Abstract

Abstract. Today, coastal cities worldwide are facing major changes resulting from climate change and anthropogenic forcing, which requires adaptation and mitigation strategies to be established. In this context, sedimentological archives in many Mediterranean cities record a multi-millennial history of environmental dynamics and human adaptation, revealing a long-lasting resilience. Founded by the Phoenicians around 3000 years ago, Cádiz (south-western Spain) is a key example of a coastal resilient city. This urban centre is considered to be one of the first cities of western Europe and has experienced major natural hazards during its long history, such as coastal erosion, storms, and also tsunamis (like the one in 1755 CE following the destructive Lisbon earthquake). In the framework of an international, joint archaeological and geoarchaeological project, three cores have been drilled in a marine palaeochannel that ran through the ancient city of Cádiz. These cores reveal a ≥50 m thick Holocene sedimentary sequence. Importantly, most of the deposits date from the 1st millennium BCE to the 1st millennium CE. This exceptional sedimentary archive will allow our scientific team to achieve its research goals, which are (1) to reconstruct the palaeogeographical evolution of this specific coastal area; (2) to trace the intensity of activities of the city of Cádiz based on archaeological data, as well as geochemical and palaeoecological indicators; and (3) to identify and date high-energy event deposits such as storms and tsunamis.

Highlights

  • Focusing on the city of Cádiz (Figs. 1, 2, 3), this starting international, geoarchaeological project offers outstanding research perspectives for two main reasons

  • Sedimentological archives in many Mediterranean cities record a multi-millennial history of environmental dynamics and human adaptation, revealing a long-lasting resilience

  • Afterwards, its history was closely linked to the main Mediterranean societies developing along its shores, experiencing successive Punic (Ramírez Delgado, 1982) and Roman domination (Bernal Casasola, 2008; Lara Medina, 2016; Bernal Casasola et al, 2019a)

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Summary

Introduction

Focusing on the city of Cádiz (Figs. 1, 2, 3), this starting international, geoarchaeological project offers outstanding research perspectives for two main reasons. Afterwards, its history was closely linked to the main Mediterranean societies developing along its shores, experiencing successive Punic (Ramírez Delgado, 1982) and Roman domination (Bernal Casasola, 2008; Lara Medina, 2016; Bernal Casasola et al, 2019a) During late antiquity, it was conquered by the Visigoths, and later by Moors in the 8th century (Fresnadillo García et al, 2008). In 2018, the University of Cádiz started to rehabilitate the Valcárcel building located above the Bahía-Caleta palaeochannel In this context, an interdisciplinary project was initiated: archaeological excavations were conducted alongside drilling of three sedimentary cores from the same area. Sedimentological and palaeoenvironmental evidence of high-energy events could be documented in this palaeochannel This project aims to understand how this city faced coastal hazards and adapted to environmental change across its history, especially during the 1st millennium BCE to the 1st millennium CE. This includes how the landscape of Cádiz appeared at the time of its foundation and how it evolved through time

Geodynamic background
Coastal areas around the Bay of Cádiz
Geoarchaeological and geomorphological studies of the Guadalete River
Methodology
New sedimentary sequences from the city centre of Cádiz
The Bahía-Caleta palaeochannel in Cádiz: a deep palaeogorge?
Late Holocene coastal dynamics and preliminary results
Palaeogeography
High-energy events from the sea: palaeostorms and palaeotsunamis
Urban geoarchaeology
Palaeoeconomy
Full Text
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