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(Appendix) Stable carbon and oxygen isotope ratios of fine-fraction sediments...
Ages were obtained using the magnetostratigraphy data reported by Chave (1984) and age interpretation made by Shackleton and Hall (1984). The K/T boundary is assumed to have an... -
(Appendix) Stable carbon and oxygen isotope ratios of fine-fraction sediments...
Ages were obtained using the magnetostratigraphy data reported by Chave (1984) and age interpretation made by Shackleton and Hall (1984). The K/T boundary is assumed to have an... -
(Table 4) Maastrichtian planktic foraminiferal datum events of DSDP Hole 74-5...
This dataset has no description
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(Table 3) Stable carbon and oxygen isotope ratios of foraminifera in Maastric...
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(Appendix C) Stable isotope ratios and paleotemperature calculation of select...
Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron. Paleotemperature estimates were... -
(Appendix B) Relative abundances of larger size planktonic foraminifera in la...
Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron -
(Appendix A) Relative abundances of smaller size planktonic foraminifera in l...
Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron -
Stable isotope ratios measured on foraminifera of DSDP Hole 74-525B
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Stable isotope ratios measured on foraminifera of DSDP Hole 74-525A
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Age model of DSDP Hole 74-525A
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Age model of DSDP Hole74-525
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(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 1) Pore water isotopes from DSDP Hole 74-525B, with respect to the Vie...
During the coring of Hole 525B with the hydraulic piston corer, a number of sediment samples were squeezed and the pore waters retained for stable isotope study. Both 18O/16O... -
(Table 1) Magnetostratigraphy and sedimentation rates of the K/T boundary int...
The results of two separate magnetic investigations are discussed in this paper. The first study produced a magnetostratigraphy from the K/T boundary interval of Hole 1001A from... -
(Table 1) Sea-surface temperatures, intermediate-water temperatures, and lati...
Climatic and oceanographic variations during the last 2 m.y. of the Maastrichtian inferred from high-resolution (10 k.y.) stable isotope analysis of the mid-latitude South... -
Nannofossil events of Maastrichtian sediments from DSDP Hole 74-525A in the S...
The phytoplankton response (calcareous nannofossils) to the Late Maastrichtian climate evolution is investigated in the South Atlantic DSDP Hole 525A and compared to published... -
Abundance of benthic foraminifera in late Paleocene to eraly Pliocene sedimen...
Benthic forammifers in the size-fraction greater than 0.073 mm were studied in 88 Paleocene to Pleistocene samples from Deep Sea Drilling Project Site 525 (Hole 525A, Walvis... -
(Appendix 1) Fluorescence of dissolved organic matter in marine sediments of ...
This dataset has no description
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(Appendix 1) 87Sr/86Sr ratios of planktonic foraminifera from DSDP Hole 74-528
87Sr/86Sr values for standards equal 0.710265 for NBS 987, and 0.709175 for seawater samples from the North Atlantic and Central Pacific. Ratios are fractionation corrected to...
