Glacial-to-Holocene sedimentation on the western slope of Great Bahama Bank by Slowey, N, Wilber, R, Haddad, G, Henderson, G

“…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. …”

U-Th dating and diagenesis of Pleistocene highstand sediments from the Bahamas slope by Henderson, G, Rendle, R, Slowey, N, Reijmer, J

U-Th dating of marine isotope stage 7 in Bahamas slope sediments by Robinson, L, Henderson, G, Slowey, N

Variation in bioturbation with water depth on marine slopes: a study on the Little Bahamas Bank by Henderson, G, Lindsay, F, Slowey, N

“…These were compared with data from the Bahamas bank tops and from elsewhere to assess the rate and depth of mixing in the slope environment. …”

Radiocarbon Ages Constraints on the Origin and Shedding of Bank-Top Sediment in the Bahamas during the Holocene by Slowey, N, Henderson, G

“…Great quantities of fine-sized aragonite needles are produced in the shallow waters that cover the tops of the Bahama Banks and then exported to the bank margins where they accumulate with shells of pelagic organisms. …”

Radiocarbon Ages Constraints on the Origin and Shedding of Bank-Top Sediment in the Bahamas during the Holocene by Slowey, N, Henderson, G

Fluid flow through carbonate platforms: constraints from U-234/U-238 and Cl- in Bahamas pore-waters by Henderson, G, Slowey, N, Haddad, G

“…In this study, we use U concentrations and isotope ratios measured on small volumes of pore-water from Bahamas slope sediment, coupled with existing chlorinity data, to place constraints on the fluid-flow in this region and, by implication, other carbonate platforms. …”

Early diagenesis of shallow-water periplatform carbonate sediments, leeward margin, Great Bahama Bank (Ocean Drilling Program Leg 166) by Malone, M, Slowey, N, Henderson, G

Evidence from U-Th dating against Northern Hemisphere forcing of the penultimate deglaciation by Henderson, G, Slowey, N

“…Here we date the penultimate deglaciation in a record from the Bahamas using a new U-Th isochron technique. After the necessary corrections for alpha-recoil mobility of 234U and 230Th and a small age correction for sediment mixing, the midpoint age for the penultimate deglaciation is determined to be 135 +/- 2.5 kyr ago. …”

Direct U-Th dating of marine sediments from the two most recent interglacial periods by Slowey, N, Henderson, G, Curry, W

“…Here we report the direct U-Th dating of aragonite-rich marine sediments from the Bahamas, and present an accurately dated marine oxygen-isotope record for the last two interglacials. …”

U-Th dating of carbonate platform and slope sediments by Henderson, G, Slowey, N, Fleisher, M

“…Using heavy liquids to separate the various carbonate minerals found in Bahamas sediment enables an isochron approach to correct for initial Th, but the presence of initial Th from two sources requires correction or removal of one source of initial Th before the other is deconvolved by the isochron. …”