Poster's note: of interest to those studying enhanced weathering

http://m.sciencemag.org/content/early/2014/01/15/science.1244908.abstract

Published Online January 16 2014
Science Express Index
Science DOI: 10.1126/science.1244908

Isaac J. Larsen
Peter C. Almond
Andre Ege
John O. Stone
David R. Montgomery
Brendon Malcolm
Corresponding author:[email protected]

Report

Rapid Soil Production and Weathering in the Western Alps, New Zealand

Abstract

Evaluating conflicting theories about the influence of mountains on carbon
dioxide cycling and climate requires understanding weathering fluxes from
tectonically uplifting landscapes. The lack of soil production and
weathering rate measurements in Earth's most rapidly uplifting mountains
has made it difficult to determine whether weathering rates increase or
decline in response to rapid erosion. 10Be concentrations in soils from the
western Southern Alps, New Zealand, demonstrate that soil is produced from
bedrock more rapidly than previously recognized, at rates up to 2.5 mm per
year. Weathering intensity data further indicate that soil chemical
denudation rates increase proportionally with erosion rates. These high
weathering rates support the view that mountains play a key role in
global-scale chemical weathering and thus have potentially important
implications for the global carbon cycle.

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