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Nannofossil abundance of Hole 71-512
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 71-511
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 71-513A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 71-512A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Paleomagnetic of Hole 71-513A
This dataset has no description
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Paleomagnetic of Hole 71-512
This dataset has no description
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Paleomagnetic of Hole 71-511
This dataset has no description
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Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks...
This dataset has no description
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Paleomagnetic measurements with a long-core spinner magnetometer of Hole 71-512
This dataset has no description
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(Figure 3) Distribution of planktonic foraminifers in the Cenozoic sediments ...
Species abundaces: C = common, F = few, R = rare, VR = very rare, - = absent. Samples 71-511-1-3,120-123 to 71-511-2-4,25-27 and 71-511-21-1,34-36 to 71-511-23-1,3-4 (Paleogene... -
(Figure 4) Distribution of planktonic foraminifers in the Cenozoic sediments ...
Species abundaces: C = common, F = few, R = rare, VR = very rare, - = absent. -
Upper Cretaceous planktic foraminiferal biozonation for the Austral Realm
A new planktic foraminiferal zonal scheme is presented for subdivision of Upper Cretaceous pelagic carbonate sequences in the circum-Antarctic region. Definition of the zones... -
Paleotemperature reconstructions from high Late Jurassic paleolatitudes
Oxygen and carbon isotopes have been determined from Late Jurassic (Oxfordian-Tithonian) belemnites and inoceramid bivalves from two Deep Sea Drilling Project (DSDP) sites... -
Strontium-isotope stratigraphy and oxygen- and carbon-isotope record of Middl...
87Sr/86Sr data of belemnites are presented from a Middle Jurassic-Early Cretaceous succession from the Falkland Plateau (Deep Sea Drilling Project Sites 511 and 330) that was... -
Chemical composition of sediments from DSDP Legs 45 and 71
Results of mineralogical and geochemical investigations of post-Middle Jurassic deposits of the Atlantic Ocean are based on materials of the Deep Sea Drilling Project.... -
Cretaceous planktonic foraminifera of DSDP Hole 71-511
Lower and Upper Cretaceous sediments of the Maurice Ewing Bank, Site 511 (black shales, mudstones, zeolitic clays, and nannofossil chalk and ooze, 361 m thick) are characterized... -
Cenozoic planktonic foraminifera of the Falkland Plateau and Argentine Basin
Sites 511 and 512 (Falkland Plateau) and 513 (Argentine Basin) penetrated calcareous-siliceous oozes of the middle and upper Eocene and lower Oligocene with rather numerous... -
Oligocene strontium isotope stratigraphy of Indian Ocean sediments
Strontium isotope (87Sr/86Sr) ages have been established for Oligocene samples of Leg 119 Site 744, Leg 120 Sites 747 and 748, and Leg 121 Sites 756 and 757. Ages were... -
Porphyrin geochemistry of DSDP Hole 71-511
Late Jurassic-early Cretaceous black shales and an overlying sequence of Albian-Campanian zeolitic claystones from the Falkland Plateau (DSDP/IPOD Leg 71, Site 511) were... -
Geochemistry at DSDP Legs 36 and 71 Holes
For Middle Jurassic to Pleistocene times, clay mineralogical and geochemical data provide information on the evolution of continental and marine paleoenvironments. They are a...
