Geochemistry at DSDP Legs 36 and 71 Holes

• Main Authors: Robert, Christian, Maillot, Henri
• Format: Dataset
• Language: English
• Published: PANGAEA 1983
• Subjects: 36-327A; 36-329; 36-330; 71-511; 71-513; 71-513A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg36; Leg71; South Atlantic/BANK; South Atlantic/CONT RISE; South Atlantic/FLANK; South Atlantic/PLATEAU; Antarctic; Southern Ocean; The Antarctic; Drake Passage; Falkland Plateau; Antarc*; Ice Sheet; South Atlantic Ocean
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.814000; https://doi.org/10.1594/PANGAEA.814000

For Middle Jurassic to Pleistocene times, clay mineralogical and geochemical data provide information on the evolution of continental and marine paleoenvironments. They are a source of information on marginal instability, on the continental and shallow marine environments related to the development of the Southern Ocean during the Middle and Late Jurassic, and on tectonic relaxation of the continental margins at the end of the Late Jurassic. They also provide evidence for the influences of the South Atlantic opening and the movement of the Falkland Plateau in a reduced marine environment until Aptian-Albian times, and the transition to an open marine environment during Albian time; the influences of the Albian-Turonian and Coniacian-Santonian Andean deformations in an open marine environment; the limited tectonic effects and strong influence of marine currents at the Cretaceous/Tertiary boundary; the influences of the global climatic cooling and inferred bottom water circulation during the late Eocene and Oligocene; the widening of the South Atlantic Ocean during Oligocene time, which was accompanied by an increased influence of the biogenic components on sedimentation; increased carbonate dissolution from late Oligocene to early Miocene, related to the deepening of the ocean; limited mineralogical and important geochemical modifications when the Drake Passage opened in the early Miocene; the influence of the late Miocene development of the Antarctic ice-sheet; the major Antarctic cooling and Patagonian glaciation during Pliocene time; and the change in the Antarctic Bottom Water circulation at the Pliocene/Pleistocene boundary.