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Persistent link between solar activity and Greenland climate during the Last Glacial Maximum
Adolphi, F., Muscheler, R., Svensson, A., Aldahan, A., Possnert, G., Beer, J., … Thiéblemont, R. (2014). Persistent link between solar activity and Greenland climate during the Last Glacial Maximum. Nature Geoscience, 7(9), 662-666. https://doi.org/10.1038/ngeo2225
Variable <SUP>10</SUP>Be fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?
Ljung, K., Björck, S., Muscheler, R., Beer, J., & Kubik, P. W. (2007). Variable 10Be fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record? Quaternary Science Reviews, 26(7-8), 829-835. https://doi.org/10.1016/j.quascirev.2006.12.016
Reply to the comment by Bard et al. on "Solar activity during the last 1000 yr inferred from radionuclide records"
Muscheler, R., Snowball, I., Joos, F., Müller, S. A., Beer, J., & Vonmoos, M. (2007). Reply to the comment by Bard et al. on "Solar activity during the last 1000 yr inferred from radionuclide records". Quaternary Science Reviews, 26(17-18), 2304-2308. https://doi.org/10.1016/j.quascirev.2007.06.014
Solar activity during the last 1000 yr inferred from radionuclide records
Muscheler, R., Joos, F., Beer, J., Müller, S. A., Vonmoos, M., & Snowball, I. (2007). Solar activity during the last 1000 yr inferred from radionuclide records. Quaternary Science Reviews, 26(1-2), 82-97. https://doi.org/10.1016/j.quascirev.2006.07.012
Geomagnetic field intensity during the last 60,000 years based on <SUP>10</SUP>Be and <SUP>36</SUP>Cl from the Summit ice cores and <SUP>14</SUP>C
Muscheler, R., Beer, J., Kubik, P. W., & Synal, H. A. (2005). Geomagnetic field intensity during the last 60,000 years based on 10Be and 36Cl from the Summit ice cores and 14C. Quaternary Science Reviews, 24(16-17), 1849-1860. https://doi.org/10.1016/j.quascirev.2005.01.012
Causes and timing of the 8200yr BP event inferred from the comparison of the GRIP <SUP>10</SUP>Be and the tree ring Δ<SUP>14</SUP>C record
Muscheler, R., Beer, J., & Vonmoos, M. (2004). Causes and timing of the 8200yr BP event inferred from the comparison of the GRIP 10Be and the tree ring Δ14C record. Quaternary Science Reviews, 23(20-22), 2101-2111. https://doi.org/10.1016/j.quascirev.2004.08.007
Changes in the carbon cycle during the last deglaciation as indicated by the comparison of <SUP>10</SUP>Be and <SUP>14</SUP>C records
Muscheler, R., Beer, J., Wagner, G., Laj, C., Kissel, C., Raisbeck, G. M., … Kubik, P. W. (2004). Changes in the carbon cycle during the last deglaciation as indicated by the comparison of 10Be and 14C records. Earth and Planetary Sciences Letters, 219, 325-340. https://doi.org/10.1016/S0012-821X(03)00722-2
Co-precipitated silver-metal oxide aggregates for accelerator mass spectrometry of <SUP>10</SUP>Be and <SUP>26</SUP>Al
Stone, J., Fifield, K., Beer, J., Vonmoos, M., Obrist, C., Grajcar, M., … Caffee, M. (2004). Co-precipitated silver-metal oxide aggregates for accelerator mass spectrometry of 10Be and 26Al. Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and Atoms, 223-224, 272-277. https://doi.org/10.1016/j.nimb.2004.04.055
Cosmogenic nuclides during isotope stages 2 and 3
Beer, J., Muscheler, R., Wagner, G., Laj, C., Kissel, C., Kubik, P. W., & Synal, H. A. (2002). Cosmogenic nuclides during isotope stages 2 and 3. Quaternary Science Reviews, 21(10), 1129-1139. https://doi.org/10.1016/S0277-3791(01)00135-4
Past climate changes derived from isotope measurements in polar ice cores
Beer, J., Muscheler, R., Wagner, G., & Kubik, P. W. (2002). Past climate changes derived from isotope measurements in polar ice cores. In C&S Papers Series: Vol. 13/P. Study of environmental change using isotope techniques. Proceedings (pp. 265-273).
Geomagnetic field intensity, North Atlantic Deep Water circulation and atmospheric Δ<sup>14</sup>C during the last 50 kyr
Laj, C., Kissel, C., Mazaud, A., Michel, E., Muscheler, R., & Beer, J. (2002). Geomagnetic field intensity, North Atlantic Deep Water circulation and atmospheric Δ14C during the last 50 kyr. Earth and Planetary Sciences Letters, 200(1-2), 177-190. https://doi.org/10.1016/S0012-821X(02)00618-0
Geomagnetic intensity and inclination variations at Hawaii for the past 98 kyr from core SOH-4 (Big Island): a new study and a comparison with existing contemporary data
Laj, C., Kissel, C., Scao, V., Beer, J., Thomas, D. M., Guillou, H., … Wagner, G. (2002). Geomagnetic intensity and inclination variations at Hawaii for the past 98 kyr from core SOH-4 (Big Island): a new study and a comparison with existing contemporary data. Physics of the Earth and Planetary Interiors, 129(3-4), 205-243. https://doi.org/10.1016/S0031-9201(01)00291-6
High-resolution analyses of an early Holocene climate event may imply decreased solar forcing as an important climate trigger
Björck, S., Muscheler, R., Kromer, B., Andresen, C. S., Heinemeier, J., Johnsen, S. J., … Veski, S. (2001). High-resolution analyses of an early Holocene climate event may imply decreased solar forcing as an important climate trigger. Geology, 29(12), 1107-1110. https://doi.org/10.1130/0091-7613(2001)029<1107:HRAOAE>2.0.CO;2
Persistent solar influence on North Atlantic climate during the Holocene
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M. N., Showers, W., … Bonani, G. (2001). Persistent solar influence on North Atlantic climate during the Holocene. Science, 294(5549), 2130-2136. https://doi.org/10.1126/science.1065680
Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both?
Marchal, O., Stocker, T. F., & Muscheler, R. (2001). Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both? Earth and Planetary Sciences Letters, 185(3-4), 383-395. https://doi.org/10.1016/S0012-821x(00)00383-6
Letzte Kaltphase mit reduzierter Ozeanströmung. Beryllium-Isotope bestätigen bisherige Theorie
Muscheler, R. (2001). Letzte Kaltphase mit reduzierter Ozeanströmung. Beryllium-Isotope bestätigen bisherige Theorie. Neue Zürcher Zeitung (Jan.), 44.
Reconstruction of the paleoaccumulation rate of central Greenland during the last 75 kyr using the cosmogenic radionuclides <SUP>36</SUP>Cl and <SUP>10</SUP>Be and geomagnetic field intensity data
Wagner, G., Laj, C., Beer, J., Kissel, C., Muscheler, R., Masarik, J., & Synal, H. A. (2001). Reconstruction of the paleoaccumulation rate of central Greenland during the last 75 kyr using the cosmogenic radionuclides 36Cl and 10Be and geomagnetic field intensity data. Earth and Planetary Sciences Letters, 193, 515-521. https://doi.org/10.1016/S0012-821X(01)00504-0
Changes in deep-water formation during the Younger Dryas event inferred from <SUP>10</SUP>Be and <SUP>14</SUP>C records
Muscheler, R., Beer, J., Wagner, G., & Finkel, R. C. (2000). Changes in deep-water formation during the Younger Dryas event inferred from 10Be and 14C records. Nature, 408(6812), 567-570. https://doi.org/10.1038/35046041
Chlorine-36 evidence for the Mono Lake event in the Summit GRIP ice core
Wagner, G., Beer, J., Laj, C., Kissel, C., Masarik, J., Muscheler, R., & Synal, H. A. (2000). Chlorine-36 evidence for the Mono Lake event in the Summit GRIP ice core. Earth and Planetary Sciences Letters, 181, 1-6. https://doi.org/10.1016/S0012-821x(00)00196-5