Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Canfield oceans

Canfield Oceans Give Anaerobic Eukaryotes Room to Breathe. 7... [Pg.1]

Canfield oceans entail globally widespread anoxic and sulfidic marine environments, whereby the sulfide comes from biological sulfate reduction, the... [Pg.11]

Bertine, K.K. and E.D. Goldberg. 1972. Trace elements in clams, mussels, and shrimp. Limnol. Ocean. 17 877-884. Besser, J.M., T.J. Canfield, and T.W. La Point. 1993. Bioaccumulation of organic and inorganic selenium in a laboratory food chain. Environ. Toxicol. Chem. 12 57-72. [Pg.1623]

Habicht KS, Canfield DE (1997) Sulfur isotope fractionation during bacterial sulfate reduction in organic-rich sediments. Geochim CosmochimActa61(24) 5351-5361 Habicht KS, Gade M, Thamdrup B, Berg P, Canfield DE (2002) Calibration of sulfate levels in the Archean ocean. Science 298 2372-2374... [Pg.315]

Canfield DE (1998) Anew model for Proterozoic ocean chemistry. Nature 396 450-453 Canfield DE, Lyons TW, Raiswell R (1996) A model for iron deposition to euxinic Black Sea sediments. Am JSci 296 818-834... [Pg.451]

Schauble EA, Rossman GR, Taylor HP (2001) Theoretical estimates of equilibrium Fe-isotope fractionations from vibrational spectroscopy. Geochim Cosmochim Acta 65 2487-2597 Shen Y, Canfield DE, Knoll AH (2002) Middle Proterozoic ocean chemistry Evidence from the McArthur Basin, northern Australia. Am J Sci 302 81-109... [Pg.453]

Painter HJ, Morrisey JM, Mather MW, Vaidya AB (2007) Specific role of mitochondrial electron transport in blood-stage Plasmodium falciparum. Nature 446 88-91 Pisani D, Cotton JA, Mclnerney JO (2007) Supertrees disentangle the chimaeric origin of eukaryote genomes. Mol Biol Evol 24 1752-1760 Poulton SW, Fralick PW, Canfield DE (2004) The transition to a sulphidic ocean 1.84 billion years ago. Nature 431 173-177... [Pg.19]

Canfield DE (1998) A new model of Proterozoic ocean chemistry. Nature 396 450-452 Canfield DE, Habicht KS, Thamdrup B (2000) The Archean sulfiir cycle and the early history of atmospheric oxygen. Science 288 658-661... [Pg.34]

Canfield DE (1998) A new model for proterozoic ocean chemistry. Nature 396 450-453 Cavalier-Smith T (1987) Eukaryotes with no mitochondria. Nature 326 332-333 Chance B, Sies H, Boveris A (1979) Hydroperoxide metabolism in mammalian organs. Physiol Rev 59 527-605... [Pg.54]

Farquhar et ah, 2000 Holland and Rye, 1997 KnoU, 1996 Summons et ah, 1999). The deep ocean appears to have remained anoxic at least until the disappearance of banded iron formations at 1.8 Ga (Holland, 1984), and possibly as late as 0.8 Ga (Arnold et al., 2004 Canfield, 1998 Canfield and Teske, 1996). [Pg.1539]

Bjerrum, C. J., and Canfield, D. E. (2002). Ocean productivity before about 1.9 Gyr ago limited by phosphorus adsorption onto iron oxides. Nature 417, 159—162. [Pg.1558]

Canfield D. E. (1998) A new model for Proterozoic ocean chemistry. Nature 396, 450-452. [Pg.3462]

Habicht K. S., Gade M., Thamdrup B., Berg P., and Canfield D. E. (2002) Cahbration of sulfate levels in Archean ocean. Science 298, 2372-2374. [Pg.3464]

Shen Y., Canfield D. E., and KnoU A. H. (2002) Middle Proterozoic ocean chemistry evidence from the McArthur Basin, Northern Australia. Am. J. Sci. 302, 81-109. [Pg.3467]

See other pages where Canfield oceans is mentioned: [Pg.1]    [Pg.7]    [Pg.7]    [Pg.9]    [Pg.10]    [Pg.10]    [Pg.13]    [Pg.14]    [Pg.1]    [Pg.7]    [Pg.7]    [Pg.9]    [Pg.10]    [Pg.10]    [Pg.13]    [Pg.14]    [Pg.34]    [Pg.447]    [Pg.447]    [Pg.449]    [Pg.207]    [Pg.6]    [Pg.9]    [Pg.15]    [Pg.576]    [Pg.219]    [Pg.42]    [Pg.1558]    [Pg.3338]    [Pg.3433]    [Pg.3442]    [Pg.3569]    [Pg.3584]    [Pg.3585]    [Pg.3585]    [Pg.3591]    [Pg.3609]    [Pg.3610]   
See also in sourсe #XX -- [ Pg.3 , Pg.7 , Pg.9 , Pg.10 , Pg.13 , Pg.14 ]



SEARCH



© 2024 chempedia.info