There are still more problems around the dating of the last interglacial, the Eemian aka Sangamonian.
http://www.sciencemag.org/cgi/content/abstract/283/5399/197
..The early (about 140,000 years ago) start of the penultimate deglaciation, well before the peak in insolation, is consistent with the Devils Hole chronology..
and
http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V61-4NPG0G1-5&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=24ce14d831a1e24f41f6caa61725cd9d
...The age of the younger flowstone demonstrates that the early highstand occurred before 134.8 ± 2.0 ka, and uplift arguments suggest that the bioherms are unlikely to be older than 136 ka. These data are consistent with the notion that most of termination II (TII) sea-level rise had occurred before 135 ka; indeed they suggest sea-level at this time reached about 2–4 (± 4) m below present sea-level, 6–18 (± 4) m higher than previous estimates. This early highstand was itself punctuated by a rapid sea-level oscillation of > 10 m (as yet undated), and this oscillation, supported by new TII sea-level data from the Red Sea [Siddall, M., Bard, E., Rohling, E.J., Hemleben, C., 2006, Sea-level reversal during termination II, Geology, 34, 817–820.], probably occurred in about 1000 yr.
but also similar problems earlier http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VBC-4K717WK-1&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=f35a8571598ae887ad898cb5755cfc24
...But U–Th and δ18O data indicate the presence of an additional highstand which post-dates the expected end of MIS 7 (*) by up to 10 ka. This event is also seen in coral reconstructions of sea-level. It suggests that sea-level is not responding in any simple way to northern-hemisphere summer insolation,...
..Although the most extreme of these dates may not be reliable (based on the low-aragonite content of the sediment) the other three appear robust and suggest that full MIS 9 interglacial conditions were established at 343 ka. This is ≈8 ka prior to the date expected if this warm period were driven by northern-hemisphere summer insolation
(*) MIS= Maritime Isotope Stage, commonly used counted periods of general high and low isotope ratio's (δ
18O) in the oceanic sediment cores, we are now in MIS1, MIS2 was the last glacial maximum.