Anderson, D. M.: Attenuation of millennial-scale events by bioturbation
in marine sediments, Paleoceanography, 16, 352–357, 2001. a
Bracewell, R. N.: The Fourier transform and its applications, vol. 31999,
McGraw-Hill, New York, 1986. a
Buck, C. E.: Bayesian Chronological Data Interpretation: Where Now?, Lecture
Notes in statistics, New Nork, Springer, 1–24, 2004. a
Caley, T., Roche, D. M., Waelbroeck, C., and Michel, E.: Oxygen stable isotopes during the Last Glacial Maximum climate: perspectives from data–model (iLOVECLIM) comparison, Clim. Past, 10, 1939–1955,
https://doi.org/10.5194/cp-10-1939-2014, 2014.
a
Clark, P. U., Shakun, J. D., Baker, P. A., Bartlein, P. J., Brewer, S., Brook,
E., Carlson, A. E., Cheng, H., Kaufman, D. S., Liu, Z., and Others:
Global climate evolution during the last deglaciation, P.
Natl. Acad. Sci. USA, 109, E1134—-E1142, 2012. a
Dee, S., Emile-Geay, J., Evans, M. N., Allam, A., Steig, E. J., and Thompson,
D.: PRYSM: An open-source framework for PRoxY System Modeling, with
applications to oxygen-isotope systems, J. Adv. Model.
Earth Sy., 7, 1220–1247,
https://doi.org/10.1002/2015MS000447,
2015.
a
Elderfield, H., Vautravers, M., and Cooper, M.: The relationship between shell
size and Mg/Ca, Sr/Ca,
δ18O, and c
δ13C of species of planktonic
foraminifera, Geochem. Geophy. Geosy., 3, 1–13,
https://doi.org/10.1029/2001GC000194,
2002.
a
Evans, M. N., Tolwinski-Ward, S. E., Thompson, D. M., and Anchukaitis, K. J.:
Applications of proxy system modeling in high resolution
paleoclimatology, Quaternary Sci. Rev., 76, 16–28, 2013.
a,
b
Fairchild, I. J., Smith, C. L., Baker, A., Fuller, L., Spötl, C., Mattey,
D., and McDermott, F.: Modification and preservation of environmental
signals in speleothems, Earth-Sci. Rev., 75, 105–153,
https://doi.org/10.1016/j.earscirev.2005.08.003, 2006.
a,
b
Haam, E. and Huybers, P.: A test for the presence of covariance
between time-uncertain series of data with application to the Dongge
Cave speleothem and atmospheric radiocarbon records,
Paleoceanography, 25,
https://doi.org/10.1029/2008PA001713, 2010.
a
Hakim, G. J., Emile-Geay, J., Steig, E. J., Noone, D., Anderson, D. M., Tardif,
R., Steiger, N., and Perkins, W. A.: The last millennium climate reanalysis
project: Framework and first results, J. Geophys. Res., 121,
6745–6764,
https://doi.org/10.1002/2016JD024751, 2016.
a
Huybers, P. and Curry, W.: Links between annual, Milankovitch
and continuum temperature variability, Nature, 441, 329–332, 2006. a
Huybers, P. and Wunsch, C.: A depth-derived Pleistocene age model: Uncertainty
estimates, sedimentation
variability, and nonlinear climate change,
Paleoceanography, 19, PA1028,
https://doi.org/10.1029/2002PA000857, 2004.
a
MARGO Project Members: Constraints on the magnitude and patterns of
ocean cooling at the Last Glacial Maximum, Nat.
Geosci., 2, 127–132, 2009.
a,
b
McGee, D., Winckler, G., Stuut, J. B. W., and Bradtmiller, L. I.:
The magnitude, timing and abruptness of changes in North
African dust deposition over the last 20,000 yr, Earth Planet.
Sc. Lett., 371, 163–176, 2013. a
Pisias, N. G. and Mix, A. C.: Aliasing of the geologic record and the
search for long-period Milankovitch cycles, Paleoceanography, 3,
613–619, 1988.
a,
b
Rhines, A. and Huybers, P.: Estimation of spectral power laws in time
uncertain series of data with application to the Greenland ice sheet project
2
δ18O
record, J. Geophys. Res.-Atmos., 116, 1–9,
https://doi.org/10.1029/2010JD014764, 2011.
a
Shannon, C. E.: Communication in the presence of noise, P. IRE, 37, 10–21, 1949. a
Telford, R. J., Heegaard, E., and Birks, H. J. B.: The intercept is a poor
estimate of a calibrated radiocarbon age, Holocene, 14, 296–298,
https://doi.org/10.1191/0959683604hl707fa, 2004.
a
Van Sebille, E., Scussolini, P., Durgadoo, J. V., Peeters, F. J., Biastoch,
A., Weijer, W., Turney, C., Paris, C. B., and Zahn, R.: Ocean currents
generate large footprints in marine palaeoclimate proxies, Nat.
Commun., 6, 1–8,
https://doi.org/10.1038/ncomms7521,
2015.
a,
b
von Albedyll, L., Opel, T., Fritzsche, D., Merchel, S., Laepple, T., and Rugel,
G.: 10 Be in the Akademii Nauk ice core–first
results for CE 1590–1950 and implications for future chronology
validation, J. Glaciol., 1–9,
https://doi.org/10.1017/jog.2017.19,
2017.
a,
b
Wunsch, C.: The North Atlantic general circulation
west of 50~W determined by inverse methods, Rev.
Geophys., 16, 583–620, 1978. a
Wunsch, C.: 0n sharp spectral lines in the climate record and the millennial
peak, Paleoceanography, 15, 417–424, 2000.
a,
b,
c
Wunsch, C.: Greenland–Antarctic phase relations and
millennial time-scale climate fluctuations in the Greenland
ice-cores, Quaternary Sci. Rev., 22, 1631–1646, 2003.
a,
b
Wunsch, C. and Gunn, D. E.: A densely sampled core and climate
variable aliasing, Geo-Mar. Lett., 23, 64–71, 2003.
a,
b
Zhao, N., Marchal, O., Keigwin, L., Amrhein, D., and Gebbie, G.: A Synthesis
of Deglacial Deep-Sea Radiocarbon Records and Their (In)Consistency With
Modern Ocean Ventilation, Paleoceanogr. Paleocl., 33,
128–151, 2018. a