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(Table 3) Uranium and thorium concentrations, ratios and ages of sediments fr...
Sediment depth is given in mcd. Raw age is calculated directly from the data in the previous two columns. Scavenging corrected age = the age corrected for initial 230Th by... -
(Table 2) Aragonite and magnesium calcite content of sediments from ODP Leg 1...
Sediment depth is given in mcd. Percentages were calculated using peak areas and standards of known composition. -
(Table DR2) Parameters of pore-waters from ODP Hole 166-1009
This dataset has no description
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(Table DR2) Parameters of pore-waters from ODP Hole 166-1008
This dataset has no description
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(Table 1) Composition of hardgrounds from ODP Hole 166-1009
This dataset has no description
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(Table 1) Composition of hardgrounds from ODP Hole 166-1008
This dataset has no description
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(Table 1) Uranium concentrations and isotope ratios from pore-water of ODP Ho...
This dataset has no description
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(Table 1) Uranium concentrations and isotope ratios from pore-water of ODP Ho...
This dataset has no description
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(Table 1) Th and U isotope ratios of sediments from ODP Site 166-1009
U and Th blanks are <1‰ of the measured sample and are corrected for. Raw ages and delta234U values are adjusted to account for initial 230Th to give the corrected numbers in... -
(Table 1) Th and U isotope ratios of sediments from ODP Site 166-1008
U and Th blanks are <1‰ of the measured sample and are corrected for. Raw ages and delta234U values are adjusted to account for initial 230Th to give the corrected numbers in... -
(Table 1) Age determination of ODP Leg 166 holes
Thick, late Quaternary sediment sections were recovered at several sites on the leeward slope of Great Bahama Bank during Leg 166 of the Ocean Drilling Program. These sections... -
Composition of hardgrounds and of pore-water parameters in ODP Holes 166-1008...
Mineralogic, petrographic, and geochemical analyses of sediments recovered from two Leg 166 Ocean Drilling Program cores on the western slope of Great Bahama Bank (308 m and 437... -
Uranium concentrations and isotope ratios Bahamas seawater and ODP holes pore...
The geometry, timing, and rate of fluid-flow through carbonate margins and platforms is not well constrained. In this study, we use U concentrations and isotope ratios measured... -
U-Th dating of marine sediments from the Bahamas slope
In order to understand the driving forces for Pleistocene climate change more fully we need to compare the timing of climate events with their possible forcing. In contrast to... -
Faunal assemblage of ODP Hole 166-1006A
This dataset has no description
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Census counts of the fraction 250-500 µm of ODP Hole 166-1006A
This dataset has no description
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Carbonate preservation of sediment cores from the Great Bahama Bank
The oceanic carbon cycle mainly comprises the production and dissolution/ preservation of carbonate particles in the water column or within the sediment. Carbon dioxide is one... -
(Table 3a) Strontium isotopic results for ODP Site 166-1006A
(a) age model Kroon D, Williams T, Pirmez C, Spezzaferri S, Sato T, Wright JD. Coupled Early Pliocene-Middle Miocene bio-cyclostratigrahy of Site 1006 reveals orbitally induced... -
(Table 2a) Neodymium isotopic results for ODP Site 166-1006A
(a) age model Kroon D, Williams T, Pirmez C, Spezzaferri S, Sato T, Wright JD. Coupled Early Pliocene-Middle Miocene bio-cyclostratigrahy of Site 1006 reveals orbitally induced... -
Morphometric study of porosity and morphology of fossil Globigerinoides, Chp5...
Nomenclature of each specimen follows the rule described in Annex 1.1. Images are grouped following the initial files names used during this work, meaning that the number of...