Impacts of ecosystem engineers on community attributes: effects of cushion plants at different elevations of the Chilean Andes

2006 ◽  
Vol 12 (4) ◽  
pp. 388-396 ◽  
Author(s):  
Ernesto I. Badano ◽  
Lohengrin A. Cavieres
2013 ◽  
Vol 19 (4) ◽  
pp. 561-568
Author(s):  
Fengshou MENG ◽  
Peili SHI ◽  
Wei YAN ◽  
Yongtao HE

Ecosystems ◽  
2021 ◽  
Author(s):  
Susana Rodríguez-Echeverría ◽  
Manuel Delgado-Baquerizo ◽  
José A. Morillo ◽  
Aurora Gaxiola ◽  
Marlene Manzano ◽  
...  

Author(s):  
Henrique Jesus de Souza ◽  
Jacques Hubert Charles Delabie
Keyword(s):  

1964 ◽  
Vol 19 (1) ◽  
pp. 21-24 ◽  
Author(s):  
James W. Terman ◽  
Jerry L. Newton

In the summer of 1962 at the White Mountain Research Station the early phases of altitude acclimatization were studied in six of the surviving eight members of the 1935 expedition to the Chilean Andes; they were from 58 to 71 years of age. Alveolar and arterial Po2 and Pco2 were determined for each man a few hours after arrival at 3,093 m and at 3,800 and 4,343 m over the next few days. The effects of age were superimposed on the classical responses to high altitude. The arterial and alveolar Pco2 values showed no significant gradient; the alveolar Pco2 was found to be lower for a given altitude than 27 years before. For example, their average alveolar Pco2 at 4,700 m in 1935 was 27.7 mm Hg as opposed to 25.1 mm Hg at 4,343 m in 1962. The case of Hall was exceptional: his alveolar Pco2 ranged from 21 to 24 mm Hg regardless of altitude for his sojourn of 22 days. In 1935 these six men had a mean A-a Po2 gradient of +3.0 mm Hg at 4,700 m, while in 1962 the gradient over the three altitudes was +12.4 mm Hg. These findings would likely be explained partially by age changes in the pulmonary ventilation-perfusion ratio. acclimatization; pulmonary ventilation-perfusion ratio; alveolar-arterial Po2 and Pco2 gradients; alveolar hyperventilation; aging and altitude Submitted on February 19, 1963


1975 ◽  
Vol 14 (70) ◽  
pp. 155-170 ◽  
Author(s):  
Cesar N. Caviedes ◽  
Roland Paskoff

The extension of the Quaternary glaciations has been studied in the semi-arid Andes of north-central Chile, where the glacial modelling is striking. In the Elqui valley (lat. 30°S.), two glacial advances were identified reaching down to 3 100 m (Laguna glaciation) and 2 500 m (Tapado glaciation). In the Aconcagua valley (lat. 33°S.), moraines from three major glacial advances were found, at 2 800 m (Portillo glaciation), 1 600 m (Guardia Vieja glaciation) and 1 300 m (Salto del Soldado glaciation).The Quaternary glaciations were linked with a decrease of temperature, but more significantly with a marked increase of precipitation probably related to an equatorward shift of 5–6 degrees of the austral polar front. The results obtained in the semi-arid Chilean Andes are correlated with those recently reported from other sectors of the southern Andes.


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