Effects of climate and the cosmic-ray flux on the 10Be content of marine sediments
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[1] M. Vautravers,et al. Gulf Stream variability during marine isotope stage 3 , 2004 .
[2] G. Henderson,et al. The use of foraminifera as a record of the past neodymium isotope composition of seawater , 2004 .
[3] A. Mangini,et al. Beryllium-10 in deep-sea sediments: a tracer for the Earth's magnetic field intensity during the last 200,000 years , 2003 .
[4] Simon Turner,et al. Uranium-series geochemistry , 2003 .
[5] G. Henderson,et al. The U-series Toolbox for Paleoceanography , 2003 .
[6] W. Chaisson,et al. Astronomical age models for Pleistocene drift sediments from the western North Atlantic (ODP Sites 1055-1063) , 2002 .
[7] C. Laj,et al. South Atlantic and North Atlantic geomagnetic paleointensity stacks (0-80 ka): implications for inter-hemispheric correlation , 2002 .
[8] S. Hemming,et al. Laschamp Excursion at Mono Lake , 2002 .
[9] G. Acton,et al. Paleomagnetic records of Stage 3 excursions, Leg 172 , 2001 .
[10] J. Southon,et al. 26Al, 10Be and U–Th isotopes in Blake Outer Ridge sediments: implications for past changes in boundary scavenging , 2001 .
[11] G. Acton,et al. 10. BRUNHES CHRON MAGNETIC FIELD EXCURSIONS RECOVERED FROM LEG 172 SEDIMENTS , 2001 .
[12] P. Damon,et al. Geomagnetic modulation of the late Pleistocene cosmic-ray flux as determined by 10Be from Blake Outer Ridge marine sediments , 2000 .
[13] M. Frank. Comparison of cosmogenic radionuclide production and geomagnetic field intensity over the last 200 000 years , 2000, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.
[14] C. Laj,et al. Rapid climatic variations during marine isotopic stage 3: magnetic analysis of sediments from Nordic Seas and North Atlantic , 1999 .
[15] T. Ku,et al. OCEANIC 231PA/230TH RATIO INFLUENCED BY PARTICLE COMPOSITION AND REMINERALIZATION , 1999 .
[16] Y. S. Kok. Climatic influence in NRM and 10Be-derived geomagnetic paleointensity data , 1999 .
[17] T. Johnson,et al. Geomagnetic field intensity from 71 to 12 ka as recorded in deep‐sea sediments of the Blake Outer Ridge, North Atlantic Ocean , 1998 .
[18] A. Aldahan,et al. A HIGH-RESOLUTION 10BE PROFILE FROM DEEP SEA SEDIMENT COVERING THE LAST 70KA : INDICATION FOR GLOBALLY SYNCHRONIZED ENVIRONMENTAL EVENTS , 1998 .
[19] M. Suter,et al. A 200 kyr record of cosmogenic radionuclide production rate and geomagnetic field intensity from 10Be in globally stacked deep-sea sediments , 1997 .
[20] J. Valet,et al. Relative variations in geomagnetic intensity from sedimentary records: the past 200 , 1996 .
[21] S. Colman. An 84-kyr paleomagnetic record from the sediments , 1996 .
[22] C. Laj,et al. Relative changes of the geomagnetic field intensity during the last 280 kyear from piston cores in the Açores area , 1996 .
[23] C. Laj,et al. The relationship between 10Be and geomagnetic field strength records in central North Atlantic sediments during the last 80 ka , 1995 .
[24] J. Beer,et al. Evidence for enhanced 10Be deposition in Mediterranean sediments 35 kyr BP , 1995 .
[25] P. Damon,et al. Enhanced cosmic‐ray production of 10Be coincident with the Mono Lake and Laschamp Geomagnetic Excursions , 1995 .
[26] A. Roberts,et al. Normalised natural remanent magnetisation intensity during the last 240 000 years in piston cores from the central North Atlantic Ocean: geomagnetic field intensity or environmental signal? , 1995 .
[27] T. Yamazaki,et al. Long-term secular variation of the geomagnetic field during the last 200 kyr recorded in sediment cores from the western equatorial Pacific , 1994 .
[28] N. Shackleton,et al. Relative geomagnetic intensity of the field during the last 140 ka , 1992 .
[29] F. Guichard,et al. Paleointensity of the geomagnetic field during the last 80,000 years , 1992 .
[30] P. Damon,et al. The global beryllium 10 cycle , 1991 .
[31] R. Karlin,et al. A sixty thousand year paleomagnetic record from Gulf of California sediments: secular variation, late Quaternary excursions and geomagnetic implications , 1989 .
[32] D. Bourlès,et al. 10Be and 9Be in marine sediments and their potential for dating , 1989 .
[33] Deepak Lal,et al. Theoretically expected variations in the terrestrial cosmic-ray production rates of isotopes , 1988 .
[34] J. Beer,et al. 10Be: Half-life and AMS-standards , 1987 .
[35] J. Jouzel,et al. Evidence for two intervals of enhanced 10Be deposition in Antarctic ice during the last glacial period , 1987, Nature.
[36] J. D. Hays,et al. Age Dating and the Orbital Theory of the Ice Ages: Development of a High-Resolution 0 to 300,000-Year Chronostratigraphy , 1987, Quaternary Research.
[37] M. Bacon. Glacial to interglacial changes in carbonate and clay sedimentation in the Atlantic Ocean estimated from 230Th measurements , 1984 .