Publique 62 (September 2014): S235. http://dx.doi.org/10.1016/j.respe.2014.06.205.

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6

Breton, Gérard, Michel Bilotte, and Gilles Eychenne. "L’ambre campanien du Mas d’Azil (Ariège, France) : gisement, micro-inclusions, taphonomie." Annales de Paléontologie 99, no. 4 (October 2013): 317–37. http://dx.doi.org/10.1016/j.annpal.2013.06.001.

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7

Lawson, Michelle. "Narrative positioning and ‘integration’ in lifestyle migration: British migrants in Ariège, France." Language and Intercultural Communication 17, no. 1 (May 25, 2016): 58–75. http://dx.doi.org/10.1080/14708477.2016.1165242.

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8

Clottes, Jean. "Paint Analyses from Several Magdalenian Caves in the Ariège Region of France." Journal of Archaeological Science 20, no. 2 (March 1993): 223–35. http://dx.doi.org/10.1006/jasc.1993.1015.

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9

Hendrickx, F., and E. Sauquet. "Impact of warming climate on water management for the Ariège River basin (France)." Hydrological Sciences Journal 58, no. 5 (July 2013): 976–93. http://dx.doi.org/10.1080/02626667.2013.788790.

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10

Leroy, S., S. X. Cohen, C. Verna, B. Gratuze, F. Téreygeol, P. Fluzin, L. Bertrand, and P. Dillmann. "The medieval iron market in Ariège (France). Multidisciplinary analytical approach and multivariate analyses." Journal of Archaeological Science 39, no. 4 (April 2012): 1080–93. http://dx.doi.org/10.1016/j.jas.2011.11.025.

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11

Tolksdorf, Johann Friedrich, Harald Floss, and Ingo Kraft. "De la France vers la Saxe – Des galets peints du Mas d’Azil (Ariège, France) dans les collections archéologiques de la Saxe." Paléo, no. 27 (December 30, 2016): 297–305. http://dx.doi.org/10.4000/paleo.3159.

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12

Pasquier, Christophe, Mathieu Fehlmann, Charlotte Bresson, Sylvain Fremaux, Alain Jean, and Jean-Philippe Thelliez. "Monitoring of Peregrine Falcons in the Ariège Pyrenees and Toulouse, Midi-Pyrénées region, France." Ornis Hungarica 26, no. 2 (December 1, 2018): 143–58. http://dx.doi.org/10.1515/orhu-2018-0023.

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Abstract Since the 1980s, the volunteers of the ornithological group of the Nature Midi-Pyrénées association have been monitoring the Peregrine Falcon (Falco peregrinus) population in the Ariège Pyrenees and in the Toulouse agglomeration. The data collected over the last 30 years show stability of the Ariège population: little variation has been observed in brood size, occupation rate of the sites or reproductive success. Only the increasing number of known nesting sites is significant, due to better knowledge of the territory by observers over time. In 2017, the breeding population was estimated to be 24 pairs. Urban monitoring proved the presence of individuals in passage, wintering or resident in Toulouse. Since 2002, downtown Toulouse has been visited by several individuals of both sexes and interactions between males and females have been observed since 2005. Despite the multiplicity of possible eyries or nesting sites in Toulouse, and the massive presence of Peregrine Falcons and dedicated bird watchers, no case of breeding has been reported. In addition to monitoring, measures to protect and support the presence of the species have been put in place. In the Pyrenees, in the light of the growth of human activities near nesting sites, some sites are now subject to official protective measures, coupled with constant vigilance and awareness. In Toulouse, to encourage the breeding of the individuals present, two nesting boxes were installed in 2016, on two buildings frequented by a female and a male. In 2017, a first attempt to reproduce in one of these installations confirmed the value of such developments in urban areas.

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13

Becam, Gaël, and Tony Chevalier. "Neandertal features of the deciduous and permanent teeth from Portel-Ouest Cave (Ariège, France)." American Journal of Physical Anthropology 168, no. 1 (November 21, 2018): 45–69. http://dx.doi.org/10.1002/ajpa.23719.

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14

Piret, Paul, Michel Deliens, and Michèle Pinet. "La trimounsite-(Y), nouveau silicotitanate de terres rares de Trimouns, Ariège, France: (TR)2Ti2SiO9." European Journal of Mineralogy 2, no. 5 (October 4, 1990): 725–30. http://dx.doi.org/10.1127/ejm/2/5/0725.

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15

Gheerbrant, Emmanuel, Claude Abrial, and Henri Cappetta. "Nouveaux sites a microvertébréscontinentaux du crétacé terminal des petites pyrénées (Haute-Garonne et Ariège, France)." Geobios 30 (January 1997): 257–69. http://dx.doi.org/10.1016/s0016-6995(97)80031-9.

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16

Lorand, J. P., J. L. Bodinier, C. Dupuy, and J. Dostal. "Abundance and distribution of gold in the orogenic-type spinel peridotites from Ariège (Northeastern Pyrenees, France)." Geochimica et Cosmochimica Acta 53, no. 11 (November 1989): 3085–90. http://dx.doi.org/10.1016/0016-7037(89)90188-9.

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17

Mastrorillo, Sylvain, Sovan Lek, and Francis Dauba. "Predicting the abundance of minnowPhoxinus phoxinus(Cyprinidae) in the River Ariège (France) using artificial neural networks." Aquatic Living Resources 10, no. 3 (May 1997): 169–76. http://dx.doi.org/10.1051/alr:1997018.

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18

Pailhaugue, Nicole. "Faune et saisons d'occupation de la salle Monique au Magdalénien Pyrénéen, grotte de la Vache (Alliat, Ariège, France) [Fauna and occupation seasons from « la salle Monique » during Pyrenean Magdalenian, grotte de la Vache, Alliat, Ariège, France]." Quaternaire 9, no. 4 (1998): 385–400. http://dx.doi.org/10.3406/quate.1998.1621.

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19

Tolksdorf, Johann Friedrich, Harald Floss, and Ingo Kraft. "From France to Saxony – Painted pebbles from Le Mas d’Azil (Ariège) in the archaeological collections from Saxony." Paléo, no. 27 (December 30, 2016): 297–305. http://dx.doi.org/10.4000/paleo.3297.

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20

de Saint Blanquat, M., J. M. Lardeaux, and M. Brunel. "Petrological arguments for high-temperature extensional deformation in the Pyrenean Variscan crust (Saint Barthélémy Massif, Ariège, France)." Tectonophysics 177, no. 1-3 (May 1990): 245–62. http://dx.doi.org/10.1016/0040-1951(90)90284-f.

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21

Fritz, Carole. "Towards the Reconstruction of Magdalenian Artistic Techniques: the Contribution of Microscopic Analysis of Mobiliary Art." Cambridge Archaeological Journal 9, no. 2 (October 1999): 189–208. http://dx.doi.org/10.1017/s0959774300015377.

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On the assumption that Magdalenian mobiliary art is the bearer of certain technical traditions which express cognitive and cultural values, research is directed towards the identification and appreciation of these values through the understanding of techniques involved in bone engraving. Examination of a set of 90 objects from sites in southwest France sheds light on repeated artistic activity and graphic ‘recipes’ which do not appear to be characteristic of local or regional groups. In the sequence of actions as well as in their final product, there is no activity specific to the Ariège as opposed to the Gironde. Magdalenian artists have identical shared artistic procedures.

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22

Cunill, Raquel, Jean-Paul Métailié, Didier Galop, Sébastien Poublanc, and Nicolas de Munnik. "Palaeoecological study of Pyrenean lowland fir forests: Exploring mid–late Holocene history of Abies alba in Montbrun (Ariège, France)." Quaternary International 366 (April 2015): 37–50. http://dx.doi.org/10.1016/j.quaint.2014.12.050.

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23

Py-Saragaglia, Vanessa, Raquel Cunill Artigas, Jean-Paul Métailié, Bruno Ancel, Sandrine Baron, Sandrine Paradis-Grenouillet, Émilie Lerigoleur, Nassima Badache, Hugues Barcet, and Didier Galop. "Late Holocene history of woodland dynamics and wood use in an ancient mining area of the Pyrenees (Ariège, France)." Quaternary International 458 (November 2017): 141–57. http://dx.doi.org/10.1016/j.quaint.2017.01.012.

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24

de Saint Blanquat, Michel, Flora Bajolet, Alexis Grand’Homme, Arnaud Proietti, Matthieu Zanti, Alexandre Boutin, Camille Clerc, Yves Lagabrielle, and Pierre Labaume. "Cretaceous mantle exhumation in the central Pyrenees: New constraints from the peridotites in eastern Ariège (North Pyrenean zone, France)." Comptes Rendus Geoscience 348, no. 3-4 (March 2016): 268–78. http://dx.doi.org/10.1016/j.crte.2015.12.003.

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25

Genthon, Pierre, Arnaud Bataille, André Fromant, Dominique D'Hulst, and Francois Bourges. "Temperature as a marker for karstic waters hydrodynamics. Inferences from 1 year recording at La Peyrére cave (Ariège, France)." Journal of Hydrology 311, no. 1-4 (September 2005): 157–71. http://dx.doi.org/10.1016/j.jhydrol.2005.01.015.

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26

Levasseur‑Garcia, Cecile, and Régis Vézian. "Differentiation of Bovinae teeth from the Portel‑Ouest Mousterian cave (Loubens, Ariège, France) by near‑infrared spectroscopy and chemometrics." Quaternaire, no. 32/1 (March 1, 2021): 1127. http://dx.doi.org/10.4000/quaternaire.15000.

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27

Brunel, C., M. Munoz, and A. Probst. "Remobilisation of Zn and Pb in a mountain stream contaminated by mining wastes during a moderate flood event (Ariège, France)." Journal de Physique IV (Proceedings) 107 (May 2003): 233–36. http://dx.doi.org/10.1051/jp4:20030285.

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28

Fabre, R., T. Lebourg, and B. Clément. "Les dépôts morainiques holocènes de la zone axiale pyrénéenne: approche déterministe de leur instabilité à Verdun sur Ariège, (Pyrénées centrales, France)." Bulletin of Engineering Geology and the Environment 58, no. 2 (February 22, 2000): 133–43. http://dx.doi.org/10.1007/s100640050007.

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29

Lacombe, Sébastien, Kathleen Sterling, Margaret Wright Conkey, and William Dietrich. "Le site de plein air de Peyre Blanque (Fabas, Ariège): un jalon original du Magdalénien dans le Sud-Ouest de la France." Bulletin de la Société préhistorique française 112, no. 2 (2015): 235–68. http://dx.doi.org/10.3406/bspf.2015.14521.

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30

Delmas, Magali, Régis Braucher, Yanni Gunnell, Valery Guillou, Marc Calvet, and Didier Bourlès. "Constraints on Pleistocene glaciofluvial terrace age and related soil chronosequence features from vertical 10Be profiles in the Ariège River catchment (Pyrenees, France)." Global and Planetary Change 132 (September 2015): 39–53. http://dx.doi.org/10.1016/j.gloplacha.2015.06.011.

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31

Lorand, J. P. "Abundance and distribution of CuFeNi sulfides, sulfur, copper and platinum-group elements in orogenic-type spinel lherzolite massifs of Ariège (northeastern Pyrenees, France)." Earth and Planetary Science Letters 93, no. 1 (May 1989): 50–64. http://dx.doi.org/10.1016/0012-821x(89)90183-0.

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32

Léger, Clément. "Bat parasites (Acari, Anoplura, Cestoda, Diptera, Hemiptera, Nematoda, Siphonaptera, Trematoda) in France (1762–2018): a literature review and contribution to a checklist." Parasite 27 (2020): 61. http://dx.doi.org/10.1051/parasite/2020051.

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This paper is a bibliographical survey of records of bat parasites in France (including Corsica) between 1762 and 2018. In total, 237 scientific publications were analysed. They show that bats are infected with a large diversity of endoparasites and ectoparasites. A total of 113 parasite taxa were identified from 27 host species; in addition, six bats were not identified to the species-level. The helminth fauna of bats comprises three species of Cestoda, 15 of Trematoda, and 13 of Nematoda. Acari parasites include 53 species (in addition to 22 invalid species). Finally, insect parasites comprise 13 species of Diptera (bat flies), 12 of Siphonaptera (fleas), 3 of Hemiptera (bugs), and 1 Anoplura species. Bat taxa reported with parasites were Barbastella barbastellus, Eptesicus serotinus, Hypsugo savii, Miniopterus schreibersii, Myotis bechsteinii, M. blythii, M. capaccinii, M. dasycneme, M. daubentonii, M. emarginatus, M. myotis, M. mystacinus, M. nattereri, M. punicus, Nyctalus lasiopterus, N. leisleri, N. noctula, Pipistrellus kuhlii, P. nathusii, P. pipistrellus, Plecotus auritus, P. austriacus, Rhinolophus euryale, R. ferrumequinum, R. hipposideros, R. mehelyi, Tadarida teniotis, Eptesicus sp., Myotis sp., Pipistrellus sp., Plecotus sp., Rhinolophus sp. and the species complex Pipistrellus pipistrellus/kuhlii/nathusii. As regards E. nilssonii, Vespertilio murinus (Particoloured Bat), M. alcathoe, M. escalerai, P. macrobullaris and P. pygmaeus, no records were found. These published field data originated from 72 of the 96 departments in metropolitan France. The most commonly cited were Ardèche, Ariège, Bouches-du-Rhône, Haute-Savoie, Maine-et-Loire, Moselle, Meurthe-et-Moselle, Pyrénées-Orientales, Sarthe, Haute-Corse and Corse-du-Sud.

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33

Berrada Hmima, Samia, Eric Marcoux, and Ahmid Hafid. "Le skarn Mo-W-Cu à grenat, wollastonite, pyroxène et vésuvianite d’Azegour (Haut-Atlas, Maroc)." Bulletin de la Société Géologique de France 186, no. 1 (January 1, 2015): 21–34. http://dx.doi.org/10.2113/gssgfbull.186.1.21.

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Abstract Le skarn minéralisé en Mo, W et Cu d’Azegour se forme aux dépens d’une série cambrienne essentiellement sédimentaire carbonatée dans l’auréole de métamorphisme d’un granite permien. Les bancs métasomatisés plurimétriques du skarn sont pour l’essentiel des grenatites et wollastonitites massives, plus rarement des pyroxénites. L’étude minéralogique montre que les grenatites sont composées pour l’essentiel d’andradite (grenat vert-noir et grenat brun-noir zoné) plus rarement de grossulaire (grenat orangé). Le pourcentage de spessartite est toujours faible (maximum 4 %). La wollastonite est légèrement manganésifère, la vésuvianite fluorée (jusqu’à 3,3 %) et chlorée (1,2 %). Les paragenèses permettent d’établir les conditions de formation du skarn aux alentours de 620–650 °C pour une pression de 1,7 à 2 kbar, avec une fCO2 de 31 mole %, en contexte réducteur (fO2 de 10−18 et 10−17 atm.). Le skarn d’Azegour est un marqueur de la fin de l’orogenèse hercynienne, et dénote la persistance de conditions réductrices, un environnement très favorable à la cristallisation de sulfures. Le skarn d’Azegour semble ainsi se former à des températures plus élevées que d’autres skarns à tungstène hercyniens comme Salau (Ariège, France).

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34

El Fouikar, Abderrahamane, and Armelle Gardeisen. "Contributions de l'archéozoologie et de l'analyse biochimique à l'étude de la conservation osseuse dans le Pléistocene supérieur de la grotte du Portel (Ariège, France)." Quaternaire 5, no. 1 (1994): 3–11. http://dx.doi.org/10.3406/quate.1994.2009.

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35

Sivelle, Vianney, David Labat, Naomi Mazzilli, Nicolas Massei, and Hervé Jourde. "Dynamics of the Flow Exchanges between Matrix and Conduits in Karstified Watersheds at Multiple Temporal Scales." Water 11, no. 3 (March 19, 2019): 569. http://dx.doi.org/10.3390/w11030569.

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The focus of this paper is to investigate the ability to assess the flow exchanges between the matrix and the conduits in two karstified watersheds (Aliou and Baget, Ariège, France) using the KarstMod modeling platform. The modeling is applied using hourly and daily time series. First, the flow dynamics between the conduit and the surrounding matrix are described on a rainfall event scale (i.e., a few days). The model allows us to describe a physical reality concerning the flow reversal between matrix and conduit when there is a significant rainfall event. Then, the long-term trends (i.e., inter-annual) in the matrix water level are evidenced using the moving average over shifting horizon method (MASH). The mean water level in the matrix dropped about 10% to 15% since the late 1960s. Also, the matrix recharge has been delayed from February in the late 1960s to April since the 1990s. Moreover, the contribution of the matrix in the total spring flow is estimated though mass balance. It is estimated that the annual matrix contribution in the total spring flow is about 3% and it can increase to up to 25% during periods with low rainfall.

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36

Saulnier, Mélanie, Raquel Cunill Artigas, Léonel Fouédjeu Foumou, Sandrine Buscaino, Jean-Paul Métailié, Didier Galop, and Vanessa Py-Saragaglia. "A study of late Holocene local vegetation dynamics and responses to land use changes in an ancient charcoal making woodland in the central Pyrenees (Ariège, France), using pedoanthracology." Vegetation History and Archaeobotany 29, no. 2 (July 22, 2019): 241–58. http://dx.doi.org/10.1007/s00334-019-00740-7.

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37

Howie, R. A. "C. Laforet, P. Monchoux, E. Oudin and F. Tollon. Ariège: T2. Bassin versant de l'Ariège (Inventaire minéralogique de la France, No. 12). Orléans B.R.G.M. 1986. 176 pp., 25 maps. Price 86 F." Mineralogical Magazine 51, no. 359 (March 1987): 181–82. http://dx.doi.org/10.1180/minmag.1987.051.359.34.

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38

Uzel, Jessica, Yves Lagabrielle, Serge Fourcade, Christian Chopin, Pierre Monchoux, Camille Clerc, and Marc Poujol. "The sapphirine-bearing rocks in contact with the Lherz peridotite body: New mineralogical data, age and interpretation." BSGF - Earth Sciences Bulletin 191 (2020): 5. http://dx.doi.org/10.1051/bsgf/2019015.

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Sapphirine-bearing rocks are described in the Aulus Basin (Ariège, France) in a contact zone between the Lherz peridotitic body and Mesozoic metasediments which underwent the Pyrenean Cretaceous high-temperature, low-pressure metamorphic event (Monchoux, 1970, 1972a, 1972b). Sapphirine crystals occur in layered clastic deposits characterized by an uncommon suite of Al-Mg-rich minerals. A detailed petrographic study of sixteen samples representative of the diversity of the Lherz sapphirine-bearing rocks is presented. These rocks include breccias and microbreccias with various compositions. Some samples are composed of polymineralic clasts and isolated minerals that derive from regionally well-known protoliths such as ultramafic rocks, meta-ophites, “micaceous hornfels”, and very scarce Paleozoic basement rocks. Nevertheless, a large portion of the sapphirine-bearing clastic suite is composed of mono- and polymineralic debris that derive from unknown protolith(s). We define a "sapphirine-bearing mineral suite” (SBMS) composed of monomineralic debris including: sapphirine + enstatite + aluminous spinel + Mg-amphiboles + Ca-amphiboles + kornerupine + accessory minerals (apatite, diopside, rutile, serpentine, smectite, tourmaline, vermiculite and a white mica). We highlight the dominance of metamorphic Keuper clastic materials in the studied rocks and the presence of inclusions of anhydrite and F-, Cl-, Sr-rich apatite in minerals of the Al-Mg-rich suite. The brecciated texture and the presence of unequivocal sedimentary features suggest that the sapphirine-bearing rocks were mechanically disaggregated and then experienced winnowing in underwater conditions with poor mixing between the different sources. We measured U-Pb rutile age data in order to provide constraints on the age of (one of) the protolith(s) of those clastic deposits. The obtained age (98.6 + 1.2 Ma) is interpreted as the age of metamorphism of this protolith of the SBMS. Previous works interpreted the Lherz sapphirine-bearing rocks as crustal protoliths modified at depth along the contact with the ultramafic rocks of the Lherz body during their ascent towards shallower depths. These new data imply: (i) an Upper Triassic to Lower Jurassic origin for the main protolith of the sapphirine-bearing rocks; (ii) the metamorphism of this protolith along an active hot crust–mantle detachment during Cenomanian times with the involvement of metasomatic, brine-type fluids; and (iii) its brecciation during the exhumation of the material due to the evolution of the detachment, followed by subsequent sedimentary reworking of the metamorphic material.

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39

Azémar, Frédéric, Frédéric Cazaban, and Laurent Pelozuelo. "Breaking the silence: how shedding light on the bone-skipper fly Thyreophora cynophila (Diptera: Piophilidae) demonstrated it still has a large distribution area in the Pyrenees mountains, France." Biodiversity Data Journal 8 (September 16, 2020). http://dx.doi.org/10.3897/bdj.8.e54868.

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Thyreophora cynophila (Panzer, 1798) is an iconic species of the European entomofauna. This winter-flying necrophagous fly was considered long extinct in Europe, before being discovered in Spain in 2010 and re-discovered in France in 2020, with a unique locality in Saint-Paul-de-Jarrat (Ariège, southern France). After bringing this species to the attention of people that are active in nature during the winter, including hunters, skilled naturalists, nature lovers and professional naturalists, we gathered seven new occurrence data for this species at six locations on the French flanks of the Pyrenees mountains. Those data considerably extend the known distribution of the species in Europe and allows mapping the first approximate extent of occurrence for this species in France.

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40

"LE CHEVAL DE MERENS." Animal Genetic Resources Information 13 (April 1994): 65–73. http://dx.doi.org/10.1017/s1014233900000298.

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RÉSUMÉRÉSUMÉ: Le cheval de Mérens, survivance du cheval préhistorique, est l'unique modèle restant aujourd'hui, du pur sang gaulois. L'image habituelle du cheval de race pure est ici renversée et les amateurs de pur-sang classique seront étonnés par le robuste et massif cheval de Mérens ; son berceau se trouve dans une terre peu connue des Pyrénées françaises : l'Ariège. On peut admirer plusieurs peintures rupestres représentant l'ancêtre du Mérens dans les grottes de Niaux (Ariège-Pyrénées). Doux et endurant, fort et élégant, disponible, confiant et économique, le cheval de Mérens retrouve cinq mois par an les pÂturages d'estives de haute montagne. Ce cheval peut être monté par des enfants en toute sécurité. Il a toutes les qualités du cheval de loisir. II est aussi champion de France d'attelage.Ces aptitudes nombreuses ont assuré au Mérens une reconnaissance internationale. Il s'exporte aujourd'hui en Hollande, en Espagne, en Allemagne, en Tunisie ainsi qu'en Outre-Mer.

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