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(Table1) Abundance of planktonic foraminifera in DSDP Hole 75-532
This dataset has no description
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(Table 3) Stable oxygen isotope ratios of Uvigerina spp. from DSDP Hole 75-532
isotopic measurements: N.J. Shackleton, Godwin Laboratory, Cambridge -
(Table 3) Stable oxygen isotope ratios of Globigerina bulloides from DSDP Hol...
isotopic measurements: Fachbereich Geowissenschaften, University of Bremen -
Pyrolysis data of South Atlantic source rocks from 20 DSDP-ODP sites: Insight...
This data set consists of analytical results from the HAWK Pyrolysis and TOC instrument for 161 bulk samples from Mesozoic to Cenozoic strata at 20 DSDP-ODP sites in the South... -
Annotated record of the detailed examination of Mn deposits from DSDP Leg 75 ...
Site 530 is located in the southeastern corner of the Angola Basin, about 20 km north of the Walvis Escarpment, near the eastern end of the easternmost (or Frio) segment of the... -
(Table 1) Sand, silt and clay at DSDP Leg 75 Holes
The distribution of sand, silt, and clay was determined on 10-cm**3 sediment samples collected at the time the cores were split and described. The sediment classification used... -
(Table 1) Sediment characteristics at DSDP Hole 75-532A
Orientation and geometry of pores as well as sediment compressibility can be approximated by determining the shrinkage behavior of standardized samples. The sections... -
(Table 1) Organic carbon isotopic composition in Cretaceous sediments at DSDP...
Cretaceous sediments from DSDP Site 530 have been analyzed for organic carbon isotopic composition. The d13C values in the sediments decrease from -22.7 per mil to -27.5 per mil... -
(Table 4) Mass accumulation rates of selected components in red, green, and b...
Deep-water sedimentary sequences of mid-Cretaceous age, rich in organic carbon, have been recovered at many DSDP sites in the Atlantic Ocean. Most of these sequences have a... -
(Table 1) Black shale characteristics at DSDP Hole 75-530A
The middle Cretaceous black shale interval at Site 530 is 170 m thick and late Albian to Coniacian in age. The organic-carbon-rich sediments occur as 260 separate beds (average... -
(Table 1) Non-arboreal and arboreal pollen spectra at DSDP Holes 75-532 and 7...
Some samples from DSDP Holes 530A and 532 were analyzed for their fossil pollen content. The sites are located in the southeastern corner of the Angola Basin, about 200 km west... -
(Table 1) Concentration of iridium at DSDP Hole 75-530A
The section recovered at Site 530 (Holes 530A and 530B) consists of eight sedimentary units and one basalt unit. The composition of the basalt recovered in Hole 530A is distinct... -
(Table 1) Comparison of adjacent Cenomanian black shales with green claystone...
Black shales possessing high concentrations of organic carbon (Foresman, 1978, doi:10.2973/dsdp.proc.40.111.1978) were deposited in many parts of the proto South Atlantic Ocean... -
Total organic carbon, lithology and alkylthiophenes in immature sediments (Ta...
A series of novel long-chain 3,4-dialkylthiophenes (C36–C54) was identified in a number of sediments ranging from Pleistocene to Cretaceous. The identifications were based on... -
(Table 1) CaCO3, terrigenous matter and Corg calculations from DSDP Hole 75-532B
Samples taken at 10 cm intervals from DSDP Core 532B-17 contain variations in carbonate, opal, organic carbon, and terrigenous components that correlate with light-dark cycles... -
(Table 1) Composition of clay minerals in DSDP Hole 75-532
An investigation of the quantitative composition of the coarse (> 40 µm) and clay (< 2 µm) fraction of HPC 532, DSDP Leg 75, in 1300 m water depth on the eastern Walvis... -
Organic chemical indicators of Hole 75-532B
This dataset has no description
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(Appendix 1) Element concentrations in sediment and basalt samples from DSDP ...
The geochemistry of the REE (rare earth elements) in oceanic sediments is discussed, based mainly on samples from DSDP Holes 530A and 530B, Leg 75, and Hole 525A, Leg 74. The... -
Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
Stable oxygen isotope ratios, calcium carbonate and opal content in late Plio...
Site 532 on the Walvis Ridge was sampled at 4000- to 800-year intervals from 2.24 to 2.60 Ma, spanning the three large glacial advances of the late Pliocene. An age model was...
