摘要：The time period between the beginning
of Heinrich event #1 (H-1)
and the onset of the B.lling/Aller.d
rivals the Younger Dryas in importance
to our understanding of
how the planet responds to abrupt
mode switches. This interval also
constitutes the onset of the most
recent termination, arguably the
most fundamental climate shift of
the last 100-kyr glacial cycle. As
some of the responses during this
time appear to be mutually contradictory,
we term it the “Mystery
Interval”.
