Learning from Geomorphological Adaptation of Coasts at Different Time Scales (2nd Edition)

A special issue of Journal of Marine Science and Engineering (ISSN 2077-1312). This special issue belongs to the section "Coastal Engineering".

Deadline for manuscript submissions: 20 June 2025 | Viewed by 711

Special Issue Editors


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Guest Editor
Centro de Investigação Marinha e Ambiental (CIMA), Universidade do Algarve, 8005-139 Faro, Portugal
Interests: coastal evolution; temporal scales; dune–beach morphodynamics
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Guest Editor
Department of Earth and Environment, Boston University, Boston, MA 02215, USA
Interests: shallow marine geology; the morphodynamics of bedform evolution; the inner-shelf sedimentary signatures from transgressions and regressions
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

It is with great pleasure that I announce the publication of a Special Issue with the aim of bringing in examples that show how coastal systems react and adapt at different temporal scales and to different stressors. Natural systems respond and adapt to changing environmental conditions or other disturbances over time. A major constraint in understanding coastal adaptation at long-term temporal scales lies in the elevated degree of complexity of the responses, a consequence of their non-linearity and the many feedbacks that exist among the different components of a coastal system. This prevents extrapolating observations to capture short- to medium-term coastal adaptations. The stratigraphic record may significantly contribute to understanding the response of natural systems at longer time scales. However, the testimony left by the continuum of change on the coast may be partially incomplete or may not capture all possible response pathways. As coastal resilience is inextricably linked to these adaptation strategies, taking place over the full spectrum of coastal change, it is extremely relevant to explore and compile examples assessing the different scales of change in order to identify not only possible tipping points but also the consequences of crossing such boundaries.

Dr. Susana Costas
Prof. Dr. Duncan M. FitzGerald
Guest Editors

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Keywords

  • coastal barrier evolution, vulnerability, and resilience
  • evidence of non-linear barrier dynamics over distinct temporal scales
  • beach and dune morphodynamics
  • shoreline evolution from years to decades
  • perturbations and (eco)geomorphic adaptation of beach–dune systems across timescales
  • formation, evolution, and sealing of transgressive coastal dunes
  • observations of coastal adaptation through different time scales
  • impacts of climate and meteocean conditions variability on the beach–dune system
  • cross-scale integration of coastal barrier changes

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Published Papers (1 paper)

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Research

12 pages, 4494 KiB  
Article
Visualization of Coastal Carbonate Lithosomes: Color-Intensity Patterns and Georadar Imaging of a Semi-Lithified Strandplain, Eleuthera Island, The Bahamas
by Ilya V. Buynevich, Michael Savarese and H. Allen Curran
J. Mar. Sci. Eng. 2025, 13(5), 950; https://doi.org/10.3390/jmse13050950 - 14 May 2025
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Abstract
Quaternary carbonate strandplains serve as archives of land–sea interaction, including the impacts of storms and tsunamis. Incipient lithification, especially of compound beach/dune ridges within the action zone of salt spray, presents challenges to geological research, which is often limited to exposures. This study [...] Read more.
Quaternary carbonate strandplains serve as archives of land–sea interaction, including the impacts of storms and tsunamis. Incipient lithification, especially of compound beach/dune ridges within the action zone of salt spray, presents challenges to geological research, which is often limited to exposures. This study combines aerial image analysis with geophysical datasets to assess the morphostratigraphy and internal structure of the Freedom Beach Strandplain along southern Eleuthera Island, The Bahamas. Color-intensity analysis of field photographs and satellite images revealed general patterns that can be used to distinguish between areas with different grayscale parameters (sand-covered surfaces, lithified ridges, vegetation, etc.). Cross-shore (dip-section) high-resolution (800 MHz) georadar images across ten ridges (A-J) documented the internal architecture of swash-aligned ridge–swale sets. Signatures attributed to storms include truncations in shore-normal radargrams, scour features in alongshore (strike-section) images, and an extensive accumulation of large mollusk shells along one of the oldest ridges (ridge J). Preliminary radiocarbon dating yielded ages of up to 600 years, suggesting intense storms with 50–60-year periodicity as a possible mechanism for ridge formation. Full article
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