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Santa Monica Basin

Pearson, A., A.P. McNichol, G.C. Benitez-Nelson, J.M. Hayes, and T.I. Eglinton. 2001. Origins of lipid biomarkers in Santa Monica Basin surface sediment A case study using compound-specific 14C analysis. Geochimica et Cosmochimica Acta 65 3123-3137. [Pg.122]

Figure 7. Mo concentotions (o) and isotopic compositions ( ) from reducing pore fluids in Santa Monica Basin (McManus et al. 2002). Dotted line indicates seawater values for both variables. The data can be fit by a 1-D reaction-diffusion model wifli a fractionation factor of —1.005. The effective fractionation factor for Mo removal across tiie sediment-water interface is smaller, <1.0025 (see text). Figure 7. Mo concentotions (o) and isotopic compositions ( ) from reducing pore fluids in Santa Monica Basin (McManus et al. 2002). Dotted line indicates seawater values for both variables. The data can be fit by a 1-D reaction-diffusion model wifli a fractionation factor of —1.005. The effective fractionation factor for Mo removal across tiie sediment-water interface is smaller, <1.0025 (see text).
Huh C-A, Zahnie DL, Small LF, et al. 1987. Budgets and behaviors of uranium and thorium series isotopes in Santa Monica basin (California, USA) sediments. Geochim Cosmochim Acta 51 1743-1754. [Pg.140]

P7a Basin) (Santa Monica Basin) Samples Samples Brooks et al. (1991) Normark et al. (2003)... [Pg.548]

Masiello, C. A., and Druffel, E. R. M. (2003). Organic and black carbon 13C and 14C through the Santa Monica Basin oxic-anoxic transition. Geophys. Res. Lett. 30, 34/1-34/4. [Pg.300]

Gong, C., and Hollander, D.J. (1997) Differential contribution of bacteria to sedimentary organic matter in oxic and anoxic environments, Santa Monica basin, California. Org. Geochem. 26, 545-563. [Pg.587]

Pearson, A., and Eglinton, T. 1. (2000). The origin of M-alkanes in Santa Monica Basin surface sediment A model based on compound-specific A C and c5 C data. Org. Geochem. 31, 1103-1116. [Pg.1271]

Eedwell J. R. and Watson A. (1991) The Santa Monica basin tracer experiment a smdy of diapycnal and isopycnal mixing. J. Geophys. Res. 96(C5), 8695 - 8718. [Pg.3095]

Pearson A., McNichol A. P., Benitez-Nelson B. C., Hayes J.M., and Eglinton T. I. (2001) Origins of lipid biomarkers in santa monica basin surface sediment a case study using compound-specific A14C analysis. Geochim. Cosmochim. Acta 65, 3123-3137. [Pg.5046]

Jahnke, R.A. (1990) Early Diagenesis and Recycling of Biogenic Debris at the Seafloor, Santa Monica basin, California. Journal of Marine Research, 48, 413-436. [Pg.234]

Gong and Hollander (1997) concluded from isotopic analyses of bulk organic matter and individual lipids that microbial biomass contributions increased under anaerobic conditions. This process could account for enhanced preservation of organic matter in the anoxic sediments relative to oxic sediments within the Santa Monica Basin, California. In... [Pg.593]

Benthic Chamber Results - Santa Monica Basin Oct 87 ROSE 2... [Pg.110]

Figure 2 A X values for bulk carbon reservoirs in the region of Santa Monica Basin, California, USA (A) prior to human influence pre-bomb A C ), and (B) contemporary values ( post-bomb A C ). Modified after Pearson (2000). Figure 2 A X values for bulk carbon reservoirs in the region of Santa Monica Basin, California, USA (A) prior to human influence pre-bomb A C ), and (B) contemporary values ( post-bomb A C ). Modified after Pearson (2000).
Lipid Biomarkers in Santa Monica Basin Sediments... [Pg.257]

Figure 8 A C data for individual lipids extracted from Santa Monica Basin sediments. The solid symbols represent compounds extracted from the post-bomb sedimentary horizon (ad 1950-1996). The hollow symbols represent compounds extracted from the prebomb sedimentary horizon (deposited prior to ad 1950). (Modified after Pearson (2000).)... Figure 8 A C data for individual lipids extracted from Santa Monica Basin sediments. The solid symbols represent compounds extracted from the post-bomb sedimentary horizon (ad 1950-1996). The hollow symbols represent compounds extracted from the prebomb sedimentary horizon (deposited prior to ad 1950). (Modified after Pearson (2000).)...
Small colloids [7,13,14] 5-200 nm Santa Monica Basin, North Atlantic, Northwest Pacific TEM 10 -10 maximum at thermocline largely organic rounded. rounded, globular, shape, diffuse... [Pg.154]

Fig. 4a-d. First transmission electron micrographs of marine colloids. Sea water samples were collected at a station in Santa Monica basin, September and July 1990 at different depths a, b 75 m c 400 m, and d 850 m (reproduced from Wells and Goldberg, 1991 [7])... [Pg.157]

Table 1. Santa Monica Basin sediment isotopic data... Table 1. Santa Monica Basin sediment isotopic data...
Fig. 1. Stable carbon isotope of organic fractions from the sediments of Santa Monica Basin. Fig. 1. Stable carbon isotope of organic fractions from the sediments of Santa Monica Basin.
Fig. 2. Radiocarbon age of the organic fractions from the sediments of Santa Monica Basin. For explanation of abbreviations of compound class fractions, refer to Fig. 1. Faa fatty acid. Fig. 2. Radiocarbon age of the organic fractions from the sediments of Santa Monica Basin. For explanation of abbreviations of compound class fractions, refer to Fig. 1. Faa fatty acid.
See other pages where Santa Monica Basin is mentioned: [Pg.387]    [Pg.440]    [Pg.1194]    [Pg.3093]    [Pg.3095]    [Pg.3252]    [Pg.4404]    [Pg.600]    [Pg.28]    [Pg.574]    [Pg.253]    [Pg.253]    [Pg.253]    [Pg.253]    [Pg.256]    [Pg.257]    [Pg.109]    [Pg.110]    [Pg.113]   
See also in sourсe #XX -- [ Pg.548 ]

See also in sourсe #XX -- [ Pg.109 , Pg.113 , Pg.114 , Pg.122 , Pg.123 ]



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Lipid biomarkers Santa Monica Basin

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