Quoting from a paper that was accepted: «Many palaeoclimate records from the North Atlantic region show a pattern of rapid climate oscillations, the so - called Dansgaard — Oeschger events, with a quasi-periodicity of ∼ 1,470 years for
the late glacial period» http://www.nature.com/articles/nature04121
Not exact matches
«Although this
period is around the
late glacial maximum, there is a blip at 23,000 years during which time it was milder.»
A prehistoric human skeleton found on the Yucatán Peninsula is at least 13,000 years old and most likely dates from a
glacial period at the end of the most recent ice age, the
late Pleistocene.
However,
latest scientific studies show that this marine species colonized the Mediterranean between 20,000 and 200,000 years ago, so the colonization event took place before the last
glacial period.
During
Late Pleistocene
glacial periods, ice volumes increased markedly along the Antarctic Peninsula [1], possibly reaching 2350 m at Mount Jackson.
The park covers 140 km ², of which 16 km ² is granite islands, formed by upwellings of hot magma during the Tertiary - Cretaceous
period some 65 million years ago, then
later smoothed by
glacial ice and wave action of the sea.
Second, sub-stage 19c lies near the middle - Pleistocene, a time when the climate system appears to have been most clearly transitioning from smaller amplitude, shorter
period, and more symmetric
glacial cycles, to the larger, longer, and more saw - toothed
glacial cycles of the
late Pleistocene.
But a major problem exists for the standard orbital hypothesis of glaciation:
Late Pliocene and early Pleistocene
glacial cycles occur at intervals of 40 ky (8 — 11), matching the obliquity
period, but have negligible 20 - ky variability.
Similarly, warm
periods with
glacial retreat occurred within the
late Cenozoic cool
period during the
late Oligocene and early Miocene epochs.