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(Table 1) Organic carbon, hydrogen and oxygen index and hydrocarbons at DSDP ...
C2-C8 hydrocarbon concentrations (about 35 compounds identified, including saturated, aromatic, and olefinic compounds) from 27 shipboard-sealed, deep-frozen core samples of... -
(Table 1) Sample descriptions, carbon contents, and lipid yields across the K...
This reconnaissance study was undertaken to determine whether the mass extinctions and faunal successions that mark the Cretaceous/Tertiary (K/T) boundary left a discernible... -
(Table 1) Proportions of clay minerals and mud, as well as description of sed...
The clay mineralogy of Lower Cretaceous deep-sea fan sediment in the western North Atlantic is dominated by smectite in most intervals, and by illite in samples from intervals... -
(Table 1) Elements at DSDP Section 93-605-66-1
The oldest sediments cored at Site 605 are upper Maestrichtian argillaceous limestone (Hole 605, Subunit VB). The terrigeneous silt content of the uppermost Maestrichtian is... -
(Table 1) Carbon and oxygen isotope composition of carbonate sediments at DSD...
Compositional, textural, and oxygen and carbon stable isotopic analysis of Lower Cretaceous pelagic cyclic sediment is necessary in order to understand the mechanisms causing... -
(Table 1) Clay minerals at DSDP Hole 93-603B
Cretaceous sediments encountered in Hole 603B contain a 17 Å smectite as the principal clay mineral, with lesser amounts of illite, kaolinite, and randomly interstratified... -
(Table 1) Calcite, siderite, and stable isotopes δ¹³C and δ¹⁸O at DSDP Hole 9...
Diagenesis of the fine-grained, feldspathic sandstones in the Lower Cretaceous submarine fan complex cored in DSDP Hole 603B can be considered to have occurred in three stages:... -
(Table 1) Magnetozone boundaries, age and sedimentation rate at DSDP Hole 93-605
Natural Remanent Magnetization (NRM) was measured for regularly spaced samples from the 620-m-thick, lower middle Eocene to upper Maestrichtian section of DSDP Site 605. The... -
(Table 1) Pollen assemblage at DSDP Holes 96-603B and 93-605
The analysis of 104 core-catcher samples from Site 603 resulted in a continuous palynological record from the middle Miocene to early Pleistocene. Two palynological zones could... -
(Appendix A) Organic facies at DSDP Hole 93-603B
The Palynology of two sections recovered during Leg 93 drilling by the Deep Sea Drilling Project in the continental rise along the western margin of the North Atlantic is... -
Geochemistry and P and Fe fractionation in anoxic sediments
We investigated the phosphorus (P) and iron (Fe) fractionation in four cores with anoxic sediments, deposited during the mid-Cretaceous oceanic anoxic event 2 (~94 Ma) and the... -
Correlation of Late Jurassic and Early Cretaceous zonation events in ODP and ...
A database was built of 378 stratigraphic events, including first and last stratigraphic occurrences (FO/LO) of calcareous nannofossils, foraminifers, and dinocysts, and... -
Organic carbon and total sulfur content and concentrations of selected molecu...
During mid-Cretaceous times large amounts of organic carbon (Corg) became sequestered in 'black shales', possibly due to 'oceanic anoxic events' characterized by the development... -
Total organic carbon content and redox-sensitiv trace metal concentrations of...
The Cenomanian/Turonian (C/T) intervals at DSDP Sites 105 and 603B from the northern part of the proto-North Atlantic show high amplitude, short-term cyclic variations in total... -
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.
