Orbital Resonances

The mean solar day loses about 230 seconds over the sidereal lunar
orbit, SLO, every million years.
Take the present SLO, 27.32166 days and divide by 27.5. Subtract
the result from one and multiply by the SLO, 2360591.47s for the
result of 15408s. Divide this by 230s for the result of 66.5 million
years.
Follow the same procedure for 28, 28.5 and 29 msds per SLO to get
the result of 249.8, 430 and 606 million years ago respectively.
These results are very close to the cretaceous, permian,
ordovicean
and precambrian extinctions respectively.
At these times the earth's magnetic field began reversing at an
increased rate of as much as 35000 percent, and sea leavels began to
rise at high latitudes and fall at middle latitudes. Temperatures
dropped with the draining of inland seas and the icing of the poles.
Could there be a siderial link between the moon's orbit and the
earth's rotation?

Further, Heinrich events, the calving off of iceburgs that leave a
layer of sediment an the atlantic floor, occured 65, 52, 39 and 12.6
thousand years ago. These correspond to the times when the earth's
axis was perpendicular to the poles of the Cosmic microwave
background. Could there be a cosmic directional force?

stephen kearney