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Carbonates and bulk sediment geochemistry of ODP Hole 166-1003A
Data derive from coulometer, CHNS analyzer, and pyrolysis oven (rock eval) -
Paleomagnetic properties of ODP Hole 166-1006A carbonate sediments
Paleomagnetic analyses from discrete samples of carbonate sediment from Hole 1006A were completed to assess the nature of magnetic remanence and to evaluate the use of... -
Planktonic foraminifera distribution during the mid-Piacenzian warm period in...
The mid-Piacenzian (MP) warm period (3.264-3.025 Ma) has been identified as the most recent time in geologic history during which mean global surface temperatures were... -
Stable carbon isotope record of Bahama Bank sediments
The carbon-isotopic composition (d13C) of bulk carbonates, obtained from a transect of sites drilled through platform and periplatform sediments of Holocene to Early Miocene... -
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... -
Chronostratigraphy of sediments from the Bahamas
Continuous cores drilled during the Bahamas Drilling Project (BDP) and the Ocean Drilling Program (ODP) Leg 166 along a transect from the top of Great Bahama Bank to the basin... -
Geochemical and mineralogical analyses of clay-rich intervals in ODP Sites 16...
The western flank of the Great Bahama Bank, drilled during ODP Leg 166 at seven sites, represents a prograding carbonate sequence from late Oligocene to Holocene [Eberli et al.,... -
Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A
During ODP Leg 166, the recovery of cores from a transect of drill sites across the Bahamas margin from marginal to deep basin environments was an essential requirement for the... -
Sediment composition and sedimentation rates of four Holes in ODP Leg 166
To date, work on the Great Bahama Bank's western, leeward margin has centred chiefly on seismic-scale expressions of carbonate sequences and systems tracts. However,... -
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... -
Depths and ages of seismic sequence boundaries in ODP Leg 166 holes
High-resolution, multichannel seismic data collected across the Great Bahama Bank margin and the adjacent Straits of Florida indicate that the deposition of Neogene-Quaternary... -
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... -
U and Th concentrations and isotope ratios of samples from ODP Leg 166
Constraining the history of seawater (234U/238U) is important because this ratio is used to assess the validity of U/Th ages, and because it provides information about the past... -
Chemical and Sr isotopic compositions of 3 step leachates and residues of bul...
Massive clinoptilolite authigenesis was observed at about 1105 meters below sea floor (mbsf) in lower Miocene wellcompacted carbonate periplatform sediments from the Great...
