[tz] tzfiles contain Unix epoch for the first transition time
Paul Eggert
eggert at cs.ucla.edu
Sat Aug 15 17:17:50 UTC 2015
Steve Allen wrote:
> Williams studied tidal rhythmites and found a nearly constant number
> of about 410 solar days per year from 2 billion to 1 billion years
> before present, which is about 77000 SI seconds in one day.
> http://onlinelibrary.wiley.com/doi/10.1029/1999RG900016/abstract
Thanks for mentioning that; I wasn't aware of this work. It appears, though,
that there's still considerable uncertainty about how long the day was way back
when. A recent review says that although tidal rhythmite analysis may help
estimate ancient lunar orbital periods in terms of lunar days/month, estimating
the length of the ancient Earth day remains uncertain because we don't know the
length of the ancient lunar sidereal month.
This is in contrast to something else I think you mentioned a while ago, namely
the length of the day going back to about 750 BC, for which Richard Stephenson
and coworkers have amassed historical eclipse records showing that our UTC-based
clocks would be off by about three hours if we naively took them back to the
year 0. See, for example, Sauter et al's reconstruction of the total solar
eclipse of 0319-05-06 which legend says converted Mirian III of Iberia to
Christianity.
Longhitano SG, Mellere D, Steel RJ, Ainsworth RB. Tidal depositional systems in
the rock record: A review and new insights. Sedimentary Geology 279, 2-22
(2012-11-20). http://dx.doi.org/10.1016/j.sedgeo.2012.03.024
Morrison L. The length of the day: Richard Stephenson’s contribution.
Astrophysics and Space Science Proceedings 43 (2015) 3-10.
http://dx.doi.org/10.1007/978-3-319-07614-0_1
Sauter J, Simonia I, Stephenson FR, Orchiston W. The legendary fourth-century
total solar eclipse in Georgia: Fact or fantasy? Astrophysics and Space Science
Proceedings Volume 43 (2015) 25-45. http://dx.doi.org/10.1007/978-3-319-07614-0_3
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