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Paleoceanography changes

Martin, J. H. (1990). Glacial-interglacial CO2 change The iron hypothesis. Paleoceanography 5,1-13. [Pg.276]

Broecker, W. S. and Henderson, G. M. (1998). The sequence of events surrounding Termination II and their implications for the cause of glacial-interglacial CO2 changes. Paleoceanography 13,352-364. [Pg.494]

Russell AD, Emerson S, Mix AC, Peterson LC (1996) The use of foraminiferal U/Ca as an indicator of changes in seawater uranium content. Paleoceanography 11 649-663 Rutherford E, Soddy F (1902) The cause and nature of radioactivity Part 11. Phil Mag Ser 6 4 569-585 Sacked WM (1960) Protactnium-231 content of ocean water and sediments. Science 132 1761-1762 Sacked WM (1958) Ionium-uranium ratios in marine deposited calcium carbonates and related materials. [Pg.404]

Bidigare RR, Hanson KL, Buesseler KO, Wakeham SG, Freeman KH, Pancost RD, Millero FJ, Steinberg P, Popp BN, Latasa M, Landry MR, Laws EA (1999) Iron-stimulated changes in C-13 fractionation and export by equatorial Pacific phytoplankton Toward a paleogrowth rate proxy. Paleoceanography 15 (5) 589-595... [Pg.488]

Adkins JF, Boyle EA (1997) Changing atmospheric A " C and the record of deep water paleoventilation ages. Paleoceanography 12(3) 337-344... [Pg.523]

Francois R, Bacon MP, Altabet MA (1993) Glacial/interglacial changes in sediment rain rate in the SW Indian sector of subantarctic waters as recorded by °Th, Pa, U and 5 N. Paleoceanography 8(5) 611-629... [Pg.525]

Sowers T, Bender M, Raynaud D, Korotkevich YS, Orchardo J (1991) The 6 0 of atmospheric O2 from air inclusions in the Vostok ice core timing of CO2 and ice volume changes during the Penultimate degladation. Paleoceanography 6 679-696... [Pg.271]

Hendy, I. L., Pedersen, T. F., Kennett, J. P., and Tada, R. (2004). Intermittent existence of a southern Californian upwehing ceU during submiUennial chmate change of the last 60 kyr. Paleoceanography 19(3). [Pg.1529]

Yang Y.-L., Elderfield H., and Ivanovich M. (1990) Glacial to Holocene changes in carbonate and clay sedimentation in the equatorial Pacific Ocean estimated from thorium 230 profiles. Paleoceanography 5, 789-809. [Pg.3189]

Cache I., Grimalt J. O., Canals M., Sbaffi L., Shackleton N. J., Schonfeld J., and Zahn R. (2001) Variability of the western Mediterranean sea surface temperature during the last 25, 000 years and its connection with the Northern Hemisphere climatic changes. Paleoceanography 16, 40-52. [Pg.3274]

Doose-Rolinski H., Rogalla U., Scheeder G., Luckge A., and von Rad U. (2001) High-resolution temperature and evaporation changes during the late Holocene in the northeastern Arabian Sea. Paleoceanography 16, 358-367. [Pg.3274]

The use of foraminiferal uranium/calcium ratios as an indicator of changes in seawater uranium content. Paleoceanography 11(6), 649—663. [Pg.3372]

Thomas E., Booth L., Mashn M., and Shackleton N. J. (1995) Northeastern Atlantic benthic foraminifera during the last 45,000 years—changes in productivity seen from the bottom up. Paleoceanography 10(3), 545-562. [Pg.3372]

Wollenburg J., Kuhnt W., and Mackensen A. (2001) Changes in Arctic Ocean paleproductivity and hydrography during the last 145 kyr the benthic foraminiferal record. Paleoceanography 16, 65-77. [Pg.3373]

Farrell J. W. and Prell W. L. (1989) Climatic change and CaCOs preservation an 800,000 year bathymetric reconstruction from the central equatorial Pacific Ocean. Paleoceanography 4, 447-466. [Pg.3393]

Barrera E. and Keller G. (1990) Stable isotope evidence for gradual environmental changes and species survivorship across the Cretaceous/Tertiary boundary. Paleoceanography 5, 867-890. [Pg.3827]


See other pages where Paleoceanography changes is mentioned: [Pg.397]    [Pg.226]    [Pg.495]    [Pg.400]    [Pg.529]    [Pg.238]    [Pg.314]    [Pg.1527]    [Pg.1533]    [Pg.3120]    [Pg.3121]    [Pg.3138]    [Pg.3270]    [Pg.3295]    [Pg.3331]    [Pg.3335]    [Pg.3369]    [Pg.3371]    [Pg.3393]    [Pg.3612]    [Pg.4328]   
See also in sourсe #XX -- [ Pg.244 , Pg.245 ]




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Paleoceanography

Paleoceanography glacial-interglacial changes

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