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Title: Variations of marine plankton [delta][sup 13]C with latitude, temperature, and dissolved CO[sub 2] in the world ocean

Journal Article · · Global Biogeochemical Cycles; (United States)
DOI:https://doi.org/10.1029/93GB03272· OSTI ID:6956113
 [1];  [2]
  1. Scripps Institution of Oceanography, La Jolla, CA (United States)
  2. Ecosystems Center, Woods Hole, MA (United States)

Variations of the [sup 13]C content of marine particulate organic carbon [delta][sup 13]C[sub POC] in the modern ocean were studied using literature data to test the assumptions underlying the calculation of atmospheric pCO[sub 2] through geological time from the [delta][sup 13]C of sedimentary organic matter. These assumptions are that (1) concentrations of CO[sub 2] in the atmosphere and the surface ocean are at equilibrium at all times and latitudes and that (2) carbon isotopic fractionation of phytoplankton ([epsilon][sub p]) covaries primarily with concentrations of dissolved molecular CO[sub 2] ([CO[sub 2]][sub aq]). Previous studies and compilations have shown that the first assumption does not strictly hold, although [CO[sub 2]][sub aq] may be predicted with a reasonable degree of accuracy from sea surface temperature for specific regions of the world ocean. The second assumption is shown to be questionable due to the weak covariation of [epsilon][sub p] and [CO[sub 2]][sub aq] in the modern ocean. The large residual variance for regressions of [epsilon][sub p] against [CO[sub 2]][sub aq] suggests that factors other than [CO[sub 2]][sub aq] strongly affect carbon isotopic fractionation in phytoplankton. It is concluded that the relationship between [epsilon][sub p] and [CO[sub 2]][sub aq] cannot be easily calibrated using [delta][sup 13]C[sub POC] data from the modern ocean. 38 refs., 3 figs., 4 tabs.

DOE Contract Number:
FG02-92ER61438
OSTI ID:
6956113
Journal Information:
Global Biogeochemical Cycles; (United States), Vol. 8:1; ISSN 0886-6236
Country of Publication:
United States
Language:
English