3.8 Article

High-resolution late Holocene sedimentary cores record the long history of the city of Cadiz (south-western Spain)

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SCIENTIFIC DRILLING
卷 27, 期 -, 页码 35-47

出版社

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/sd-27-35-2020

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资金

  1. Government of Spain/FEDER [HAR2016-78691-P]
  2. SA-CEIMAR of the CEIMAR Excellence Campus (University of Cadiz)
  3. ARQUEOSTRA of the Junta de Andalucia - Investments for the Future programme of the French Government [P18-FR-1483, 2019-250]
  4. ARQUEOFISH of the Junta de Andalucia - Investments for the Future programme of the French Government [P18-FR-1483, 2019-250]
  5. PheniCane - CNRS (MITI-PEPS ECOMOB)

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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, Cadiz (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 Cadiz. These cores reveal a >= 50m 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 Cadiz 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.

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