chromian spinel as a petrogenetic indicator in abyssal and alpine-type peridotites and spatially associated lavas.
the habitats under study are situated at the subalpine to alpine vegetation level with an altitude of 09568892434 m above sea level (fig. 1).
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the highland is a system of chaotic alpine ridges with absolute heights of up to 1146 m asl (average 600-800 m).
timberline and alpine vegetation on the tropical and warm-temperate oceanic islands of the world: elevation, structure and floristics.
another perspective on altitudinal limits of alpine timberlines.
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efficiency of indigenous and inoculated cold-adapted soil microorganisms for biodegradation of diesel oil in alpine soils.
positive interactions among alpine plants increase with stress.
evidence for a drought-induced alpine timberline.
features of afro-alpine plant ecology.
cold tolerance in tropical alpine plants.
metamorphism of alpine peridotite and serpentinite.
tropical alpine environments: plant form and function.
comparative water relations of tropical alpine plants.
causes of population differentiation in alpine amphibians.
tropical-alpine life-forms of vascular plants.
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