古新世—始新世界线的全球事件

深海钻探揭示的古新世－析世界线许多全球性变化引起了地质学家的普遍关注。这些变化表现在岩性，粘土矿物组合，大陆植物群，大陆哺乳动物，钙质超微化石，底栖有孔虫，氧碳同位素，大气环流强度，海洋环流模式，海平面等方面，通过对古新世－始新世地层沉积学、古生物学、古气候学和古海洋学的研究，确认古新世－始新世地层界线是全球构造事件的结果，表现为全球板块边界重组，扩张中心和转换断层模式改变，海底热液活动呈一至二个

GLOBAL EVENTS AT THE PALEOCENE-EOCENE BOUNDARY

Lots of global changes at the Paleocene-Eocene boundary, Which were discovered by Deep Sea Drilling Project and which have been attracting geologists’ s attention, include: a change in lithology from glauconitic quartz sand to clay; a change in clay mineral suites from illite/smectite-dominated to kaolinite-dominated; the extinction and migration in the terrestrial flora; an increased species turnover rate in marine calcareous nanofossils; the extinction and lower diversity in the benthic foraminiferal assemblages; a considerable excursion in δ18O and δ13C values; a change in the evolution of land mammals; a significant reduction of the intensity of atmospheric circulation; a change in the style of abyssal circulation; an increase in water depth; and one to two order of magnitude increase in hydrothermal activity at the Paleocene-Eocene boundary. The Paleocene-Eocene boundary was the result of global tectonic events by researching lithology, palaeobiology, palaeoclimatology, palaeoceanography of the Paleocene-Eocene stratigraphic sections. The events include that global plate boundary rearrangement, changes in patterns of spreading centers and transform faults, and increase in hydrothermal activity.