Dynamic responses of oxygen uptake at the onset and end of moderate and heavy exercise in trained subjects.

Inconsistencies about dynamic asymmetry between the on- and off-transient responses in VO2 are found in the literature. Therefore the purpose of this study was to examine VO2 on- and off-transients during moderate- and heavy-intensity cycling exercise in trained subjects. Ten men underwent an initial incremental test for the estimation of ventilatory threshold (VT) and, on different days, two bouts of square-wave exercise at moderate (<VT) and heavy (>VT) intensities. VO2 kinetics in exercise and recovery were better described by a single exponential model (<VT), or by a double exponential with two time delays (>VT). For moderate exercise, we found a symmetry of VO2 kinetics between the on- and off-transients (i.e., fundamental component), consistent with a system manifesting linear control dynamics. For heavy exercise, a slow component superimposed on the fundamental phase was expressed in both the exercise and recovery, with similar parameter estimates. But the on-transient values of the time constant were appreciably faster than the associated off-transient, and independent of the work rate imposed (<VT and >VT). Our results do not support a dynamically linear system model of VO2 during cycling exercise in the heavy-intensity domain.

Relation of heart rate to percent VO2 peak during submaximal exercise in the heat.

We tested the hypothesis that elevation in heart rate (HR) during submaximal exercise in the heat is related, in part, to increased percentage of maximal O(2) uptake (%Vo(2 max)) utilized due to reduced maximal O(2) uptake (Vo(2 max)) measured after exercise under the same thermal conditions. Peak O(2) uptake (Vo(2 peak)), O(2) uptake, and HR during submaximal exercise were measured in 22 male and female runners under four environmental conditions designed to manipulate HR during submaximal exercise and Vo(2 peak). The conditions involved walking for 20 min at approximately 33% of control Vo(2 max) in 25, 35, 40, and 45 degrees C followed immediately by measurement of Vo(2 peak) in the same thermal environment. Vo(2 peak) decreased progressively (3.77 +/- 0.19, 3.61 +/- 0.18, 3.44 +/- 0.17, and 3.13 +/- 0.16 l/min) and HR at the end of the submaximal exercise increased progressively (107 +/- 2, 112 +/- 2, 120 +/- 2, and 137 +/- 2 beats/min) with increasing ambient temperature (T(a)). HR and %Vo(2 peak) increased in an identical fashion with increasing T(a). We conclude that elevation in HR during submaximal exercise in the heat is related, in part, to the increase in %Vo(2 peak) utilized, which is caused by reduced Vo(2 peak) measured during exercise in the heat. At high T(a), the dissociation of HR from %Vo(2 peak) measured after sustained submaximal exercise is less than if Vo(2 max) is assumed to be unchanged during exercise in the heat.

Reliability of stable carbon and oxygen isotope compositions of pedogenic needle fibre calcite as environmental indicators: examples from Western Europe.

Stable carbon and oxygen isotope analyses were conducted on pedogenic needle fibre calcite (NFC) from seven sites in areas with roughly similar temperate climates in Western Europe, including the Swiss Jura Mountains, eastern and southern France, northern Wales, and north-eastern Spain. The δ(13)C values (-12.5 to-6.8 0/00 Vienna Pee Dee Belemnite (VPDB)) record the predominant C(3) vegetation cover at the sites. A good correlation was found between mean monthly climatic parameters (air temperature, number of frost days, humidity, and precipitation) and δ(18)O values (-7.8 to-3.40/00 VPDB) of all the NFC. Similar seasonal variations of δ(18)O values for monthly NFC samples from the Swiss sites and those of mean monthly δ(18)O values of local precipitation and meteorological data point out precipitation and preferential growth/or recrystallisation of the pedogenic needle calcite during dry seasons. These covariations indicate the potential of stable isotope compositions of preserved NFC in fossil soil horizons as a promising tool for palaeoenvironmental reconstructions.

Auditory spatial deficits following hemispheric lesions: Dissociation of explicit and implicit processing.

Auditory spatial deficits occur frequently after hemispheric damage; a previous case report suggested that the explicit awareness of sound positions, as in sound localisation, can be impaired while the implicit use of auditory cues for the segregation of sound objects in noisy environments remains preserved. By assessing systematically patients with a first hemispheric lesion, we have shown that (1) explicit and/or implicit use can be disturbed; (2) impaired explicit vs. preserved implicit use dissociations occur rather frequently; and (3) different types of sound localisation deficits can be associated with preserved implicit use. Conceptually, the dissociation between the explicit and implicit use may reflect the dual-stream dichotomy of auditory processing. Our results speak in favour of systematic assessments of auditory spatial functions in clinical settings, especially when adaptation to auditory environment is at stake. Further, systematic studies are needed to link deficits of explicit vs. implicit use to disability in everyday activities, to design appropriate rehabilitation strategies, and to ascertain how far the explicit and implicit use of spatial cues can be retrained following brain damage.

Dissociation of allocentric and egocentric orientation: Effect on hippocampal place cells and place navigation

Navigation by means of cognitive maps appears to require the hippocampus; hippocampal place cells (PCs) appear to store spatial memories because their discharge is confined to cell-specific places called firing fields (FFs). Experiments with rats manipulated idiothetic and landmark-related information to understand the relationship between PC activity and spatial rotation. Rotating a circular arena in the caused a discrepancy between these cuse. This discrepancy caused most FFs to disappear in both the arena and room reference frames. However, FFs persisted in the rotating arena frame when the discrepancy was reduced by darkness or by a card in the arena. The discrepancy was increased by "field clamping" the rat in a room-defined FF location by rotations that countered its locomotion. Most FFs disspared and reappeared an hour or more after the clamp. Place-avoidance experiments showed that navigation uses independent idiothetic and exteroceptive memories. Rats learned to avoid the unmarked footshock region within a circular arena. When acquired on the stable arena in the light, the location of the punishment was learned by using both room and idiothetic cues; extinction in the dark transferred to the following session in the light. If, however, extinction occured during rotation, only the arena-frame avoidance was extinguished in darkness; the room-defined location was avoided when the light were turned back on. Idiothetic memory of room-defined avoidance was not formed during rotation in light; regardless of rotation with a randomly dispersed pellet. The resulting behaviour alternated between random pellet searching and target-directed navigation, making it possible to examine PC correlates of these two classes of spatial behaviour. The independence of idiothetic and exteroceptive spatial memories and the disruption of PC firing during rotation suggest that PCs may not be necessary for spatial cognition; this idea can be tested by recording during place-avoidance and preference tasks.

Right-left digit ratio (2D:4D) and maximal oxygen uptake.

A low digit ratio (2D:4D) and low 2D:4D in the right compared with the left hand (right-left 2D:4D) are thought to be determined by high in utero concentrations of testosterone, and are related to "masculine" traits such as aggression and performance in sports like running and rugby. Low right-left 2D:4D is also related to sensitivity to testosterone as measured by the number of cytosine-adenine-guanine triplet repeats in exon 1 of the androgen receptor gene. Here we show that low right-left 2D:4D is associated with high maximal oxygen uptake (VO2(max)), high velocity at VO2(max), and high maximum lactate concentration in a sample of teenage boys. We suggest that low right-left 2D:4D is linked to performance in some sports because it is a proxy of high sensitivity to prenatal and maybe also circulating testosterone and high VO2(max).

Physiopathologie du coeur embryonnaire soumis à l'anoxie-réoxygénation: rôle protecteur du NO et des canaux KATP

RESUME Introduction : Dans le coeur adulte, l'ischémie et la reperfusion entraînent des perturbations électriques, mécaniques, biochimiques et structurales qui peuvent causer des dommages réversibles ou irréversibles selon la sévérité de l'ischémie. Malgré les récents progrès en cardiologie et en chirurgie foetales, la connaissance des mécanismes impliqués dans la réponse du myocarde embryonnaire à un stress hypoxique transitoire demeure lacunaire. Le but de ce travail a donc été de caractériser les effets chrono-, dromo- et inotropes de l'anoxie et de la réoxygénation sur un modèle de coeur embryonnaire isolé. D'autre part, les effets du monoxyde d'azote (NO) et de la modulation des canaux KATP mitochondriaux (mito KATP) sur la récupération fonctionnelle postanoxique ont été étudiés. La production myocardique de radicaux d'oxygène (ROS) et l'activité de MAP Kinases (ERK et JNK) impliquées dans la signalisation cellulaire ont également été déterminées. Méthodes : Des coeurs d'embryons de poulet âgés de 4 jours battant spontanément ont été placés dans une chambre de culture puis soumis à une anoxie de 30 min suivie d'une réoxygénation de 60 min. L'activité électrique (ECG), les contractions de l'oreillette, du ventricule et du conotroncus (détectées par photométrie), la production de ROS (mesure de la fluorescence du DCFH) et l'activité kinase de ERK et JNK dans le ventricule ont été déterminées au cours de l'anoxie et de la réoxygénation. Les coeurs ont été traités avec un bloqueur des NO synthases (L-NAME), un donneur de NO (DETA-NONOate), un activateur (diazoxide) ou un inhibiteur (5-HD) des canaux mitoKATP un inhibiteur non-spécifique des PKC (chélérythrine) ou un piégeur de ROS (MPG). Résultats : L'anoxie et la réoxygénation entraînaient des arythmies (essentiellement d'origine auriculaire) semblables à celles observées chez l'adulte, des troubles de la conduction (blocs auriculo-ventriculaires de 1er, 2ème et 3ème degré) et un ralentissement marqué du couplage excitation-contraction (E-C) ventriculaire. En plus de ces arythmies, la réoxygénation déclenchait le phénomène de Wenckelbach, de rares échappements ventriculaires et une sidération myocardique. Aucune fibrillation, conduction rétrograde ou activité ectopique n'ont été observées. Le NO exogène améliorait la récupération postanoxique du couplage E-C ventriculaire alors que L'inhibition des NOS la ralentissait. L'activation des canaux mito KATP augmentait la production mitochondriale de ROS à la réoxygénation et accélérait la récupération de la conduction (intervalle PR) et du couplage E-C ventriculaire. La protection de ce couplage était abolie par le MPG, la chélérythrine ou le L-NAME. Les fonctions électrique et contractile de tous les coeurs récupéraient après 30-40 min de réoxygénation. L'activité de ERK et de JNK n'était pas modifiée par L'anoxie, mais doublait et quadruplait, respectivement, après 30 min de réoxygénation. Seule l'activité de JNK était diminuée (-60%) par l'activation des canaux mitoKATP. Cet effet inhibiteur était partiellement abolit par le 5-HD. Conclusion: Dans le coeur immature, le couplage E-C ventriculaire semble être un paramètre particulièrement sensible aux conditions d'oxygénation. Sa récupération postanoxique est améliorée par l'ouverture des canaux mitoKATP via une signalisation impliquant les ROS Ies PKC et le NO. Une réduction de l'activité de JNK semble également participer à cette protection. Nos résultats suggèrent que les mitochondries jouent un rôle central dans la modulation des voies de signalisation cellulaire, en particulier lorsque les conditions métaboliques deviennent défavorables. Le coeur embryonnaire isolé représente donc un modèle expérimental utile pour mieux comprendre les mécanismes associés à une hypoxie in utero et pour améliorer les stratégies thérapeutiques en cardiologie et chirurgie foetales. ABSTRACT Physiopathology of the anoxic-reoxygenated embryonic heart: Protective role of NO and KATP channel Aim: In the adult heart, the electrical, mechanical, biochemical and structural disturbances induced by ischemia and reperfusion lead to reversible or irreversible damages depending on the severity and duration of ischemia. In spite of recent advances in fetal cardiology and surgery, little is known regarding the cellular mechanisms involved in hypoxia-induced dysfunction in the developing heart. The aim of this study was to precisely characterize the chrono-, dromo- and inotropic disturbances associated with anoxia-reoxygenation in an embryonic heart model. Furthermore, the roles that nitric oxide (NO), reactive oxygen species (ROS), mitochondrial KATP, (mito KATP) channel and MAP Kinases could play in the stressed developing heart have been investigated. Methods: Embryonic chick hearts (4-day-old) were isolated and submitted in vitro to 30 min anoxia followed by 60 min reoxygenation. Electrical (ECG) and contractile activities of atria, ventricle and conotruncus (photometric detection), ROS production (DCFH fluorescence) and ERK and JNK activity were determined in the ventricle throughout anoxia-reoxygenation. Hearts were treated with NO synthase inhibitor (L-NAME), NO donor (DETA-NONOate), mitoKATP channel opener (diazoxide) or blocket (5-HD), PKC inhibitor (chelerythrine) and ROS scavenger (MPG). Results: Anoxia and reoxygenation provoked arrhythxnias (mainly originating from atrial region), troubles of conduction (st, 2nd, and 3rd degree atrio-ventricular blocks) and disturbances of excitation-contraction (E-C) coupling. In addition to these types of arrhythmias, reoxygenation triggered Wenckebach phenomenon and rare ventricular escape beats. No fibrillations, no ventricular ectopic beats and no electromechanical dissociation were observed. Myocardial stunning was observed during the first 30 min of reoxygenation. All hearts fully recovered their electrical and mechanical functions after 30-40 min of reoxygenation. Exogenous NO improved while NOS inhibition delayed E-C coupling recovery. Mito KATP, channel opening increased reoxygenation-induced ROS production and improved E-C coupling and conduction (PR) recovery. MPG, chelerythrine or L-NAME reversed this effect. Reoxygenation increased ERK and JNK activities land 4-fold, respectively, while anoxia had no effect. MitoKATP channel opening abolished the reoxygenation-induced activation of JNK but had no effect on ERK activity. This inhibitory effect was partly reversed by mitoKATP channel blocker but not by MPG. Conclusion: In the developing heart, ventricular E-C coupling was found to be specially sensitive to hypoxia-reoxygenation and its postanoxic recovery was improved by mitoKATP channel activation via a ROS-, PKC- and NO-dependent pathway. JNK inhibition appears to be involved in this protection. Thus, mitochondria can play a pivotal role in the cellular signalling pathways, notably under critical metabolic conditions. The model of isolated embryonic heart appears to be useful to better understand the mechanisms underlying the myocardial dysfunction induced by an in utero hypoxia and to improve therapeutic strategies in fetal cardiology and surgery.

Effects of dopamine on total oxygen consumption and oxygen delivery in healthy men.

The effect of acute intravenous dopamine (DA) administration at three sequential (but randomized) infusion rates was studied in eight young male volunteers. DA was infused at 2.5, 5, and 10 micrograms.kg-1.min-1. O2 consumption (VO2) and CO2 production (VCO2) were measured continuously by means of a computerized indirect calorimeter (blood system). In response to the 5- and 10-micrograms.kg-1.min-1 DA infusion rates, a significant increase (P less than 0.01) in VO2 corresponding to a 6% (range, 3-10) and 15% (range, 12-23) increase, respectively, of preinfusion values was observed. In contrast, at the low dose (2.5 micrograms.kg-1.min-1), DA induced no significant change in VO2. Cardiac output (Qc) increased significantly after the three DA administration rates [19% (range, 0-42), 34% (range, 17-71), and 25% (range, -3 to +47)] for the doses 2.5, 5, and 10 micrograms.-kg-1.min-1, respectively. The increase in O2 delivery (QO2) outweighed VO2 at all administration rates despite the relative drop in QO2 at the maximal DA administration rate. These results indicate that in humans DA improves net O2 supply to tissues proportionally more than it increases VO2 at all doses used in the present study.

Constraints on the upper Permian to upper Triassic marine carbon isotope curve : case studies from the Tethys

Secular variations of the seawater carbon isotopic composition provide evidence for paleoceanographic and paleoclimatic changes and may serve for chemiostratigraphic correlations. The present study aimed to improve the current knowledge on the Upper Permian and Triassic segment of the Phanerozoic marine carbon isotope curve, whose Triassic part was poorly constrained by previous studies. Profiles of inorganic carbon isotopes are provided for sections from Himalaya (Salt Range, Kashmir, Spiti and Nepal), Oman and North Dobrogea (Romania) on the basis of whole-rock carbonate analysis. The data acquired, together with a literature compilation confirmed that most of the Upper Permian is characterized by high δ13C values (averaging +40/00) but failed to detect a positive excursion as suggested by recent compilations. In the light of these observations, the large drop in δ13C values associated with the end-Permian mass extinction appears to be driven by a sudden transfer of previously stocked 13C depleted carbon, rather than by the overturn of a Late Permian stratified ocean. The Triassic data-set outlines significant secular variations. The best documented is a carbon isotope positive excursion just across the Lower-Middle Triassic boundary, globally developed since it was detected in various paleogeographic settings. It is interpreted to reflect variations in surface ocean chemistry, possibly related to increased primary productivity, at times when the biotic recovery after the end-Permian mass-extinction began to accelerate significantly and when a sharp rise in seawater δ34S values occurred globally. Strontium isotope data obtained from well preserved biogenic phosphates allow a refinement of the Middle Triassic segment of the seawater strontium isotope curve and show a major inflexion point of the seawater strontium isotope curve also near the Lower Triassic - Middle Triassic boundary. These facts suggest that the transition from the Early to the Middle Triassic was a time of revolutionary global change which represented an important step in the evolution of Mesozoic marine environments. A tentative carbon isotope curve for the Upper Permian to Upper Triassic time interval is proposed. Its major features are: ? high but constant δ13C values during the Late Permian ? a sharp drop in δ13C values in the latest Permian ? subsequent recovery of δ13C values ? a short-lived positive excursion across the Early-Middle Triassic boundary ? a gradual rise in δ13C values starting in the Late Ladinian or in the Early Carnian It is foreseen that these fluctuations of the carbon isotope curve may serve as chronostratigraphic markers and further assist in the correlation of Permian and Triassic carbonate deposits.

Evaluation of the quantity of Fe3+ in spinels for obtaining the oxygen fugacities in xenoliths.

The analysis by electron microprobe allows the evaluation of the quantity of Fe3+ ih spinels with considerable errors. The use of a correction equation which is based on a the calibration of analyses with an electron microprobe in relation to those carried out with Mossbauer spectroscopy gives more precise evaluations of Fe3+. In fact, it allows a calculation of the oxygen fugacity in peridotitic xenoliths. The obtained results show that peridotites of the French Central Massif crystallised under oxygen fugacities which were higher than those of the Moroccan Anti-Atlas.