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(Table 1) Age model of ODP Hole 120-747A
This dataset has no description
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(Table 2) Age model of DSDP Hole 30-289
This dataset has no description
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(Table 1) Depth-age points used for initial chronology and adjusted ages of O...
Ocean Drilling Program (ODP) Site 982 in the North Atlantic contains a complete latest Miocene to early Pliocene section that was tuned to the astronomical timescale by... -
(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) Subsidence and calcite accumulation for South Pacific DSDP drill sites
Patterns of crustal subsidence in the southeast Pacific Ocean reflect the complex tectonic history of that region. A plot of the depth-time history of calcite accumulation... -
(Table 1) Ages of planktonic foraminiferal datums at Leg 94 Sites
The six Leg 94 sites have produced a unique data set from a north-south transect of sites, all with good paleomagnetic records, and all but one with above-average accumulation... -
(Table T1) Depths and ages of datum levels at ODP Leg 182 sites
The first and last appearances of Quaternary planktonic foraminifers in the Great Australian Bight were evaluated using datum levels from magnetostatigraphy, oxygen isotope... -
(Table 1) Biostratigraphic datums of ODP Leg 133 sites
We use benthic foraminifers to reconstruct the Neogene paleobathymetric history of the Marion Plateau, Queensland Plateau, Townsville Trough, and Queensland Trough on the... -
(Table 1) Ages and depths of magnetostratigraphic boundaries in ODP Hole 132-...
A magnetic stratigraphy study was undertaken on Hole 810C cores to provide age constraints and to characterize sedimentation on the summit of Shatsky Rise. Sediments from this... -
(Table 1) Age control for magnetic reversals in ODP Hole 138-853B
The Messinian salinity crisis is widely regarded as one of the most dramatic episodes of oceanic change of the past 20 or so million years (Hsü et al., 1973,... -
Revised age calibrations for the Eocene/Oligocene boundary of ODP Site 199-1218
The ocean depth at which the rate of calcium carbonate input from surface waters equals the rate of dissolution is termed the calcite compensation depth. At present, this depth... -
Calcareous nannofossil biomagneochronology of ODP Hole 122-762B (Tables 1, 2)
Drilling on the Exmouth Plateau during Ocean Drilling Program Leg 122 recovered an almost complete Cenozoic sequence at Site 762. Sediments at this site contain abundant,... -
(Table 1) Age determination of ODP Hole 119-744A
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Age estimates of ODP Hole 175-1085A bio-and paleomagnetic events (Table 1)
High-resolution benthic oxygen isotope and XRF (Fe and Ca) records from Site 1085 drilled in the Mid-Cape basin (ODP Leg 175) are used to investigate global climate changes... -
Age models, stable isotope record, and physical properties of ODP Hole 154-926B
We extend existing high-resolution Oligocene–Miocene proxy records from Ocean Drilling Program (ODP) Leg 154. The extended record spans the time interval from ~17.86 to 26.5... -
(Table 2) Correlation of Mi zones with hiatuses in ODP Site 181-1124
Results from Ocean Drilling Program sites 1121-1124 show the Eastern New Zealand Oceanic Sedimentary System (ENZOSS) evolved in response to: (1) the inception of the... -
Trace element abundance, and Sr and Nd isotope ratios of dust samples in the ...
Eolian dust preserved in deep-sea sediment cores provides a valuable indicator of past atmospheric circulation and continental paleoclimate. In order to identify the provenance... -
Strontium isotope ratios of planktonic foraminifera from ODP Site 119-744 on ...
87Sr/86Sr ratios of well-preserved early Miocene-Oligocene planktonic foraminifers from Site 744 in the southern Indian Ocean provide the highest southern latitude Sr isotope... -
Age estimations of calcareous nannofossil biohorizons of the middle Paleocene...
Over the last several decades debates on the 'tempo and mode' of evolution have centered on the question whether morphological evolution preferentially occurs gradually or...
