Abstract
As soils develop in humid environments, rock-derived elements are gradually lost, and under constant conditions it seems that ecosystems should reach a state of profound and irreversible nutrient depletion. We show here that inputs of elements from the atmosphere can sustain the productivity of Hawaiian rainforests on highly weathered soils. Cations are supplied in marine aerosols and phosphorus is deposited in dust from central Asia, which is over 6,000 km away.
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Acknowledgements
This research was supported by the Andrew Mellon Foundation, by the NSF, and by NASA-MTPE. For logistical assistance and access to sites, we are indebted to USDA–National Resources Conservation Service, USGS–Biological Resources Division, Hawaii Volcanoes National Park, Hawaii DL&NR, the Nature Conservancy, and Parker Ranch.
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Chadwick, O., Derry, L., Vitousek, P. et al. Changing sources of nutrients during four million years of ecosystem development. Nature 397, 491–497 (1999). https://doi.org/10.1038/17276
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DOI: https://doi.org/10.1038/17276
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