Decoupling of unpolluted temperate forests from rock nutrient sources revealed by natural 87Sr/86Sr and 84Sr tracer addition

Martin J. Kennedy*, Lars O. Hedin, Louis A. Derry

*Corresponding author for this work

Research output: Contribution to journalArticle

59 Citations (Scopus)

Abstract

An experimental tracer addition of 84Sr to an unpolluted temperate forest site in southern Chile, as well as the natural variation of 87Sr/86Sr within plants and soils, indicates that mechanisms in shallow soil organic horizons are of key importance for retaining and recycling atmospheric cation inputs at scales of decades or less. The dominant tree species Nothofagus nitida feeds nearly exclusively (>90%) on cations of atmospheric origin, despite strong variations in tree size and location in the forest landscape. Our results illustrate that (i) unpolluted temperate forests can become nutritionally decoupled from deeper weathering processes, virtually functioning as atmospherically fed ecosystems, and (ii) base cation turnover times are considerably more rapid than previously recognized in the plant available pool of soil. These results challenge the prevalent paradigm that plants largely feed on rock-derived cations and have important implications for understanding sensitivity of forests to air pollution.

Original languageEnglish
Pages (from-to)9639-9644
Number of pages6
JournalProceedings of the National Academy of Sciences of the United States of America
Volume99
Issue number15
DOIs
Publication statusPublished - 23 Jul 2002
Externally publishedYes

Fingerprint Dive into the research topics of 'Decoupling of unpolluted temperate forests from rock nutrient sources revealed by natural 87Sr/86Sr and 84Sr tracer addition'. Together they form a unique fingerprint.

  • Cite this