Modeling the relationship between 231Pa/230Th distribution in North Atlantic sediment and Atlantic meridional overturning circulation
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F. Joos | T. Stocker | M. Siddall | G. Henderson | N. Edwards | S. Müller | M. Frank | S. P. Ritz
[1] G. Henderson,et al. Comment on “Do geochemical estimates of sediment focusing pass the sediment test in the equatorial Pacific?” by M. Lyle et al. , 2007 .
[2] M. Fleisher,et al. Diatom productivity in the equatorial Pacific Ocean from the last glacial period to the present: A test of the silicic acid leakage hypothesis , 2006 .
[3] F. Joos,et al. Water mass distribution and ventilation time scales in a cost-efficient, three-dimensional ocean model , 2006 .
[4] S. B. Moran,et al. Accelerated drawdown of meridional overturning in the late‐glacial Atlantic triggered by transient pre‐H event freshwater perturbation , 2006 .
[5] M. Gehlen,et al. On the potential of 230Th, 231Pa, and 10Be for marine rain ratio determinations: A modeling study , 2006 .
[6] Alexander L. Thomas,et al. Interpretation of the 231 Pa/ 230 Th paleocirculation proxy: New water-column measurements from the southwest Indian Ocean , 2006 .
[7] E. Cortijo,et al. Evidence from the Northeastern Atlantic basin for variability in the rate of the meridional overturning circulation through the last deglaciation , 2005 .
[8] F. Joos,et al. 231Pa/230Th fractionation by ocean transport, biogenic particle flux and particle type , 2005 .
[9] Yuan-hui Li. Controversy over the relationship between major components of sediment-trap materials and the bulk distribution coefficients of 230Th, 231Pa, and 10Be , 2005 .
[10] Robert F. Anderson,et al. Increased productivity in the subantarctic ocean during Heinrich events , 2005, Nature.
[11] A. Schmittner. Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulation , 2005, Nature.
[12] A. Mix,et al. Do geochemical estimates of sediment focusing pass the sediment test in the equatorial Pacific , 2005 .
[13] Robert Marsh,et al. Uncertainties due to transport-parameter sensitivity in an efficient 3-D ocean-climate model , 2005 .
[14] P. Stoffers,et al. Radionuclide fluxes in the Arabian Sea: the role of particle composition , 2005 .
[15] J. McManus,et al. Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes , 2004, Nature.
[16] R. Usbeck,et al. Adsorption of thorium and protactinium onto different particle types: experimental findings , 2004 .
[17] T. Ku,et al. On the importance of opal, carbonate, and lithogenic clays in scavenging and fractionating 230Th, 231Pa and 10Be in the ocean , 2004 .
[18] T. Ku,et al. Reply to Comment on “On the importance of opal, carbonate, and lithogenic clays in scavenging and fractionating 230Th, 231Pa and 10Be in the ocean” , 2004 .
[19] T. Stocker,et al. A minimum thermodynamic model for the bipolar seesaw , 2003 .
[20] Paul E. Robbins,et al. Data-Based Meridional Overturning Streamfunctions for the Global Ocean , 2003 .
[21] A. Ganachaud. Large-scale mass transports, water mass formation, and diffusivities estimated from World Ocean Circulation Experiment (WOCE) hydrographic data , 2003 .
[22] G. Henderson,et al. The U-series Toolbox for Paleoceanography , 2003 .
[23] P. Kubik,et al. The influence of particle composition and particle flux on scavenging of Th, Pa and Be in the ocean , 2002 .
[24] F. Joos,et al. Ocean thermohaline circulation and sedimentary 231Pa/230Th ratio , 2000 .
[25] C. Heinze,et al. Global distribution of the 230Th flux to ocean sediments constrained by GCM modelling , 1999 .
[26] G. Kuhn,et al. Variations of biogenic particle flux in the southern Atlantic section of the Subantarctic Zone during the late Quaternary: Evidence from sedimentary and , 1999 .
[27] T. Ku,et al. OCEANIC 231PA/230TH RATIO INFLUENCED BY PARTICLE COMPOSITION AND REMINERALIZATION , 1999 .
[28] H. J. Walter,et al. Enhanced scavenging of 231Pa relative to 230Th in the South Atlantic south of the Polar Front: Implications for the use of the 231Pa/230Th ratio as a paleoproductivity proxy , 1997 .
[29] G. Wasserburg,et al. 230Th232Th systematics in the central Pacific Ocean: The sources and the fates of thorium , 1996 .
[30] J. Overpeck,et al. Rapid climate changes in the tropical Atlantic region during the last deglaciation , 1996, Nature.
[31] E. Yu,et al. Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data , 1996, Nature.
[32] R. Anderson,et al. 231Pa/230Th ratios in sediments as a proxy for past changes in Southern Ocean productivity , 1993, Nature.
[33] W. Broecker,et al. Transport and burial rates of 10Be and 231Pa in the pacific-ocean during the holocene period , 1992 .
[34] G. Wasserburg,et al. 234U—238U—230Th—232Th systematics in saline groundwaters from central Missouri , 1990 .
[35] W. Broecker,et al. Boundary scavenging in the Pacific Ocean: a comparison of 10Be and 231Pa , 1990 .
[36] L. Balistrieri,et al. Oceanic trace metal scavenging: the importance of particle concentration , 1988 .
[37] H. Yang,et al. Scavenging of thorium in the ocean , 1987 .
[38] G. Wasserburg,et al. 238 U, 234 U and 232 Th in seawater , 1986 .
[39] P. Brewer,et al. Removal of 230Th and 231Pa at ocean margins , 1983 .
[40] P. Brewer,et al. Removal of230Th and231Pa from the open ocean , 1983 .
[41] R. Anderson,et al. Distribution of thorium isotopes between dissolved and particulate forms in the deep sea , 1982 .
[42] P. Brewer,et al. 210Pb/226Ra and 210Po/210Pb disequilibria in seawater and suspended particulate matter , 1976 .