Why do arms extract less oxygen than legs during exercise?

[EN] To determine whether conditions for O2 utilization and O2 off-loading from the hemoglobin are different in exercising arms and legs, six cross-country skiers participated in this study. Femoral and subclavian vein blood flow and gases were determined during skiing on a treadmill at approximately 76% maximal O2 uptake (V(O2)max) and at V(O2)max with different techniques: diagonal stride (combined arm and leg exercise), double poling (predominantly arm exercise), and leg skiing (predominantly leg exercise). The percentage of O2 extraction was always higher for the legs than for the arms. At maximal exercise (diagonal stride), the corresponding mean values were 93 and 85% (n = 3; P < 0.05). During exercise, mean arm O2 extraction correlated with the P(O2) value that causes hemoglobin to be 50% saturated (P50: r = 0.93, P < 0.05), but for a given value of P50, O2 extraction was always higher in the legs than in the arms. Mean capillary muscle O2 conductance of the arm during double poling was 14.5 (SD 2.6) ml.min(-1).mmHg(-1), and mean capillary P(O2) was 47.7 (SD 2.6) mmHg. Corresponding values for the legs during maximal exercise were 48.3 (SD 13.0) ml.min(-1).mmHg(-1) and 33.8 (SD 2.6) mmHg, respectively. Because conditions for O2 off-loading from the hemoglobin are similar in leg and arm muscles, the observed differences in maximal arm and leg O2 extraction should be attributed to other factors, such as a higher heterogeneity in blood flow distribution, shorter mean transit time, smaller diffusing area, and larger diffusing distance, in arms than in legs.

Maximal muscular vascular conductances during whole body upright exercise in humans

[EN] That muscular blood flow may reach 2.5 l kg(-1) min(-1) in the quadriceps muscle has led to the suggestion that muscular vascular conductance must be restrained during whole body exercise to avoid hypotension. The main aim of this study was to determine the maximal arm and leg muscle vascular conductances (VC) during leg and arm exercise, to find out if the maximal muscular vasodilatory response is restrained during maximal combined arm and leg exercise. Six Swedish elite cross-country skiers, age (mean +/-s.e.m.) 24 +/- 2 years, height 180 +/- 2 cm, weight 74 +/- 2 kg, and maximal oxygen uptake (VO(2,max)) 5.1 +/- 0.1 l min(-1) participated in the study. Femoral and subclavian vein blood flows, intra-arterial blood pressure, cardiac output, as well as blood gases in the femoral and subclavian vein, right atrium and femoral artery were determined during skiing (roller skis) at approximately 76% of VO(2,max) and at VO(2,max) with different techniques: diagonal stride (combined arm and leg exercise), double poling (predominantly arm exercise) and leg skiing (predominantly leg exercise). During submaximal exercise cardiac output (26-27 l min(-1)), mean blood pressure (MAP) (approximately 87 mmHg), systemic VC, systemic oxygen delivery and pulmonary VO2(approximately 4 l min(-1)) attained similar values regardless of exercise mode. The distribution of cardiac output was modified depending on the musculature engaged in the exercise. There was a close relationship between VC and VO2 in arms (r= 0.99, P < 0.001) and legs (r= 0.98, P < 0.05). Peak arm VC (63.7 +/- 5.6 ml min(-1) mmHg(-1)) was attained during double poling, while peak leg VC was reached at maximal exercise with the diagonal technique (109.8 +/- 11.5 ml min(-1) mmHg(-1)) when arm VC was 38.8 +/- 5.7 ml min(-1) mmHg(-1). If during maximal exercise arms and legs had been vasodilated to the observed maximal levels then mean arterial pressure would have dropped at least to 75-77 mmHg in our experimental conditions. It is concluded that skeletal muscle vascular conductance is restrained during whole body exercise in the upright position to avoid hypotension.

Leg and arm lactate and substrate kinetics during exercise

[EN] To study the role of muscle mass and muscle activity on lactate and energy kinetics during exercise, whole body and limb lactate, glucose, and fatty acid fluxes were determined in six elite cross-country skiers during roller-skiing for 40 min with the diagonal stride (Continuous Arm + Leg) followed by 10 min of double poling and diagonal stride at 72-76% maximal O(2) uptake. A high lactate appearance rate (R(a), 184 +/- 17 micromol x kg(-1) x min(-1)) but a low arterial lactate concentration ( approximately 2.5 mmol/l) were observed during Continuous Arm + Leg despite a substantial net lactate release by the arm of approximately 2.1 mmol/min, which was balanced by a similar net lactate uptake by the leg. Whole body and limb lactate oxidation during Continuous Arm + Leg was approximately 45% at rest and approximately 95% of disappearance rate and limb lactate uptake, respectively. Limb lactate kinetics changed multiple times when exercise mode was changed. Whole body glucose and glycerol turnover was unchanged during the different skiing modes; however, limb net glucose uptake changed severalfold. In conclusion, the arterial lactate concentration can be maintained at a relatively low level despite high lactate R(a) during exercise with a large muscle mass because of the large capacity of active skeletal muscle to take up lactate, which is tightly correlated with lactate delivery. The limb lactate uptake during exercise is oxidized at rates far above resting oxygen consumption, implying that lactate uptake and subsequent oxidation are also dependent on an elevated metabolic rate. The relative contribution of whole body and limb lactate oxidation is between 20 and 30% of total carbohydrate oxidation at rest and during exercise under the various conditions. Skeletal muscle can change its limb net glucose uptake severalfold within minutes, causing a redistribution of the available glucose because whole body glucose turnover was unchanged.

Indicios de antecedencia en la red fluvial del sureste de Galicia

[ES] El presente trabajo ofrece un análisis preliminar de la red fluvial con antecedencia terciaria del sureste gallego. Las observaciones geomorfológicas de campo se centran en la cartografía de terrazas erosivas, canales abandonados, meandros colgados, codos de captura y redes anómalas. Para su interpretación se confrontaron con los thalwegs de los cursos principales y las fracturas alpinas cartografiadas por otros autores. Se propone una cronología para los procesos fluviales identificados; cronología que apunta una antigüedad de la red fluvial mayor a la estimada hasta el momento. De las siete tendencias identificadas, tres presentan una entidad regional (ENE-WSW, NE-SW, N-S), y cuatro local (NW-SE, SW-NE, SE-NW, S-N). Se confirma el carácter principal de la paleorred ENE-WSW (caracterizada por el río Sil) y como hipótesis se propone, para la Sierra de Queixa-San Mamede, el carácter de paleorrelieve positivo de herencia mesozoica. Este relieve habría sufrido varios procesos de levantamiento isostático y también tectónico durante la Orogenia Alpina. Estos levantamientos habrían provocado la superposición de capturas en las estribaciones surorientales de la Sierra de Queixa-San Mamede.

Evolución geomorfológica del Macizo Hespérico peninsular:estudio de un sector comprendido entre las provincias de Lugo y Ourense (Galicia, NW de España)

[EN] This paper deals with the relief generation in Ourense, an interior territory of the Galicia Country, at NW Spain, after the breakdown of Pangea 200 million years ago. The rupture of supercontinent causes the main effects in the outer part of Galicia, the present coast line and the shelf, but also the inner parts of Galicia where the landscape changes dramatically mainly ruled by fluvial incision connected with uprising, (orogenic, epirogenic, or isostatic origin), or even with eustatic oscillations, that shaped the previous old mesozoic landscape. Various things complicate the correct understanding of Galician geomorphology:1) the prevalent hercynian structure, (presumably reactivated during the Alpine Orogeny), causes that the epigenic processes, (fluvial, glaciar, marine and etching), acting on Galicia from Mesozoic to present times, produce end forms identified erroneously at the previous literature as tectonic and not as etch forms profiting from lithological or structural contrasts. 2) the common morphotectonic model accepted by all previous researchers establishes for the whole of Galicia a blocky pattern, (horst and graben like), due to extensional tectonic regime. This model is proved as no longer valid because the Galician tertiary basins, even were described at the past as graben depressions never have this origin. 3) big differences exist between the north and western sides of Galicia that show contrasted tectonic regime: compressional (with forms as the so called raised platforms), at the northern coast border, and extensional (with forms so typical as the Rias), at the western side. The study area is located at the confluence of two tectonic domains where the above mentioned effects are coincidents and specially well showed through different effects: prominent assimetry of fluvial captures (west facing), pronounced river incision and different kinds of tertiary basins: either strike slipe faults (Maceda, Xinzo de Limia, etc), or overslipped by inverse faults, (Quiroga, A Rúa, etc.), or even corresponding with depressions never, (or anywise passively), affected by tectonic movements, (Monforte). The paper include a detailed inventory of surfaces and terrace levels and their incision sequence which allow stablish a relative chronology of geomorphic evolution at this area of NW Spain during meso-cainozoic times.

Formaciones superficiales del replano erosivo R1000 en el sector de los Llanos de Castro Caldelas (Ourense, NO de España)

[ES] Se presenta la cartografía geomorfológica y el análisis de cuatro formaciones superficiales que recubren algunos sectores de los Llanos de Castro Caldelas, una planicie topográficamente aislada por el profundo encajamiento de la red fluvial del río Sil y por la falla de Maceda, de edad alpina. Sobre este replano erosivo se ha identificado una red fluvial fosil, parcialmente capturada por el río Sil y varios niveles de terrazas erosivas que corresponden al desmantelamiento del replano inicial R1000. La relación entre morfologías y depósitos permitió elaborar una secuencia de procesos desencadenada por un pulso tectónico que descabaló el replano R800 y produjo el levantamiento relativo de los Llanos de Castro Caldelas y otras áreas adyacentes