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Stable isotopes on benthic foraminifera from Hole 47-397
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Stable isotope ratio of benthic foraminifera from Hole 47-397
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Calcium carbonate content from Hole 47-397
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Sediment silt size fractions of site 47-397, tab A-V,X,XV,XXI
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Age Model of Site 47-397
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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 3) Survey of Atlantic Ocean DSDP sites for hiatuses PH and NH 1 throug...
This dataset has no description
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(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. -
(Table 5) Quaternary paleoproductivity of organic carbon in oceans based on D...
By analogy with the present-day ocean, primary productivity of paleoceans can be reconstructed using calculations based on content of organic carbon in sediments and their... -
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... -
Occurrence of hiatuses PH and NH 1 through NH 7 in DSDP holes
Miocene paleoceanographic evolution exhibits major changes resulting from the opening and closing of passages, the subsequent changes in oceanic circulation, and development of... -
(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... -
Planktic foraminifera abundance of Hole 47-397
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Benthic foraminifera abundance of Hole 47-397
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 47-398D
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(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 3) Results of apatite fission track dating, DSDP Site 47-397
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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... -
Maximum and mean diameter record of Orbulina universa from DSDP Hole 47-397 o...
Measurements of the diameter of O. universa carried out on 30 specimens from 39 samples covering a sediment thickness of 78 m and going back in time to approximately 750 000 y... -
Isotope ratios of sediments from DSDP Hole 47-397 (Table 1)
We report the Sr, Nd and Pb isotopic compositions (1) of 66 lava flows and dikes spanning the circa 15 Myr subaerial volcanic history of Gran Canaria and (2) of five Miocene...
