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Synthesis of early Pliocene and mid-Pliocene carbon anomaly
This dataset has no description
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(Table 1) 3He/4He and 4He/20Ne ratios in pore water and gas in deep-sea sedim...
This dataset has no description
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(Table 1) Estimated age for the last occurrence of Globoquadrina dehiscens
Ages were transfered to the timscale of Berggren et al. (1995) -
(Appendix III) Neogene radiolarian events of DSDP Site 89-586 in the western ...
Raw data this publication and Caulet (1986) doi:10.2973/dsdp.proc.90.114.1986 -
(Appendix II-C) Occurrence of radiolarians in Neogene sediments of DSDP Site ...
species abundance: P = present, + = very rare (1 specimen), - = absent -
(Table 5) Analyses of representative tholeiites and tholeiitic ferrobasalts o...
This dataset has no description
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(Table 2) Geochemistry and acculumation rates of DSDP Hole 89-586
Age based on nannofossil biostratigraphy by Worsley for this study, documented in Chaboudy (1984) -
Pacific Neogene carbonate accumulation rates
I have compiled CaCO3 mass accumulation rates (MARs) for the period 0–25 Ma for 144 Deep Sea Drilling Project and Ocean Drilling Program drill sites in the Pacific in order to... -
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... -
Pelagic phosphorus accumulation in the Pacific Ocean
As a limiting nutrient to marine life, phosphorus (P) is an effective tracer of today's marine productivity. The distribution of P in marine sediments likewise tracks the... -
3He/4He and 4He/20Ne ratios in pore water and gas in Pacific deep-sea sediments
We have measured the 3He/3He and 3He/20 Ne ratios of thirty-nine pore water and gas samples in deep-sea sediments collected at twelve sites on the Pacific Ocean bottom during... -
Late Miocene development of the western Pacific warm pool: Planktonic foramin...
The disappearance at ~10 Ma of the deep dwelling planktonic foraminifer Globoquadrina dehiscens from the western Pacific including the South China Sea was about 3 Myr earlier... -
Neogene radiolarian datum levels in the equatorial Indian and Pacific Oceans
Fifty radiolarian events of early Pleistocene and Neogene age were identified in an E-W transect of equatorial DSDP sites, extending from the Gulf of Panama to the western... -
(Table 3) Benthic foraminifera in early-middle Miocene sediments of DSDP Site...
Abundances: X = present, A = very abundant, - = absent. -
(Table 2) Benthic foraminifera in Pliocene sediments of DSDP Hole 89-586B
Abundances: X = present, A = very abundant, - = absent. -
(Table 1) Benthic foraminifera in late Miocene sediments of DSDP Hole 89-586B
Abundances: X = present, A = very abundant, - = absent. -
(Table 1) Distribution of Cretaceous redeposited benthic foraminifers at DSDP...
Abundances based on total fauna recovered from 20-cm**3 samples greater than 42 µm. -
(Appendix B) Benthic foraminifera in DSDP Site 89-586 sediments
This dataset has no description
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(Table 1) 40Ar/39Ar geochronology at DSDP Hole 89-462A
40Ar/39Ar geochronological studies were performed on basalts taken from the bottom of Hole 462A. An age of 129.7 ± 4.6 Ma was obtained for two temperature fractions (800 and... -
(Table 1) Oxides and carbonates at DSDP Sample 89-585A-18-6,84-88
DSDP Site 585 was selected for drilling the Central Old Pacific as a relic of the Mesozoic superocean Panthalassa. The basal lithologic unit recovered from Holes 585 and 585A is...
