Premium
Carbon isotope cycle and mantle structure
Author(s) -
Coltice N.,
Simon L.,
Lécuyer C.
Publication year - 2004
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2003gl018873
Subject(s) - geology , subduction , mantle (geology) , oceanic crust , adakite , mantle wedge , sedimentary rock , crustal recycling , geochemistry , isotopes of carbon , geochemical cycle , crust , carbon cycle , earth science , geophysics , continental crust , isotope , paleontology , tectonics , physics , quantum mechanics , ecosystem , biology , ecology
Despite that no change is observed in the δ 13 C of sediments and upper mantle rocks over the Earth's history, the carbon isotope cycle is probably not at steady state. The δ 13 C of −5‰ of the upper mantle is different from that of the subducted carbon, which is close to −1‰. Indeed, most of the subducted carbon is made of carbonates: 85% of subducted sedimentary carbon plus carbonates formed by low temperature hydrothermal alteration of oceanic crust. Since no long term evolution is observed for the mantle and sedimentary rocks, the net subduction flux of heavy carbon requires to be compensated by a deep mantle process. End‐member models for the carbon isotope cycle at the Gyr scale suggest that it could be a flux from a deep primitive reservoir or the segregation of subducted oceanic crust at the core‐mantle boundary.