Unexpected dominance of parent-material strontium in a tropical forest on highly weathered soils

Controls over nutrient supply are key to understanding the structure and functioning of terrestrial ecosystems. Conceptual models once held that in situ mineral weathering was the primary long-term control over the availability of many plant nutrients, including the base cations calcium (Ca), magnes...

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Published in:	Ecology (Durham) 2005-03, Vol.86 (3), p.626-632
Main Authors:	Bern, Carleton R., Townsend, Alan R., Farmer, G. Lang
Format:	Article
Language:	eng
Subjects:	Animal and plant ecology Animal, plant and microbial ecology Atmosphere atmospheric deposition atmospheric nutrients Atmospherics Basalt Basaltic soils biogeochemical cycles Biological and medical sciences Calcium cations Costa Rica Forest soils Fundamental and applied biological sciences. Psychology General aspects Isotopes nutrient availability nutrient sources Nutrients parent material Rainforests Soil air soil erosion Soil nutrients Soil parent materials soil weathering strontium tropical forest Tropical forests tropical rain forests Tropical soils Weathering processes
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Summary:	Controls over nutrient supply are key to understanding the structure and functioning of terrestrial ecosystems. Conceptual models once held that in situ mineral weathering was the primary long-term control over the availability of many plant nutrients, including the base cations calcium (Ca), magnesium (Mg), and potassium (K). Recent evidence has shown that atmospheric sources of these "rock-derived" nutrients can dominate actively cycling ecosystem pools, especially in systems on highly weathered soils. Such studies have relied heavily on the use of strontium isotopes as a proxy for base-cation cycling. Here we show that vegetation and soil-exchangeable pools of strontium in a tropical rainforest on highly weathered soils are still dominated by local rock sources. This pattern exists despite substantial atmospheric inputs of Sr, Ca, K, and Mg, and despite nearly 100% depletion of these elements from the top 1 m of soil. We present a model demonstrating that modest weathering inputs, resulting from tectonically driven erosion, could maintain parent-material dominance of actively cycling Sr. The majority of tropical forests are on highly weathered soils, but our results suggest that these forests may still show considerable variation in their primary sources of essential nutrients.
ISSN:	0012-9658 1939-9170