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(Appendix 1) Biostratigraphy and Sr isotopic composition of sediments from DS...
This dataset has no description
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(Appendix 1) Biostratigraphy and Sr isotopic composition of sediments from DS...
This dataset has no description
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(Table 7) Magnetostratigraphy and calcareous plankton stratigraphy and zonal ...
In this study, core catchers are located in continuity with the lowest recovered section in a core, in agreement with the current ODP policy. Also several samples analyzed for... -
(Table 1) Paleocene planktonic foraminiferal datum levels of ODP Hole 122-761...
This dataset has no description
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(Table 1) Oligocene sediment packages, unconformities and sedimentation rates...
Depth is composite depth (mcd) -
(Table 1) Borings chips and/or borings of the ichnogenus Entobia at DSDP Hole...
Pelagic carbonate oozes of DSDP Site 526 contain remnants of the activity of boring sponges of the family Clionidae: (1) the borings themselves = ichnogenus Entobia and (2) the... -
(Table 2) Sub-bottom depths, biostratigraphic zones, and ages for major refle...
The analysis of high-resolution watergun seismic profiles collected in support of DSDP Leg 85 drilling reveals several major, regionally traceable reflectors that can be... -
(Table 1) Biostratigraphic zonation and core depth of microtektite occurrence...
Microtektites have been recovered from three horizons in eight middle Eocene to middle Oligocene marine sediment sequences. Five of these occurrences are coeval and of latest... -
(Table 1) Oxygen and carbon isotope data of bulk carbonate and foraminiferal ...
In low and middle latitudes, the Cretaceous/Tertiary boundary is marked by a sudden and pronounced decrease in d13C values of near-surface-water carbonates and a reduction in... -
(Table 1a) Biostratigraphy of Umbria-Marche composite section
Stratigraphic information was obtained from Deino et al. (1997), Montanari et al. (1997a, 1997b), Mader et al. (2001), and Hilgen et al. (2005). -
(Table 1b) Biostratigraphy of western Monferrato area
Stratigraphic information was obtained from Mühlstrasser (2002).
