Registros del 1 al 10 de 15 encontrados |
1.- A 120-YEAR OLD RECORD OF WIDESPREAD CONTAMINATION FROM MINING OF THE IBERIAN PYRITE BELT AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1996 AGU 1996 FALL MEETING Ver registro
2.- A 14,000 year foraminiferal trace metal record of ENSO-influenced upwelling near southern Baja California American Geophysical Union; Washington, DC; USA; United States, 2005 AGU 2005 fall meeting Ver registro
3.- BENTHIC SULFUR CYCLING IN THE SEDIMENTS FROM THE OXYGEN MINIMUM ZONE OFF BAJA CALIFORNIA GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2001 GEOLOGICAL SOCIETY OF AMERICA, 2001 ANNUAL MEETING Ver registro
4.- Centennial scale variations of sea surface temperature and productivity over the last 14 ka in core PC-14 from the continental margin of Baja California American Geophysical Union; Washington, DC; USA; United States, 2008 AGU 2008 fall meeting Ver registro
5.- Decadal-scale variations in eastern Pacific thermocline structure from Soledad Basin, Baja California American Geophysical Union; Washington, DC; USA; United States, 2004 AGU 2004 fall meeting Ver registro
6.- DISTINGUISHING BETWEEN WATER COLUMN AND SEDIMENTARY DENITRIFICATION IN THE SANTA BARBARA BASIN USING THE STABLE ISOTOPES OF NITRATE AMERICAN GEOPHYSICAL UNION AND THE GEOCHEMICAL SOCIETY;; USA; UNITED STATES, 2003 Ver registro
7.- Dynamical response of the tropical Pacific Ocean to solar forcing during the Holocene American Geophysical Union; Washington, DC; USA; United States, 2009 AGU 2009 fall meeting Ver registro
8.- ENHANCED MARINE PRODUCTIVITY OFF WESTERN NORTH AMERICA DURING WARM CLIMATE INTERVALS OF THE PAST 52 K.Y. GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2004 Ver registro
9.- Expansion of the Northeast Pacific oxygen-minimum zone since 1995? Sediment N-isotope evidence from Soledad Basin, Baja California Elsevier; New York, NY; III; International, 2009 Abstracts of the 19th annual V. M. Goldschmidt conference Ver registro
10.- Intermediate water 14C evidence for the mechanism of deglacial CO2 increase American Geophysical Union; Washington, DC; USA; United States, 2006 AGU 2006 fall meeting Ver registro
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