Efficient transport of fossil organic carbon to the ocean by steep mountain rivers: An orogenic carbon sequestration mechanism

R. Hilton,A. Galy,N. Hovius,M. Horng,Hongey Chen

Published 2011 in Geology

ABSTRACT

Mountain building exposes fossil organic carbon (OC fossil ) in exhumed sedimentary rocks. Oxidation of this material releases carbon dioxide from long-term geological storage to the atmosphere. OC fossil is mobilized on hillslopes by mass wasting and transferred to the particu- late load of rivers. In large fl uvial systems, it is thought to be oxidised in transit, but in short, steep rivers that drain mountain islands, OC fossil may escape oxidation and re-enter geological storage due to rapid fl uvial transfer to the ocean. In these settings, the rates of OC fossil transfer and their controls remain poorly constrained. Here we quantify the erosion of OC fossil from the Taiwan mountain belt, combining discharge statistics with measurements of particulate organic carbon load and source in 11 rivers. Annual OC fossil yields in Taiwan vary from 12 ± 1 to 246 ± 22 tC km −2 yr −1 , controlled by the high physical erosion rates that accompany rapid crustal shortening and frequent typhoon impacts. Effi cient transfer of this material ensures that 1.3 ± 0.1 ◊ 10 6 tC yr −1 of OC fossil exhumed in Taiwan is delivered to the ocean, with <15% loss due to weathering in transit. Our fi ndings suggest that erosion of coastal mountain ranges can force effi cient transfer and long-term re-accumulation of OC fossil in marine sediments, further enhancing the role of mountain building in the long-term storage of carbon in the lithosphere.

PUBLICATION RECORD

  • Publication year

    2011

  • Venue

    Geology

  • Publication date

    Unknown publication date

  • Fields of study

    Geology, Environmental Science

  • Identifiers
  • External record

    Open on Semantic Scholar

  • Source metadata

    Semantic Scholar

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