Sea Level History in 3D: Early results of an ultra-high resolution MCS survey across IODP Expedition 313 drillsites

Tuesday, 15 December 2015
Poster Hall (Moscone South)
Gregory S Mountain1, Hilmi Mert Kucuk2,3, Mladen R Nedimovic4, James A Austin Jr5, Craig Fulthorpe5, Andrew Newton6, Kimberly Baldwin7, Christopher Johnson1, James N. Stanley7 and Tarini Bhatnagar8, (1)Rutgers University New Brunswick, New Brunswick, NJ, United States, (2)Lamont -Doherty Earth Observatory, Borehole Research Group, Palisades, NY, United States, (3)Dokuz Eyl├╝l University, Institute of Marine Sciences and Technology, Izmir, Turkey, (4)Dalhousie University, Halifax, NS, Canada, (5)University of Texas at Austin, Austin, TX, United States, (6)University of Manchester, Manchester, United Kingdom, (7)Rutgers University, Earth and Planetary Sciences, Piscataway, NJ, United States, (8)Columbia University, New york city, NY, United States
Although globally averaged sea level is rising at roughly 3 mm/yr (and is accelerating), rates of local sea-level change measured at coastlines may differ from this number by a factor of two or more; at some locations, sea level may even be falling. This is due to local processes that can match or even reverse the global trend, making it clear that reliable predictions of future impacts of sea-level rise require a firm understanding of processes at the local level. The history of local sea-level change and shoreline response is contained in the geologic record of shallow-water sediments. We report on a continuing study of sea-level history in sediments at the New Jersey continental margin, where compaction and glacial isostatic adjustment are currently adding 2 mm/yr to the globally averaged rise.

We collected 570 sq km of ultra-high resolution 3D MCS data aboard the R/V Langseth in June-July 2015; innovative recording and preliminary results are described by Nedimovic et al. in this same session. The goal was to provide regional context to coring and logging at IODP Exp 313 sites 27-29 that were drilled 750 m into the New Jersey shelf in 2009. These sites recovered a nearly continuous record of post-Eocene sediments from non-marine soils, estuaries, shoreface, delta front, pro-delta and open marine settings. Existing seismic data are good but are 2D high-resolution profiles at line spacings too wide to enable mapping of key nearshore features. The Langseth 3D survey used shallow towing of a tuned air gun array to preserve high frequencies, and twenty-four 50-m PCables each 12.5 apart provided 6.25 x 3.125 m common-midpoint bins along seventy-seven 50-km sail lines.

With this especially dense spatial resolution of a pre-stack time migrated volume we expect to map rivers, incised valleys, barrier islands, inlets and bays, pro-delta clinoforms, tidal deltas, sequence boundaries, debris flow aprons, and more. Seismic attributes linked to sedimentary facies and geochronology at Exp 313 drill sites will be extended throughout the volume to map the local response to global sea-level change. These analyses will provide an unrivaled opportunity to gauge the local expression of sea-level change for much of the last 40 Ma and lead to informed predictions regarding impacts of a global rise of sea level expected to continue well into the future.