Svm. Clube et Wm. Napier, GALACTIC DARK-MATTER AND TERRESTRIAL PERIODICITIES, Quarterly Journal of the Royal Astronomical Society, 37(4), 1996, pp. 617-642
Analysis of recent geological databases reveals the presence of a simi
lar to 26.5 Myr periodicity in the terrestrial record of the last simi
lar to 200 Myr. The same periodicity is found to be present, at a high
confidence level, in the record of impact cratering on Earth. It thus
appears that global disturbances are modulated or caused largely by e
xogenous forcing. The likely source is a periodic comet influx caused
by Oort cloud disturbance as the Sun oscillates vertically through the
Galactic disk. The Earth may thus be regarded as a probe of the disk
environment; and to account for the periodicity, the Galactic disk is
required to have a substantial dark matter component (similar to 0.15
M. pc(-3)). The purpose of this paper is to review the relevant observ
ational framework, and to describe the basic astro- and geophysical pr
ocesses which now seem to underpin evolution on Earth. Attention is dr
awn in particular to recent oceanic sediment evidence which seems to c
onfirm a continuous sequence of events from periodic Galactic forcing
through the influx of giant comets (diameter greater than or similar t
o 100 km) into stable sub-Jovian orbits at the rate of similar to 10 M
yr(-1) and the resulting climatic disturbances due to their disintegra
tion in near-Earth space. This rate, producing episodic multiple threa
ts to the Earth by bodies in the sub-kilometre range, is numerically c
omparable to the long-term cratering flux to Earth owing to 'one-off'
greater than or similar to 1 km asteroids and comets. The resulting cu
rrent hazard to Earth, amounting to a more substantial input and explo
sion megatonnage in toto, is both more complex and more profound.