Paleogene Newfoundland sediment drifts

• Main Authors: R. D. Norris, P. A. Wilson, P. Blum, A. Fehr, AGNINI, CLAUDIA, A. Bornemann, S. Boulila, P. R. Bown, C. Cournede, O. Friedrich, A. Kumar Ghosh, C. J. Hollis, P. M. Hull, K. Jo, C. K. Junium, M. Kaneko, D. Liebrand, P. C. Lippert, Z. Liu, H. Matsui, K. Moriya, H. Nishi, B. N. Opdyke, D. Penman, B. Romans, H. D. Scher, P. Sexton, H. Takagi, S. Kirtland Turner, J. H. Whiteside, T. Yamaguchi, Y. Yamamoto
• Other Authors: R. D., Norri, P. A., Wilson, P., Blum, A., Fehr, Agnini, Claudia, A., Bornemann, S., Boulila, P. R., Bown, C., Cournede, O., Friedrich, A., Kumar Ghosh, C. J., Holli, P. M., Hull, K., Jo, C. K., Junium, M., Kaneko, D., Liebrand, P. C., Lippert, Z., Liu, H., Matsui, K., Moriya, H., Nishi, B. N., Opdyke, D., Penman, B., Roman, H. D., Scher, P., Sexton, H., Takagi, S., Kirtland Turner, J. H., Whiteside, T., Yamaguchi, Y., Yamamoto
• Format: Article in Journal/Newspaper
• Language: English
• Published: Integrated Ocean Drilling Program Management International, Inc. 2012
• Subjects: Paleogene; Newfoundland; North Atlantic; Northwest Atlantic
• Online Access: http://hdl.handle.net/11577/2572744; https://doi.org/10.2204/iodp.pr.342.2012; http://publications.iodp.org/preliminary_report/342/index.html

Integrated Ocean Drilling Program Expedition 342 was designed to recover Paleogene sedimentary sequences with unusually high deposition rates across a wide range of water depths (Sites U1403–U1411). The drilling area is positioned to capture sedimentary and geochemical records of ocean chemistry and overturning circulation beneath the flow of the Deep Western Boundary Current in the northwest Atlantic Ocean. In addition, two operational days were dedicated to a sea trial of the Motion Decoupled Hydraulic Delivery System developmental tool (Site U1402). The expedition was primarily targeted at reconstructing the Paleogene carbonate compensation depth (CCD) in the North Atlantic for reference to recently obtained high-fidelity records of the CCD in the equatorial Pacific. The site located in the deepest water (Site U1403) was at a paleodepth of ~4.5 km 50 m.y. ago, whereas the site located in the shallowest water (Site U1408) can be backtracked to a paleodepth of 2.5 km at the same time. The combination of sites yields a record of the history of CCD change over a 2 km depth range from the ocean abyss to middle range water depths. Notable findings include the discovery of intermittent calcareous sediments in the Cretaceous, Paleocene, and early to middle Eocene at 4.5 km paleodepth, suggesting a deep Atlantic CCD during these times. We find evidence of carbonate deposition events following the Cretaceous/Paleogene (K/Pg) boundary mass extinction, the Paleocene/Eocene Thermal Maximum, and the Eocene–Oligocene transition. These deposition events may reflect the rebalancing of ocean alkalinity after mass extinctions or abrupt global climate change. Intervals during which the CCD appears to have been markedly shallow in the North Atlantic include the Early Eocene Climatic Optimum, the late Eocene, and the middle Oligocene. A second major objective of Expedition 342 was to recover clay-rich sequences with well-preserved microfossils and high rates of accumulation in comparison to the modest rates of accumulation (~0.5–1 ...