-
Content of organic and inorganic carbon, nitrogen and opal for IODP Hole 344-...
The total weight percent of sedimentary carbon (% C) and nitrogen (% N), as well as inorganic carbon (% Cinorg) and organic carbon (% Corg) were measured using a macro elemental... -
Reconstructed biogenic opal percentage and accumulation for site J1007, Chile...
Sediment cores at sites J1007 were collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) in 2019. Sedimentary Green/Blue (G/B) ratio data were... -
Opal mass accumulation rates from IODP Site 361-U1475
Biogenic silica accumulation was obtained by analyzing approximately 200 mg of homogenized and freeze dried sediment for each sample. Cleaning, chemical treatment, and... -
Abundance of Neogloboquadrina pachyderma sinistral from IODP Site 361-U1475
Neogloboquadrina pachyderma abundance was obtained by washing ~ 10 cm³ of sediment through a 150µm sieve and drying at ~ 50 ºC for 24 h. This dried fraction was split until a... -
δ¹⁵N in planktonic foraminifera species Globigerina bulloides and Globorotali...
Individual species were identified and ~550 individuals per species were picked from the >250 µm fraction under dissecting microscope for each sample. Approximately 7 mg of... -
Planktonic and benthic foraminifera, benthic foraminiferal stable isotopes, s...
This bundle publication contains six individual datasets of micropaleontological data (planktonic and benthic foraminiferal assemblages), geochemical data (sedimentary organic... -
Stable oxygen isotope ratios in opal and seawater from various locations
This dataset has no description
-
Concentrations of export production indicators and corrected and non-correcte...
Studying oceanic particle fluxes from sediment records is an important component of paleoceanography. Traditionally, we calculate these fluxes using a combination of linear... -
(Table 5) Mass accumulation rates for sediment components at DSDP Hole 75-532
Sediment depth is given in mbsf. Wet-bulk density, porosity, and water content are from Site 532 chapter, this volume. Bulk-sediment MAR = [(1 - poros./100) x 2.7] x 100 x (sed.... -
(Table 2) Temporal variations of chemical element- and sediment component acc...
This dataset has no description
-
(Table 2) Temporal variations of chemical element- and sediment component acc...
This dataset has no description
-
(Table 2) Geochemistry and acculumation rates of sediment core GPC-3
Dated by Prince et al. (1980) using paleomagnetics and by Doyle et al. (1979, doi:10.2973/dsdp.proc.26.135.1974) using fish teeth -
(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) -
(Table 2) Geochemistry and acculumation rates of DSDP Hole 85-572
Age based on nannofossil biostratigraphy by Worsley for this study, documented in Chaboudy (1984) -
Radiolarian relative abundance and opal and radiolarian accumulation rate fro...
A high-resolution record of radiolarian assemblages from Site U1314 was studied to reconstruct hydrographic and climatic changes in the North Atlantic Ocean during the... -
(Table S1) N15 isotope ratios, age determination and accumulation rates of se...
In a piston core from the central Bering Sea, diatom microfossil-bound N isotopes and the concentrations of opal, biogenic barium, calcium carbonate, and organic N are measured... -
Atlantic 231Pa/230Th and biogenic opal compilation of the Holocene and the LGM
The strength and geometry of the Atlantic meridional overturning circulation is tightly coupled to climate on glacial-interglacial and millennial timescales, but has proved... -
Tab.A.3.5. Sediment composition and accumulation rates of ODP Hole 105-646A
This dataset has no description
-
Tab.A.3.4. Sediment composition and accumulation rates of ODP Hole 104-644A
This dataset has no description
-
Tab.A.3.3. Sediment composition and accumulation rates of ODP Hole 104-643A
This dataset has no description
