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Similar articles for PubMed (Select 17776858)

1.

Laminated diatomaceous sediments from the guaymas basin slope (central gulf of california): 250,000-year climate record.

Schrader H, Kelts K, Curray J, Moore D, Aguayo E, Aubry MP, Einsele G, Fornari D, Gieskes J, Guerrero J, Kastner M, Lyle M, Matoba Y, Molina-Cruz A, Niemitz J, Rueda J, Saunders A, Simoneit B, Vaquier V.

Science. 1980 Mar 14;207(4436):1207-9.

PMID:
17776858
2.

Increased dissolved oxygen in Pacific intermediate waters due to lower rates of carbon oxidation in sediments.

Stott LD, Berelson W, Douglas R, Gorsline D.

Nature. 2000 Sep 21;407(6802):367-70.

PMID:
11014190
3.

ENSO-like forcing on oceanic primary production during the Late Pleistocene.

Beaufort L, de Garidel-Thoron T, Mix AC, Pisias NG.

Science. 2001 Sep 28;293(5539):2440-4.

4.

Biosphere frontiers of subsurface life in the sedimented hydrothermal system of Guaymas Basin.

Teske A, Callaghan AV, LaRowe DE.

Front Microbiol. 2014 Jul 31;5:362. doi: 10.3389/fmicb.2014.00362. eCollection 2014.

6.

Bacterial Sulfate Reduction Above 100{degrees}C in Deep-Sea Hydrothermal Vent Sediments.

Jørgensen BB, Isaksen MF, Jannasch HW.

Science. 1992 Dec 11;258(5089):1756-7.

PMID:
17831655
7.

Migration of the subtropical front as a modulator of glacial climate.

Bard E, Rickaby RE.

Nature. 2009 Jul 16;460(7253):380-3. doi: 10.1038/nature08189.

PMID:
19606147
8.
9.

[Presence of red tides along the eastern coast of the Gulf of California].

Cortés-Altamirano R, Manrique FA, Luna-Soria R.

Rev Latinoam Microbiol. 1995 Oct-Dec;37(4):337-42. Spanish.

PMID:
8900569
10.

Late cretaceous precessional cycles in double time: a warm-Earth milankovitch response.

Park J, D'Hondt SL, King JW, Gibson C.

Science. 1993 Sep 10;261(5127):1431-4.

PMID:
17745354
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14.

The "white ocean" hypothesis: a late pleistocene southern ocean governed by coccolithophores and driven by phosphorus.

Flores JA, Filippelli GM, Sierro FJ, Latimer J.

Front Microbiol. 2012 Jul 2;3:233. doi: 10.3389/fmicb.2012.00233. eCollection 2012.

15.

Variations of Younger Dryas atmospheric radiocarbon explicable without ocean circulation changes

Goslar T, Arnold M, Tisnerat-Laborde N, Czernik J, Wieckowski K.

Nature. 2000 Feb 24;403(6772):877-80.

PMID:
10706281
16.

Deep-sea temperature and ice volume changes across the Pliocene-Pleistocene climate transitions.

Sosdian S, Rosenthal Y.

Science. 2009 Jul 17;325(5938):306-10. doi: 10.1126/science.1169938.

17.
18.

Manganese flux from continental margin sediments in a transect through the oxygen minimum.

Johnson KS, Berelson WM, Coale KH, Coley TL, Elrod VA, Fairey WR, Iams HD, Kilgore TE, Nowicki JL.

Science. 1992 Aug 28;257(5074):1242-5.

PMID:
17742757
19.

Oceanographic conditions and diversity of sea stars (Echinodermata: Asteroidea) in the Gulf of California, México.

Cintra-Buenrostro CE, Reyes-Bonilla H, Herrero-Pérezrul MD.

Rev Biol Trop. 2005 Dec;53 Suppl 3:245-61.

PMID:
17469254
20.

A thermodynamic analysis of the anaerobic oxidation of methane in marine sediments.

Larowe DE, Dale AW, Regnier P.

Geobiology. 2008 Dec;6(5):436-49. doi: 10.1111/j.1472-4669.2008.00170.x. Epub 2008 Aug 11.

PMID:
18699783
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