37 Integrating Field and Modeling Approaches to Understand Changing Coastal Systems (Posters)

Saturday, 21 March 2020
8:00 AM - 12:00 PM
Grand Ballroom A–D

IMPROVING SEA LEVEL MODELS FOR THE NEW YORK BIGHT WITH SUBMERGED PEATS

Paper number: 37-21
Program: Theme Sessions
Time: 8:00 AM – 12:00 PM

Authors

Abstract

Since the early 1900s, scallop fisherman trawling along the shores of Long Island have noted peat deposits under the Atlantic Ocean (1). These deposits are records of submerged land and contain tree trunks and mammoth teeth (2). Previous work (3) has shown that the submerged peat can be up to 12,000 years old. Though these deposits provide a valuable record of past environmental changes and help create models of how and at what rates local sea level has changed, there has not been extensive research on these deposits since the 1970s. Understanding sea level change in the Northeast is especially important due to its high population affected by future sea level rise. New sediment cores conducted by the Bureau of Ocean and Energy Management (BOEM) in this region reveal peat deposits buried under 2-3m of sand and clay 15km off shore Long Island in the Atlantic Ocean (3) and provide the opportunity to investigate a unique pattern of environmental change. We use a variety of techniques to characterize these changes and look for evidence of past storms and sea level change, including: sedimentological analysis and radiocarbon dating.

Our results provide evidence for an event such as a storm or tsunami that drastically transformed the land from terrestrial to marine approximately 5,000-7,000 kyr ago. We are continuing to work on understanding the event caused this change, its rate, and nature of the terrestrial environment. The peat reflects a terrestrial environment and the cores are currently at 24.2m water depth, therefore sea level has risen at least that amount since they formed. This information is crucial for constraining and understanding all the variables that impact sea level change. Since the last glacial maximum (~20,000 ka), when the Laurentide Ice Sheet melted, the land in Canada has been uplifting while the coastal US is sinking. This process, known as glacial isostatic adjustment (GIA) has major implications for forecasting future sea level change in the Northeastern US; however, it is not currently well constrained (4). Our results from the BOEM cores provide important new constraints for North American and Atlantic GIA estimates and will improve sea level and flood models for North America and Europe over the next several hundred years.

  1. Emery + (1967)
  2. Whitmore + (1967)
  3. BOEM, OCS Study Report 2012-008
  4. Rovere + (2016)

Geological Society of America Abstracts with Programs. Vol. 52, No. 2

doi: 10.1130/abs/2020SE-342905

© Copyright 2020 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.