Based upon the features of nannofossil composition, distribution, abundance
and diversity, the fossil-bearing sediments exposed by five drill holes in
the offshore area of southern Hongkong can be divided into the upper Middl
e Pleistocene, the Upper Pleistocene and Holocene. There were two palaeocli
matic stages in the Holocene in this area according to fossil palaeoecologi
c and sedimentation analyses: the temperature-rising stage and the warm sta
ge. The latter involves two temperature-falling periods, which could be the
major factor causing sea-level fall during that time.