Definition
Eustasy originally referred to a globally simultaneous and uniform change in sea level. However, sea-level changes are affected by many processes that operate on different temporal and spatial scales. These processes are described more fully below and summarized in Table 1. Therefore, the original concept of eustasy, as a globally uniform rise in sea level, has been challenged, and some authors suggest abandoning the term altogether (e.g., Carlson and Clark 2012). Nevertheless, eustatic sea level plays an important role within the framework of geophysical models that calculate glacial isostasy (see below; Peltier 2004; Mitrovica et al. 2010; Lambeck et al. 2010; Spada 2017). In current usage, the eustatic sea-level change is the global sea-level change averaged over the surface of the oceans, over a specified time interval (Spada 2017).
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Gornitz, V. (2017). Eustasy. In: Finkl, C., Makowski, C. (eds) Encyclopedia of Coastal Science . Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-48657-4_142-2
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