Amongst the well - known proxies that have revealed a millennial - scale climate variability during the Holocene, the ice - rafted debris (IRD) indices in the North Atlantic developed by Bond et al. (1997, 2001) present a cyclicity of 1470 ± 500 years, which matches the 1228 ± 327 -
year periodicity evidenced in the Mar Menor, considering the respective uncertainties in the periodicities.
Not exact matches
It has also been known that a component of the variability seems to have a full period of about 60
years although the
evidence has not been strong on any real
periodicity or even quasi-
periodicity.
These events not only show a corresponding age and correct
periodicity, but they also constitute the highest petrological tracer peaks for each 2400
year period, suggesting that they were the strongest cooling periods at each time, as glaciological, biological and geophysical
evidence also supports.
The
evidence, however, shows that the HCO displays a millennial
periodicity in Bond events, with single isolated peaks separated by ~ 1000
years, while the Neoglacial shows a more complex picture with multiple peaks not so well resolved and a more irregular spacing.
I don't know if the 4672 -
year periodicity is also present in the ¹⁴ C
evidence.
Evidence is presented specifying the timing and amplitude of the natural 60 + / -
year and, more importantly, 1,000
year periodicities (observed emergent behaviors) that are so obvious in the temperature record.