Navarre Beach Marine Sanctuary

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General information about the effort to establish beach accessible diving and snorkeling reefs at Navarre Beach, Florida

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Perhaps it does. Sea level rise may change the spatial structure of marshes where up to some point, it would enhance habitat provision. With all the concern about sea level rise degrading marshes, what will really happen to marshes as habitats as the sea level rises in the coming years? Using a landscape ecology approach, we modeled how habitat properties such as area, edge density, fractal dimension and connectivity of salt marsh patches change with different rates of sea level rise. We found that moderate sea level rise retains and even improves habitat complexity. Marsh area, edge density and mean patch sized increased. Nearest neighborhood distance and juxtaposition between marsh patches and fractal dimension of the seaward edges remained constant. Patch size carrying capacity for select estuarine fishes also increased. Of course, patch connectivity improves when tidal barriers are removed to accommodate sea level rise. All these lead us to suggest that sea level rise may temporarily have positive effect for fish until rates of rise become so high that they drown the marshes or marshes are faced with coastal squeeze.

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With technical advances in surface seismic and downhole electrical imaging techniques, it is now possible to not only map the distribution of reservoir sandstones in the subsurface, but to accurately define the orientation of productive fairways, or “sweet-spots”, within the sequence. Channel sands frequently have favorable reservoir characteristics. Having often been laid down in higher energy settings, they commonly have coarser and better sorted grains, less clay and improved poro-perm characteristics. However, they often have limited lateral extent and shoe-string geometries which make them more difficult to predict in the subsurface.

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On Friday, March 19, 2021, ICLR conducted a Friday Forum webinar titled 'Solutions for Tantramar marshes flooding', led by Dr. Jeff 0llerhead, Professor, Geography and Environment Department, Mount Allison University. Most former salt marshes in the Tantramar region of Atlantic Canada are now protected by dykes and are used primarily for agriculture. This has been true for decades to centuries and, as such, their elevation can be as much as 2 m below that of undyked salt marshes in the region. The key environmental drivers shaping the marshes are changing over time with climate change. The rate of relative sea level (RSL) rise is accelerating and there is some evidence that storms are becoming more frequent and sea ice is diminishing. The risk of a catastrophic dyke failure and associated flooding increases each year. Risk from inland flooding is also increasing. Possible solutions include a combination of: (i) raise and reenforce the dyke system, (ii) realign existing dykes and restore salt marshes to provide natural protection, and (iii) remove existing dykes and allow the system to return to a natural state. The highest priority for managing our salt marshes should be to provide them with sufficient accommodation space into which they can transgress naturally. Jeff 0llerhead is a member of the Geography and Environment Department at Mount Allison University in Sackville, NB. He is a coastal geomorphologist who studies beaches and salt marshes. In recent years, he has been particularly involved in designing and monitoring salt marsh restorations in the upper Bay of Fundy.

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