Éditeur(s) : Apud Frid. Fleischer in comm
Extrait de : Flora brasiliensis. Volumen I. Pars I (après l'index de la deuxième partie)
Résumé : Cascade appelée Ribeirao do Palmital, près de Sabara dans la province de Minas Gerais
Tab. physiognom XXII.
Siècle(s) traité(s) : 19
Permalien : http://www.manioc.org/images/TLS17055-0273i1
TLS17055-0273i1

Résumé : Titre de société
Siècle(s) traité(s) : 20
Provenance : ORkidé|Fonds privé Pierre Rostan
Permalien : http://www.manioc.org/images/ORK120200001
ORK120200001

Éditeur(s) : HAL CCSD
Résumé : International audience
Previous studies have reported respiratory, cardiac and muscle changes at rest in triathletes 24 h after completion of the event. To examine the effects of these changes on metabolic and cardioventilatory variables during exercise, eight male triathletes of mean age 21.1 (SD 2.5) years (range 17-26 years) performed an incremental cycle exercise test (IET) before (pre) and the day after (post) an official classic triathlon (1.5-km swimming, 40-km cycling and 10-km running). The IET was performed using an electromagnetic cycle ergometer. Ventilatory data were collected every minute using a breath-by-breath automated system and included minute ventilation (V(E)), oxygen uptake (VO2), carbon dioxide production (VCO2), respiratory exchange ratio, ventilatory equivalent for oxygen (V(E)/VO2) and for carbon dioxide (V(E)/VCO2), breathing frequency and tidal volume. Heart rate (HR) was monitored using an electrocardiogram. The oxygen pulse was calculated as VO2/HR. Arterialized blood was collected every 2 min throughout IET and the recovery period, and lactate concentration was measured using an enzymatic method. Maximal oxygen uptake (VO2max) was determined using conventional criteria. Ventilatory threshold (VT) was determined using the V-slope method formulated earlier. Cardioventilatory variables were studied during the test, at the point when the subject felt exhausted and during recovery. Results indicated no significant differences (P > 0.05) in VO2max [62.6 (SD 5.9) vs 64.6 (SD 4.8) ml x kg(-1) x min(-1)], VT [2368 (SD 258) vs 2477 (SD 352) ml x min(-1)] and time courses of VO2 between the pre- versus post-triathlon sessions. In contrast, the time courses of HR and blood lactate concentration reached significantly higher values (P < 0.05) in the pre-triathlon session. We concluded that these triathletes when tested 24 h after a classic triathlon displayed their pre-event aerobic exercise capacity, bud did not recover pretriathlon time courses in HR or blood lactate concentration.
EUROPEAN JOURNAL OF APPLIED PHYSIOLOGY

hal-00720432
https://hal.univ-antilles.fr/hal-00720432
https://hal.univ-antilles.fr/hal-00720432/document
https://hal.univ-antilles.fr/hal-00720432/file/Article_2.pdf

Résumé : Titre de société

Provenance : ORkidé|Fonds privé Pierre Rostan
Permalien : http://www.manioc.org/images/ORK120490001
ORK120490001

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : À Madagascar, depuis quelques années, la sauvegarde de la biodiversité est devenue une priorité pour le gouvernement. Avec l’aide des partenaires étrangers, le pays étend actuellement de manière spectaculaire son réseau d’espaces protégés. Malgré l’intégration de la gouvernance participative sur le terrain, ce mouvement s’accompagne d’une très forte déstabilisation des communautés locales. Parallèlement, le pays qui affronte des crises multiples (crise économique latente et crises politiques à répétition) est le théâtre d’un formidable « boum » des activités informelles en général et de l’artisanat minier en particulier. Dans bien des cas, lorsque la gestion des milieux sensible est retirée aux communautés locales au profit d’acteurs institutionnels, on assiste au développement de ces activités destructrices. Pour lutter contre cet effet pervers de l’institutionnalisation de la protection environnementale, il devient urgent de disposer d’un plus large panel de systèmes de gouvernance. Ceux-ci doivent être conçus pour s’adapter aussi bien que possible à la multitude de contextes rencontrés, en prenant en compte l’ensemble des acteurs, qu’ils soient formels, issus de la société traditionnelle, ou informels.
In Madagascar, during the last few years, conservation of biodiversity has become a major priority for the government. Indeed, with the help of the foreign countries, Madagascar is currently expanding its network of protected areas. But despite the integration of participant governance on the ground, this movement contributes to the destabilization of local communities. Meanwhile, multiple crises (economic crisis, latent and recurrent political crises) take place in Madagascar. Besides, the country is the scene of a tremendous “boom” of informal activities in general, and small-scale mining in particular. In many cases, when the protection of sensitive environments is taken from local communities for the benefit of institutional actors, the development of these destructive activities in protected areas increases. To fight against this pernicious effect of the institutionalization of environmental protection, it is urgent to extend the modes of governance. These modes must be as flexible as possible, according to local contexts, and have to take into account traditional, formal or informal actors.
Madagascar

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.3622
http://journals.openedition.org/etudescaribeennes/3622

Éditeur(s) : Dunod Dunod
Résumé : Extrait des Annales des Mines 1898
Guyane française
19

Droits : Domaine public
patrimon:HASH1bca5324530311c76ece18

Éditeur(s) : Apud Frid. Fleischer in comm
Extrait de : Flora brasiliensis. Volumen I. Pars I (après l'index de la deuxième partie)
Résumé : Forêt brésilienne d'Araucaria (pin du Brésil) dans la province du Minas Gerais
Tab. physiognom XXXIX
Siècle(s) traité(s) : 19
Permalien : http://www.manioc.org/images/TLS17055-0307i1
TLS17055-0307i1

Éditeur(s) : HAL CCSD Wiley
Résumé : International audience
The Sivas Basin, located in the Central Anatolian Plateau of Turkey, is a foreland basin that records a complex interaction between sedimentation, salt tectonics and regional shortening during the Oligo-Miocene leading to the formation of numerous mini-basins. The Oligocene sedimentary infill of the mini-basins consists of a thick continental succession, the Karayün Formation, comprising a vertical succession of three main sub-environments: (i) playa-lake, (ii) fluvial braided, and (iii) saline lacustrine. These sub-environments are seen as forming a large Distributive Fluvial System (DFS) modified through time as a function of sediment supply and accommodation related to regional changes in climate and tectonic regime. Within neighbouring mini-basins and despite a similar vertical stratigraphic succession, subtle variations in facies assemblages and thickness are observed in stratigraphic units of equivalent age, thus demonstrating the local control exerted by halokinesis. Stratigraphic and stratal patterns reveal in great detail the complex interaction between salt tectonics and sedimentation including different types of halokinetic structures such as hooks, wedges and halokinetic folds. The regional variations of accommodation/sediment supply led to coeval changes in the architectural patterns recorded in the mini-basins. The type of accommodation regime produces several changes in the sedimentary record: (i) a regime dominated by regional accommodation limits the impact of halokinesis, which is recorded as very small variations in stratigraphic thickness and facies distribution within and between mini-basins; (ii) a regime dominated by localized salt-induced accommodation linked to the subsidence of each individual mini-basin enhances the facies heterogeneity within the DFS, causing sharp changes in stratigraphic thickness and facies assemblages within and between mini-basins.
ISSN: 0950-091X

hal-01685659
https://hal.archives-ouvertes.fr/hal-01685659
DOI : 10.1111/bre.12171

Éditeur(s) : HAL CCSD
Résumé : International audience
Tsavorite is exclusively hosted in the Neoproterozoic Metamorphic Mozambique Belt (NMMB). The gemstone mines, widespread between Kalalani (Tanzania) and Mgama Ridge (Kenya), define a continuous corridor over a hundred kilometers in length. The tsavorite is hosted by a metasedimentary sequence defined as the Kurase tsavorite-bearing metasediments (Kurase-TB metasediments) that also hosts rubies. These metasediments underwent amphibolite-facies metamorphism and are surrounded by granulitic gneisses that are also of sedimentary origin (the Kurase high-temperature gneisses). All these rocks lie below the Kasigau Group, a unit dominated by granulite-facies metamagmatic rocks.To constrain the timing of events that led to this peculiar occurrence of tsavorite, we have performed geochronological analyses of thin sections and of separated grains of zircon, monazite, and rutile using LA-ICP-MS and ID-TIMS, as well as 40Ar/39Ar of muscovite and phlogopite from various lithologies. The results show that the different terranes were metamorphosed synchronously between 620–580 Ma but under different P-T strain conditions. The Kurase-HT gneisses and the rocks from the Kasigau Group are highly strained and underwent granulite-facies metamorphism with abundant partial melting and emplacement of felsic melts between 620 and 600 Ma. Textural observations also underlined a late regional water flux controlling the occurrence of V-free muscovite and monazite mineralizations at 585 Ma. The latter event can be related to the activity of the Galana shear zone, in the east. The Kurase-TB metasediments escaped strain and partial melting. They record amphibolite-facies conditions with static heating, since initial sedimentary structures were locally preserved. The age of the tsavorite mineralization was inferred at 600 Ma from metamorphic zircon rims and monazite from the closest host-rocks, sampled in the mines. Hence, tsavorite crystallization occurred statically at the end of the metamorphic event, probably when the temperature and the amount of volatiles were at maximum levels.Conversely, the ruby formed by local metasomatism of felsic dikes and isolated ultramafic bodies. The rubies are older and zircons and monazites from a ruby-bearing felsic dike (plumasite) were dated at 615 Ma. Finally, data from rutile and micas indicate a global cooling below 430 °C of the whole region between 510 and 500 Ma.
The Canadian Mineralogist

hal-01616037
https://hal.archives-ouvertes.fr/hal-01616037
https://hal.archives-ouvertes.fr/hal-01616037/document
https://hal.archives-ouvertes.fr/hal-01616037/file/JEM.pdf
DOI : 10.3749/canmin.1700019

Éditeur(s) : Apud Frid. Fleischer in comm
Extrait de : Flora brasiliensis. Volumen I. Pars I (après l'index de la deuxième partie)
Résumé : Vallée de la province de Minas Gerais
Tab. physiognom IV.
Siècle(s) traité(s) : 19
Permalien : http://www.manioc.org/images/TLS17055-0237i1
TLS17055-0237i1

Résumé : Cliché
Siècle(s) traité(s) : 20
Droits : Domaine public
Provenance : ORkidé|Association Le Planeur Bleu (Cacao), Collection Philippe Soler
Permalien : http://www.manioc.org/images/ORK13i0630001
ORK13i0630001

Éditeur(s) : HAL CCSD Elsevier
Résumé : Two peat sequences were sampled in the vicinity of the main mining districts of the Vosges Mountains: Sainte-Marie-aux-Mines and Plancher-les-Mines. Lead isotopic compositions and excess lead fluxes were calculated for each of these radiocarbon-dated sequences. Geochemical records are in very good agreement with the mining history of the area, well known over the last millennium. Except for an anomaly corresponding to the Middle Bronze Age which has not yet been resolved, there is no clear geochemical evidence of local metal production in the Vosges before the 10th century as excess lead deposition archived between 500 BC and 500 AD is attributed to long-range transport of polluted particulate matter. The approach described here can be applied to other mining districts where archaeological evidence is scarce or even lacking, but where past exploitation is suspected.
ISSN: 0375-6742

hal-00512409
https://hal.archives-ouvertes.fr/hal-00512409
DOI : 10.1016/j.gexplo.2010.05.004

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Well-dispersed iron oxide nanoparticles supported onto graphene oxide sheets (i.e. GO-Fe3O4 nanocomposite) were synthesised and used as heterogeneous Fenton-like catalyst for the degradation of Acid Orange 7 dye (AO7). The reaction was systematically investigated under various experimental conditions such as nanocomposite dosage, pH, temperature, oxidant and dye concentrations. Best results showed a fast 80% degradation in ∼20 min, whilst ∼98% of AO7 was successfully removed after 180 min of reaction time. The degradation kinetics of AO7 was most influenced by pH and temperature, and can be described by a pseudo-first-order reaction following the Langmuir-Hinshelwood mechanism. Analysis of the spent nanocomposite suggested that the phase of iron oxide nanoparticles remained unchanged whilst minor pore volume losses occurred via carbon deposition and/or re-stacking of GO sheets. © 2014 Elsevier Ltd.
ISSN: 2213-3437

hal-01683206
https://hal.univ-antilles.fr/hal-01683206
DOI : 10.1016/j.jece.2014.08.001

Éditeur(s) : Arboleda & Valencia Arboleda & Valencia ( Bogota )
Résumé : (Statement of Responsibility) Español-ingles-frances.
At head of title: Tirado Macias.
Colombia

03183053
24001860
ocm03183053

Résumé : Titre de société
Siècle(s) traité(s) : 20
Permalien : http://www.manioc.org/images/ORK120960001
ORK120960001

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : International audience
Objectifs. - Évaluer les effets du triathlon classique (1,5 km natation, 40 km cyclisme, 10 km course à pied) sur la capacité de diffusion pulmonaire (DLCO) 24 heures après la compétition. Méthodes et résultats. - Dix triathlètes masculins (21,5 ± 2,8 ans) ont effectué une spirométrie et une mesure de la capacité de diffusion pulmonaire avant la compétition (pré-T) et 24 heures après l'épreuve (post-T). Les résultats montrent une diminution significative du volume expiratoire maximal en 1 s (5,17 ± 0,4 L.s-1 contre 4,09 ± 0,6 L.s-1) et du débit expiratoire maximal 25-75 % de la capacité vitale (6,98 ± 0,2 L.s-1 contre 4,90 ± 0,2 L.s-1). En revanche, les résultats ne montrent pas de différence significative entre les DLCO pré-T et post-T (38,1 ± 3,3 mL.min-1.mmHg-1 contre 37,1 ± 3,7 mL.min-1.mmHg-1) ni les ratios DLCO/VA (5,59 ± 0,5 mL.min-1.mmHg-1.A-1 contre 5,55 ± 0,7 ml.min-1.mmHg-1.A-1). Conclusion. - La DLCO est normale chez les triathlètes 24 heures après une compétition classique. Ceci peut traduire l'absence de lésions alvéolocapillaires pendant le triathlon. La baisse de la DLCO rapportée deux heures après un exercice dans la littérature peut s'expliquer par la baisse du volume sanguin pulmonaire qui apparaît comme un phénomène transitoire. Cependant, la baisse des débits pulmonaires observée 24 heures après le triathlon suggère la persistance chez les triathlètes d'un syndrome obstructif bronchique.
ISSN: 0765-1597

hal-00720522
https://hal.univ-antilles.fr/hal-00720522
https://hal.univ-antilles.fr/hal-00720522/document
https://hal.univ-antilles.fr/hal-00720522/file/Article_3_.pdf

Éditeur(s) : HAL CCSD Human Kinetics
Résumé : International audience
Purpose: Postexercise alveolar-capillary membrane-diffusing capacity (DLco) often decreases in highly trained endurance athletes and seems linked to their training status. To test the hypothesis that training status influences postexercise DLco, 13 male and 2 female triathletes (20.2 ± 4.4 y old, 175.2 ± 6.7 cm tall; weight in a range of 66.6 ± 7.4 kg to 67.4 ± 7.8 kg during the 1-y study) were randomized into experimental (n = 7) and control (n = 8) groups and performed VO2max cycle tests and simulated cycle-run successions (CR) of 30 min + 20 min after 3 periods in the competitive season. Methods: Both groups were tested before (pre- HTP) and after a 30-wk high-training period (HTP) with high training volume, intensity, and frequency. The experimental group was then also tested after a 6-wk low-training period (LTP) with low training volume, intensity, and frequency, while the control group continued training according to the HTP schedule for these 6 wk. Ventilatory data were collected continuously. DLco testing was performed before and 30, 60, and 120 min after the CR trials. Results: Whatever the period or group, DLco was significantly decreased 30 min after CR, with a significantly greater decrease in the experimental group than the control group in LTP (–15.7% and –9.3% of DLco, respectively). Conclusions: Six weeks of low training volume and intensity were sufficient to reverse the effects of high training volume and intensity on the alveolar-capillary membrane after a CR succession in competitive triathletes.
ISSN: 1555-0265

hal-01163434
https://hal.univ-antilles.fr/hal-01163434

Éditeur(s) : HAL CCSD
Résumé : National audience
Objectives To define the different stages of spontaneous labour. To determine the indications, modalities of use and the effects of administering synthetic oxytocin. And to describe undesirable maternal and perinatal outcomes associated with the use of synthetic oxytocin. Method A systematic review was carried out by searching Medline database and websites of obstetrics learned societies until March 2016. Results The 1st stage of labor is divided in a latence phase and an active phase, which switch at 5 cm of cervical dilatation. Rate of cervical dilatation is considered as abnormal below 1 cm per 4 hour during the first part of the active phase, and blow 1 cm per 2 hours above 7 cm of dilatation. During the latent phase of the first stage of labor, i.e. before 5 cm of cervical dilatation, it is recommended that an amniotomy not be performed routinely and not to use oxytocin systematically. It is not recommended to expect the active phase of labor to start the epidural analgesia if patient requires it. If early epidural analgesia was performed, the administration of oxytocin must not be systematic. If dystocia during the active phase, an amniotomy is recommended in first-line treatment. In the absence of an improvement within an hour, oxytocin should be administrating. However, in the case of an extension of the second stage beyond 2 hours, it is recommended to administer oxytocin to correct a lack of progress of the presentation. If dynamic dystocia, it is recommended to start initial doses of oxytocin at 2 mUI/min, to respect at least 30 min intervals between increases in oxytocin doses delivered, and to increase oxytocin doses by 2 mUI/min intervals without surpassing a maximum IV flow rate of 20 mUI/min. The reported maternal adverse effects concern uterine hyper-stimulation, uterine rupture and postpartum haemorrhage, and those of neonatal adverse effects concern foetal heart rate anomalies associated with uterine hyper-stimulation, neonatal morbidity and mortality, neonatal jaundice, weak suck/poor breastfeeding latch and autism. Conclusion The widespread use of oxytocin during spontaneous labour must not be considered as simply another inoffensive prescription without any possible deleterious consequences for mother or foetus. Conditions for administering the oxytocin must therefore respect medical protocols. Indications and patient consent have to be report in the medical file. © 2016 Elsevier Masson SAS
Revue Sage - Femme

hal-01467543
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01467543
DOI : 10.1016/j.sagf.2016.11.006

Résumé : Titre de société CAP 5 MF
Siècle(s) traité(s) : 20
Permalien : http://www.manioc.org/images/ORK120860001
ORK120860001

Éditeur(s) : George A. Smathers Libraries, University of Florida George A. Smathers Libraries, University of Florida ( Gainesville, FL )
Résumé : (Acquisition) Collected for University of Florida's Institutional Repository by the UFIR Self-Submittal tool. Submitted by Joseph Piazza.
Grant in collaboration with Peter Szok, Associate Professor of Latin America Studies at Texas Christian University Mini Grant Award $2,715

Droits : All rights reserved by the source institution.
http://ufdc.ufl.edu/IR00004137/00001