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. 2017 Oct 5;62(6):2829–2849. doi: 10.1002/lno.10664

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© 2017 The Authors Limnology and Oceanography published by Wiley Periodicals, Inc. on behalf of Association for the Sciences of Limnology and Oceanography

This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made.

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Bathymetric map of the Nauset Marsh system. Salt Pond is connected to the Atlantic Ocean and other drowned kettle holes within the marsh through a network of shallow channels within a central marsh area. Upper left: Salt Pond bathymetry. The red line indicates a section that passes through the location of the observatory raft (red circle) and is represented in profile in the middle left bathymetry section. Lower left: Cumulative distribution of bottom depths within Salt Pond. About half the pond is ≤ 2 m deep.