Presence of the Solar de Vries Cycle (∼205 years) during the Last Ice Age

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Long-term indirect indices of solar variability (2000, background): “For a more reliable separation independent information is required, e. g. in the form of paleomagnetism derived from remanence measurements on sediments (Wagner et al., 2000a).”
The solar magnetic field (2006, background): “. Spectral analysis of the isotope data in fact reveals signicant signals at periods around 90 years (the Gleissberg cycle, which is also found in the sunspot record [47]), 210 years, and 2200 years [45, 48, 49]. The solar magnetic eld 13 3.4. A ‘fossil’ magnetic eld in the radiative interior? Owing”
Large variations in Holocene solar activity: Constraints from 10Be in the Greenland Ice Core Project ice core (2006, methodology): “Greenland Ice Core Project (GRIP) ice core (Summit, Central Greenland) covering several hundred thousand years [Baumgartner et al., 1997b; Muscheler et al., 2004; Wagner et al., 2001; Yiou et al., 1997].”
El Niño as a mediator of the solar influence on climate (2007, background): “The record clearly contains the documented centennial variability of the Gleissberg ( 88 years) and DeVries ( 205 years) cycles [Peristykh and Damon, 2003; Wagner et al., 2001], as well as significant power around 500 years, and a broad band around 1000 years.”