10Be evidence for delayed acquisition of remanent magnetization in marine sediments: Implication for a new age for the Matuyama–Brunhes boundary
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[1] F. Blanckenburg,et al. Determination of the 10Be half-life by multicollector ICP-MS and liquid scintillation counting , 2010 .
[2] G. Dollinger,et al. A new value for the half-life of 10Be by Heavy-Ion Elastic Recoil Detection and liquid scintillation counting , 2010 .
[3] A. Roberts,et al. Post-depositional remanent magnetization lock-in and the location of the Matuyama-Brunhes geomagnetic reversal boundary in marine and Chinese loess sequences , 2008 .
[4] J. Jouzel,et al. An ice core perspective on the age of the Matuyama-Brunhes boundary , 2008 .
[5] P. Renne,et al. Synchronizing Rock Clocks of Earth History , 2008, Science.
[6] M. Knudsen,et al. In-phase anomalies in Beryllium-10 production and palaeomagnetic field behaviour during the Iceland Basin geomagnetic excursion , 2008 .
[7] T. Stocker,et al. Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10 , 2007 .
[8] Kenji Kawamura,et al. The EDC3 chronology for the EPICA Dome C ice core , 2007 .
[9] A. Schilt,et al. Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years , 2007, Science.
[10] P. Kubik,et al. Highly resolved Beryllium-10 record from ODP Site 1089—A global signal? , 2007 .
[11] J. Southon,et al. Absolute calibration of 10Be AMS standards , 2007 .
[12] Karl Fabian,et al. Paleomagnetic reconstruction of the global geomagnetic field evolution during the Matuyama/Brunhes transition: Iterative Bayesian inversion and independent verification , 2007 .
[13] J. Jouzel,et al. 10Be evidence for the Matuyama–Brunhes geomagnetic reversal in the EPICA Dome C ice core , 2006, Nature.
[14] L. Tauxe,et al. Depositional remanent magnetization: Toward an improved theoretical and experimental foundation , 2006 .
[15] Hirokuni Oda,et al. A geomagnetic paleointensity stack between 0.8 and 3.0 Ma from equatorial Pacific sediment cores , 2005 .
[16] L. Meynadier,et al. Geomagnetic dipole strength and reversal rate over the past two million years , 2005, Nature.
[17] B. Jicha,et al. Structural and temporal requirements for geomagnetic field reversal deduced from lava flows , 2005, Nature.
[18] N. Shackleton,et al. An Atlantic lead over Pacific deep-water change across Termination I: implications for the application of the marine isotope stage stratigraphy , 2005 .
[19] M. Raymo,et al. A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ18O records , 2005 .
[20] A. Roberts,et al. Why are geomagnetic excursions not always recorded in sediments? Constraints from post-depositional remanent magnetization lock-in modelling , 2004 .
[21] Xixi Zhao,et al. Matuyama-Brunhes reversal and Kamikatsura event on Maui: paleomagnetic directions, 40 Ar/ 39 Ar ages and implications , 2004 .
[22] J. Overpeck,et al. 14C Activity and Global Carbon Cycle Changes over the Past 50,000 Years , 2004, Science.
[23] James G. Ogg,et al. A Geologic Time Scale 2004: CONCEPTS AND METHODS , 2004 .
[24] 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 .
[25] A. Roberts,et al. A 2.14-Myr astronomically tuned record of relative geomagnetic paleointensity from the western Philippine Sea , 2003 .
[26] K. Wei,et al. Astronomically calibrated ages for geomagnetic reversals within the Matuyama chron , 2002 .
[27] H. Synal,et al. Cosmogenic nuclides during Isotope Stages 2 and 3. , 2002 .
[28] C. Kissel,et al. Geomagnetic paleointensity and environmental record from Labrador Sea core MD95-2024: global marine sediment and ice core chronostratigraphy for the last 110 kyr , 2000 .
[29] H. Synal,et al. Reconstruction of the geomagnetic field between 20 and 60 kyr BP from cosmogenic radionuclides in the GRIP ice core , 2000 .
[30] J. Beer,et al. North Atlantic palaeointensity stack since 75ka (NAPIS–75) and the duration of the Laschamp event , 2000, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.
[31] J. Channell,et al. Geomagnetic palaeointensities and astrochronological ages for the Matuyama–Brunhes boundary and the boundaries of the Jaramillo Subchron: palaeomagnetic and oxygen isotope records from ODP Site 983 , 2000, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.
[32] C. Richter,et al. Paleointensity record from Pleistocene sediments (1.4-0 Ma) off the California margin , 1999 .
[33] H. Igel,et al. Lateral mixing and advection of reactive isotope tracers in ocean basins: observations and mechanisms , 1999 .
[34] J. McManus,et al. Orbital modulation of the Earth's magnetic field intensity , 1998, Nature.
[35] B. Boudreau. Mean mixed depth of sediments: The wherefore and the why , 1998 .
[36] 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 .
[37] T. Herbert,et al. Astronomical calibration of the Matuyama-Brunhes boundary: Consequences for magnetic remanence acquisition in marine carbonates and the Asian loess sequences , 1996 .
[38] L. Tauxe,et al. A precursor to the Matuyama/Brunhes transition-field instability as recorded in pelagic sediments , 1996 .
[39] B. Boudreau. Is burial velocity a master parameter for bioturbation , 1994 .
[40] P. Damon,et al. The global beryllium 10 cycle , 1991 .
[41] P. deMenocal,et al. Depth of post-depositional remanence acquisition in deep-sea sediments: a case study of the Brunhes-Matuyama reversal and oxygen isotopic Stage 19.1 , 1990 .
[42] W. B. Harland,et al. A Geologic time scale , 1982 .
[43] K. Verosub. Depositional and postdepositional processes in the magnetization of sediments , 1977 .
[44] D. Kent. Post-depositional Remanent Magnetisation in Deep-sea Sediment , 1973, Nature.
[45] E. Irving. POST‐DEPOSITIONAL DETRITAL REMANENT MAGNETIZATION IN A SYNTHETIC SEDIMENT , 1964 .