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Global shallow sediment diagenesis survey results based on all available IODP...
Global shallow sediment diagenesis survey results based on all available IODP sediment core images. -
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... -
Geochemistry and geological ages for organic-rich black shales of the Quatern...
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Sediment silt size fractions of site 79-544B, tab A-V,X,XV,XXI
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Age Model of Site 79-544B
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Sand and carbonate content from Hole 79-544B
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Clay mineralogy of Hole 79-544B
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Sedimentological, organic petrographic and organic chemical characteristics o...
Large parts of the Cretaceous Atlantic Ocean are characterized by the wide-spread deposition of organic-carbon-rich sediments ("black shales“), with a maximum occurrence during... -
Stable isotope ratios of benthic foraminifera from DSDP Hole 79-544B (Table 1)
At DSDP Hole 544B, oxygen-isotope stratigraphy, carbonate proportion, clay mineralogy, and (terrigenous) grain sizes show short-term (Milankovitch-type) sediment cycles from 5.1... -
Sedimentology of sites 14-141, 41-366, 47-397 and 79-544B
Along the N-S-transect of DSDP-Sites 5446, 397, 141, and 366, oxygen and carbon isotopes, flux rates of calcium carbonate, terrigenous matter, and biogenic opal, clay minerals... -
(Table 2) Distribution and relative abundance of mid-Cretaceous planktonic fo...
Abundances: Based on 300-specimen counts. A = abundant (25%), C = common (5-25%), R = rare (1-5%), V = very rare (1%), - = absent, ? = questionable occurrence, cf. = confer,... -
(Table 1) Distribution and relative abundance of mid-Cretaceous planktonic fo...
Abundances: Based on 300-specimen counts. A = abundant (25%), C = common (5-25%), R = rare (1-5%), V = very rare (1%), - = absent, ? = questionable occurrence, cf. = confer,... -
(Figure 4) Distribution and relative abundances of the benthic foraminifers r...
Species abundance: F = few (1-3 specimens), C = common (4-9 specimens), A = abundant (>10 specimens), - = absent. -
(Table 1) Stable isotope record of Middle Cretaceous benthic foraminifera
Preservation of planktic foraminiferal calcite has received widespread attention in recent years, but the taphonomy of benthic foraminiferal calcite and its influence on the... -
(Table 1) Distribution of ostracods in Jurassic sediments of DSDP Hole 79-547
Eighteen samples from the Early Jurassic (Hettangian to Pliensbachian) and nine from the Bajocian to Berriasian interval have been examined. The ostracode fauna has been left... -
(Table 2) Potassium, argon and K-Ar dates of the Mazagan granodiorite at V30-...
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Stable carbon isotope ratios and accumulation rates of organic carbon and nut...
Future warming is predicted to shift the Earth system into a mode with progressive increase and vigour of extreme climate events possibly stimulating other mechanisms that... -
(Table 1) Mineralogy at DSDP Leg 79 Holes
Four sites in the region of the Mazagan Plateau off northwest Africa were drilled during Leg 79 of the Deep Sea Drilling Project. Bulk mineralogy and clay mineralogy were... -
(Table 1) Organic petrography and Rock-Eval pyrolysis at DSDP Hole 79-547B
A lenticle of organic matter in a piece of dolomite rock embedded in Triassic sandy mudstone of Core 547B-35 (DSDP Leg 79) was identified as inertinite-rich coal by organic... -
(Figure 1) Stratigraphic distribution of taxa at DSDP Hole 79-547B
Twenty-five samples from selected cored intervals of problematic Triassic-Jurassic age from Sites 545, 546, and Hole 547B have been analyzed palynologically to aid age...
