Abstract
We have performed the first known semicontinuous monitoring of particulate orgame carbon (POC) fluxes and dissolved Si concentrations delivered to the ocean during a typhoon. Sampling of the Choshui River in Taiwan during Typhoon Mindulle in 2004 revealed a POC flux of 5.00 × 105 t associated with a sediment flux of 61 Mt during a 96 h period. The linkage of high amounts of POC with sediment concentrations capable of generating a hyperpyenal plume upon reaching the ocean provides the first known evidence for the rapid delivery and burial of POC from the terrestrial system. These fluxes, when combined with storm-derived CO2 consumption of 1.65 × 108 mol from silicate weathering, elucidate the important role of these tropical cyclone events on small mountainous rivers as a global sink of CO2.
Original language | English |
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Pages (from-to) | 483-486 |
Number of pages | 4 |
Journal | Geology |
Volume | 36 |
Issue number | 6 |
DOIs | |
Publication status | Published - 2008 Jun |
Externally published | Yes |
Keywords
- CO consumption
- Chemical weathering
- Fluxes
- Organic carbon
- Particulate materials
ASJC Scopus subject areas
- Geology