Basin Guaymas

Teske A, K-U Hinrichs, V Edgcomb, A de Vera Gomez, D Lysela, SP Sulva, ML Sogin, HW Jannach (2002) Microbial diversity of hydrothermal sediments in the Guaymas Basin evidence for anaerobic methano-trophic communities. Appl Environ Microbiol 68 1994-2007. [Pg.637]

C data on CO2 in hydrothermal solution from back-arc and midcxieanic ridge are not different except Guaymas Basins data. of hydrothermal solution from... [Pg.360]

N Guaymas Basin 14 Middle Valley 43 Escanaba Trough 32 Atlantic II Red Sea 53... [Pg.389]

Peter, J.M. and Scott, S.D. (1988) Mineralogy, composition, and fluid inclusion microthermometry of seafloor hydrothermal deposits in the Southern Trough of Guaymas Basin, Gulf of California. Can. Mineral, 26, 567-587. [Pg.401]

The CO2 concentrations of hydrothermal solutions at Guaymas Basin vary widely and some data show high CO2 concentrations. These high CO2 concentrations and low of fluids (—10.5%o) are considered to be caused by the effect of decomposition and dissolution of organic matters and carbonates in the sediments overlying basalt (Simoneit et al., 1984). [Pg.414]

Von Damm, K.L., Edmond, J.M., Measure, C.I. and Grant, B. (1985b) Chemistry of submarine hydrothermal solutions at Guaymas Basin, Gulf of California. Geochim. Cosmochim. Acta, 49, 2221-2237. [Pg.429]

Fig. 2 d-f (continued) d sediment, terrestrial source - Mediterranean Sea e hydrothermal petroleum - Guaymas basin, Gulf of California f road surface runoff water... [Pg.11]

Fig. 12. Salient features of the GC-MS data for a hydrothermal petroleum (Guaymas Basin, Gulf of California, Mexico) (a) TIC trace of total oil, (b) mjz 191 key ion for hopanes, and ctmjz 217 key ion for steranes. Numbers refer to carbon chain (/ -alkanes) or skeleton, UCM = unresolved complex mixture, Pr = pristane, Ph = phytane, asterisks = other isoprenoids, ot, ot, R, S = configurations of biomarkers.

Simoneit BRT, Hydrothermal petroleum Genesis, migration and deposition in Guaymas Basin, Gulf of California, Canadian Journal of Earth Sciences 22 1919— 1929, 1985. [Pg.114]

Kawka OE, Simoneit BRT, Polycyclic aromatic hydrocarbons in hydrothermal petroleums from the Guaymas Basin spreading center, in Simoneit BRT (ed.). [Pg.114]

Simoneit BRT, Lonsdale PF, Hydrothermal petroleum in minerahzed mounds at the seabed of Guaymas Basin, Nature 295 198—202, 1982. [Pg.124]

Simoneit BRT, Mazurek MA, Brenner S, Crisp PT, Kaplan IR, Organic geochemistry of Recent sediments from Guaymas Basin, Gulf of California, Deep-Sea Research 26A K73- 3, 1979. [Pg.124]

Bazylinski, D. A., Wirsen, C. O. Jannasch, H. W. (1989)- Microbial utilization of naturally occurring hydrocarbons at the Guaymas Basin hydrothermal vent site. Applied and Environmental Microbiology, 55, 2832-6. [Pg.119]

P7 Guaymas Basin) California, USA (Eel River BSR Field and Kvenvolden (1985)... [Pg.548]

Lupton, J. E. (1979) Helium-3 in the Guaymas Basin Evidence for injection of mantle volatiles in the Gulf of California.. 1 Geophys. Res., 84, 7446-52. [Pg.265]

Simoneit B. R. T. (1991) Hydrothermal effects on recent diatomaceous sediments in Guaymas Basin—generation, migration, and deposition of petroleum. In AAPG Memoir 47 The Gulf and Peninsular Province of the Californias, American Association of Petroleum Geologists, Tulsa, OK, chap. 38, pp. 793-825. [Pg.3072]

Ziveri P. and ThuneU R. (2000) Cocolithophore export in Guaymas Basin, Gulf of California response to cUmate forcing. Deep-Sea Res. II47, 2073-2KX). [Pg.3279]

Piepgras D. J. and Wasserburg G. J. (1985) Strontium and neodymium isotopes in hot springs on the East Paciflc Rise and Guaymas Basin. Earth Planet Sci. Lett. 72(4), 341-356. [Pg.3334]

Koski R. A., Lonsdale P. F., Shanks W. C., Berndt M. F., and Howe S. S. (1985) Mineralogy and geochemistry of a sediment-hosted hydrothermal sulfide deposit from the southern trough of Guaymas Basin, Gulf of California. J. Geophys. Res. 90, 6695-6707. [Pg.3501]

Figure 6. Plot of the pigment yield index (PYI) versus depth of burial for DSDP/IPOD Site 479 in the northeastern Guaymas basin slope. Gulf of California (cf. 20).

Sediments from the north rift of the Guaymas Basin (DSDP/IPOD Leg 64, Site 481.20) yielded 2 pigments of this series. Given as Figure 10 is the FTectronic spectra of purpurin-18 and chlorin-Pg isolates from this site. Spectra, chromatographic behavior and reactivity towards borohydride match that of authentic pigments. [Pg.120]

Didyk B.M., Simoneit B.R.T. (1989) Hydrothermal oil of Guaymas Basin and implications for petroleum formation mechanisms. Nature 342, 65-9. [Pg.333]

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