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(Table 3) Age model of the Paleocen section of ODP Hole 122-761B in the easte...
Event Chron C24r/C25r depth bottom unknown -
(Table 1) Age comparison between the GPTS and ODP Site 181-1123 age model for...
Today the deep western boundary current (DWBC) east of New Zealand is the most important route for deep water entering the Pacific Ocean. Large-scale changes in deep water... -
(Table 12) Planktonic foraminifera stratigraphy and ages of ODP Hole 162-981A
DEPTH, sediment is given in mbsf. -
(Table 1) Planktonic foraminiferal datum events of ODP Leg 166 sites
Planktonic foraminifers recovered from Leg 166 drilling showed a progression from well-preserved to poorly preserved specimens with increasing depth. The high carbonate... -
(Table 2) Age interval and accumulation rates of organic and inorganic carbon...
The Ocean Drilling Program Leg 175 recovered a unique series of stratigraphically continuous sedimentary sections along the SW African margin, an area which is presently... -
Late Eocene to Early Oligocene magnetostratigraphic chron boundaries of ODP H...
The earliest Oligocene (~33.5 Ma) is marked by a major step in the long-term transition from an ice-free to glaciated world. The transition, characterized by both cooling and... -
Stable isotope from Miocene exceptionally preserved foraminifera from Tanzania
The dataset presents oxygen and carbon stable isotopes measured on multispecies planktonic foraminiferal shells and on Cibicidoides spp. and Uvigerina spp. (benthic...
