-
δ13C data from the DSDP Leg 47B, Hole 398D, cores 56 to 58 (offshore NW Iberi...
A palynological and carbon-isotope analysis was carried out from the mid-Cretaceous of the DSDP Hole 398D located in the southern flank of the Vigo Seamount (NW Iberian... -
Complementary palynological data from the DSDP Leg 47B, Hole 398D, cores 56 t...
A palynological and carbon-isotope analysis was carried out from the mid-Cretaceous of the DSDP Hole 398D located in the southern flank of the Vigo Seamount (NW Iberian... -
(Table 2) U, Th, and Sm of apatite from rapidly cooled samples
Sediment depth is given in mbsf. AGE [ka BP] gives the deposition age. -
(Table 1) U, Th, and Sm of rapidly cooled samples
Sediment depth is given in mbsf. AGE [ka BP] gives the deposition age. -
Sediment silt size fractions of site 47-397, tab A-V,X,XV,XXI
This dataset has no description
-
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 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... -
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...
This dataset has no description
-
(Table S2) Characteristics of analysed apatite grains from rapidly cooled sam...
Sediment depth is given in mbsf. AGE [ka] gives the deposition age. -
(Table AT2) Petrology in point counts of ODP Hole 210-1276A, two ODP Leg 173 ...
This dataset has no description
-
(Table T1) Petrology of ODP Hole 210-1276A, two ODP Leg 173 sites and DSDP Ho...
This dataset has no description
-
(Table 1) Description of CTBE samples from ODP Hole 103-641A and DSDP Hole 43...
Clay minerals are numbered according to their relative abundance in the clay fraction; higher numbers indicate decreasing amounts; smectite, the dominant clay mineral in all... -
(Data Set S1) Compiled benthic foraminiferal stable isotopic values
d13C_adj: carbon isotopic value adjusted to Cibicidoides equivalent.d18O_adj: oxygen isotopic value adjusted to Cibicidoides equivalent. -
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... -
Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites
Sand detrital modes of Albian-Eocene clastic gravity-flow deposits cored and recovered at Ocean Drilling Program Site 1276 reflect the postrift geologic evolution of the... -
The Cenomanian/Turronian Boundary Event at ODP Hole 103-641A
Drilling at ODP Site 641 (on the western margin of Galicia Bank, off northwestern Spain) revealed a thin, but pronounced, interval of black shale and gray-green claystone. Our... -
Cretaceous radiolarians of the North Atlantic Ocean
Radiolarians form a remarkable part of the fossil plankton for Cretaceous sediments of the North Atlantic. Selected sites with long-term sedimentary successions of deep facies... -
Age and chemical composition of apatites from five DSDP and ODP Sites in the ...
Since studies on deep-sea cores were carried out in the early 1990s it has been known that ambient temperature may have a marked affect on apatite fission track annealing. Due... -
Diversity of abyssal agglutinated foraminifera from Cenomanian to Santonian s...
Benthic foraminiferal assemblages of distinctive taxonomic composition occur at the top of benthic fossil-free black shales which correspond to the anoxic event at the...