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Geomorphological dynamics at the coast

A sedimentary stratigraphy for Atlit-Yam, the earliest coastal village at the Eastern Mediterranean and its submerged landscape

Dados Bibliográficos

ID24138997
AutoresVishal Kataria (University of Haifa), Gilad Shtienberg (0000-0003-0303-7872, University of Haifa), Isaac Ogloblin Ramírez (0000-0001-7793-6147, Rutgers, the State University of New Jersey), Roni Zuckerman-Cooper (0009-0008-6013-295X), Roni Zuckerman‐Cooper (Qualcomm (United States)), Nimer Taha (University of Haifa), E Grono (0000-0002-3607-6686, University of Haifa), Marko Runjajić (0000-0002-4086-4386, University of Haifa), Ehud Galili (0000-0002-9621-4921, University of Haifa), Nicolas Waldmann (0000-0003-4627-208X, University of Haifa), D E Friesem (0000-0002-5541-6156, University of Cambridge)
Ano2026
Volume783
Páginas110434
Data de publicação2026-11-01
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoQuaternary International (JOURNAL)
Identificadores do periódicoISSN: 1040-6182 • E-ISSN: 1873-4553
EditoraElsevier BV (PUBLISHER)
DOI10.1016/j.quaint.2026.110434
OpenAlexW7135217946
IdiomaEN
Referências citadas76

During the early Holocene, rapid sea level rise led to the inundation of worldwide coastal areas, with the surrounding shallow landscapes being the most affected. The Carmel coast, located in the East Mediterranean, preserves a rich record of such a submerged landscape dotted by many archaeological sites, including the well-preserved Atlit-Yam village (Neolithic), which is currently buried and submerged at 8-11 m water depth. In order to reconstruct the geomorphological evolution of the submerged landscape, 23 sediment cores of variable length (ranging 60-240 cm) were drilled both inside and outside the known extent of the Atlit-Yam village. A detailed stratigraphy of the submerged landscape was generated based on the analysis of 18 out of 23 cores, framed by robust radiocarbon ages. The sedimentary sequences identified in the analyzed cores were defined by respective facies associations, and combined with physical (grain size, magnetic susceptibility), chemical (elemental geochemistry), and organic (total organic content) properties of the sediments. Our analysis reveals a non-uniform evolution of submerged coastal sediments, influenced by sediment supply, regional geomorphology, and human activity. Within a spatial stratigraphy, we found distinct anthropogenic units that underlines the intricate balance between humans and the Early Holocene changing environment (including sea level rise, depositional processes, and sediment dynamics). This study holds implications for future research in identifying and preserving potential archeological sites elsewhere and helps to shed light on the impact of climate change, sea level, and surface processes on coastal communities.

Facies · Geoarchaeology · Holocene · Radiocarbon dating · Sea level · Sediment · Sedimentary depositional environment · Sedimentary rock · Geology and Paleoclimatology Research · Marine and environmental studies · Maritime and Coastal Archaeology · Stratigraphy

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