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ODP Site 1006

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Journal Article

ECOSTRATIGAPHIC REGIME SHIFT DURING LATE QUATERNARY MARINE ISOTOPE STAGES 8–9 IN SANTAREN CHANNEL, WESTERN TROPICAL ATLANTIC OCEAN: BENTHONIC FORAMINIFERAL EVIDENCE FROM ODP HOLE 1006A

Brent Wilson
Published: 01 April 2013
Journal of Foraminiferal Research (2013) 43 (2): 143–153.
DOI: https://doi.org/10.2113/gsjfr.43.2.143
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Nature and origin of carbonate particles along a transect on the western margin of Great Bahama Bank (Middle Miocene): sedimentary processes and depositional model

Mélanie Turpin, Laurent Emmanuel, Maurice Renard
Published: 01 May 2008
Bulletin de la Société Géologique de France (2008) 179 (3): 231–244.
DOI: https://doi.org/10.2113/gssgfbull.179.3.231
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New allocyclic dimensions in a prograding carbonate bank; evidence for eustatic, tectonic, and paleoceanographic control (late Neogene, Bahamas)

Barbara H. Lidz, Donald F. McNeill
Published: 01 March 1998
Journal of Sedimentary Research (1998) 68 (2): 269–282.
DOI: https://doi.org/10.2110/jsr.68.269
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