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Inland salt marsh

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  • 4 chapters

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Through Saline water, Precipitation and Sodium

Overview

Inland salt marshes (ISMs) are rare, non-tidal wetlands which form either due to the influence of saline groundwater and proximate springs and seeps or from evapotranspiration exceeding precipitation. Primarily located in the Great Lakes region of the US, they are dominantly composed of salt-tolerant, halophytic plant communities including the invasive Phragmites australis (common reed). Anthropogenic impacts on brine springs have decreased their already low global coverage and have led to their classification as G1 critically imperiled ecosystems. Of note, inland salt marshes are globally occurring, though this article primarily discusses ISMs from the US and Europe.

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