The Chicxulub impact structure exhibits asymmetries in its geophysical
signatures that closely resemble asymmetries produced by oblique impa
cts in laboratory experiments and recognized on planetary surfaces, Th
ese asymmetric signatures suggest a trajectory for the Chicxulub bolid
e from the southeast to the northwest at a 20 degrees-30 degrees angle
from the horizontal. As a result, biotic extinctions may have been mo
st severe and catastrophic in the Northern Hemisphere, Geographic vari
ation in the magnitude of the Cretaceous-Tertiary (K-T) ''fern spike''
and palynofloral extinctions are consistent with the proposed traject
ory.