Storm-Related Rhodolith Deposits from the Upper Pleistocene and Recycled Coastal Holocene on Sal Island (Cabo Verde Archipelago)

This project examines the role of tropical storms in the northeast Atlantic Ocean related to the post-mortem deposition of rhodoliths in coastal settings during Neogene to Holocene time with primary emphasis on Sal Island in the Cabo Verde Archipelago located 600 km off the coast of Senegal in north...

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Published in:Geosciences
Main Authors: Markes E. Johnson, Ricardo Ramalho, Carlos Marques da Silva
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/geosciences10110419
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spelling ftmdpi:oai:mdpi.com:/2076-3263/10/11/419/ 2023-08-20T04:08:40+02:00 Storm-Related Rhodolith Deposits from the Upper Pleistocene and Recycled Coastal Holocene on Sal Island (Cabo Verde Archipelago) Markes E. Johnson Ricardo Ramalho Carlos Marques da Silva agris 2020-10-23 application/pdf https://doi.org/10.3390/geosciences10110419 EN eng Multidisciplinary Digital Publishing Institute Sedimentology, Stratigraphy and Palaeontology https://dx.doi.org/10.3390/geosciences10110419 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 10; Issue 11; Pages: 419 coastal storm deposits wind-driven waves long-shore currents coralline red algae Text 2020 ftmdpi https://doi.org/10.3390/geosciences10110419 2023-08-01T00:20:06Z This project examines the role of tropical storms in the northeast Atlantic Ocean related to the post-mortem deposition of rhodoliths in coastal settings during Neogene to Holocene time with primary emphasis on Sal Island in the Cabo Verde Archipelago located 600 km off the coast of Senegal in northwest Africa. Fossil rhodoliths from 10 to 15 cm in diameter are equal in size to contemporary rhodoliths that survive for a century or more at water depths undisturbed by all but the most energetic storms. The shape of large rhodoliths makes them susceptible to rare disturbances with sufficient energy to export them beyond their preferred habitat into extreme environments that include supratidal settings. The methodology of this study gauges the relative sphericity of rhodoliths based on measurements across three axes perpendicular to one another, plots size variations on bar graphs, and considers whether or not individual nodules are nucleated around rock cores eroded from proximal rocky shores. Sal Island is impacted on a steady basis by wave swell generated from the Northeast Trade Winds, but Pleistocene and Holocene deposits with large rhodoliths on the Island’s windward coast are interpreted as the result of major storms of hurricane intensity. Comparison of Sal Island rhodoliths with Pliocene and Miocene examples from other insular localities in the Northeast Atlantic considers evidence for displacement of the Inter-Tropical Convergence Zone (ITCZ) into more northern latitudes as an influence on past hurricane tracks that are less common today. Text Northeast Atlantic MDPI Open Access Publishing Geosciences 10 11 419
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic coastal storm deposits
wind-driven waves
long-shore currents
coralline red algae
spellingShingle coastal storm deposits
wind-driven waves
long-shore currents
coralline red algae
Markes E. Johnson
Ricardo Ramalho
Carlos Marques da Silva
Storm-Related Rhodolith Deposits from the Upper Pleistocene and Recycled Coastal Holocene on Sal Island (Cabo Verde Archipelago)
topic_facet coastal storm deposits
wind-driven waves
long-shore currents
coralline red algae
description This project examines the role of tropical storms in the northeast Atlantic Ocean related to the post-mortem deposition of rhodoliths in coastal settings during Neogene to Holocene time with primary emphasis on Sal Island in the Cabo Verde Archipelago located 600 km off the coast of Senegal in northwest Africa. Fossil rhodoliths from 10 to 15 cm in diameter are equal in size to contemporary rhodoliths that survive for a century or more at water depths undisturbed by all but the most energetic storms. The shape of large rhodoliths makes them susceptible to rare disturbances with sufficient energy to export them beyond their preferred habitat into extreme environments that include supratidal settings. The methodology of this study gauges the relative sphericity of rhodoliths based on measurements across three axes perpendicular to one another, plots size variations on bar graphs, and considers whether or not individual nodules are nucleated around rock cores eroded from proximal rocky shores. Sal Island is impacted on a steady basis by wave swell generated from the Northeast Trade Winds, but Pleistocene and Holocene deposits with large rhodoliths on the Island’s windward coast are interpreted as the result of major storms of hurricane intensity. Comparison of Sal Island rhodoliths with Pliocene and Miocene examples from other insular localities in the Northeast Atlantic considers evidence for displacement of the Inter-Tropical Convergence Zone (ITCZ) into more northern latitudes as an influence on past hurricane tracks that are less common today.
format Text
author Markes E. Johnson
Ricardo Ramalho
Carlos Marques da Silva
author_facet Markes E. Johnson
Ricardo Ramalho
Carlos Marques da Silva
author_sort Markes E. Johnson
title Storm-Related Rhodolith Deposits from the Upper Pleistocene and Recycled Coastal Holocene on Sal Island (Cabo Verde Archipelago)
title_short Storm-Related Rhodolith Deposits from the Upper Pleistocene and Recycled Coastal Holocene on Sal Island (Cabo Verde Archipelago)
title_full Storm-Related Rhodolith Deposits from the Upper Pleistocene and Recycled Coastal Holocene on Sal Island (Cabo Verde Archipelago)
title_fullStr Storm-Related Rhodolith Deposits from the Upper Pleistocene and Recycled Coastal Holocene on Sal Island (Cabo Verde Archipelago)
title_full_unstemmed Storm-Related Rhodolith Deposits from the Upper Pleistocene and Recycled Coastal Holocene on Sal Island (Cabo Verde Archipelago)
title_sort storm-related rhodolith deposits from the upper pleistocene and recycled coastal holocene on sal island (cabo verde archipelago)
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/geosciences10110419
op_coverage agris
genre Northeast Atlantic
genre_facet Northeast Atlantic
op_source Geosciences; Volume 10; Issue 11; Pages: 419
op_relation Sedimentology, Stratigraphy and Palaeontology
https://dx.doi.org/10.3390/geosciences10110419
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/geosciences10110419
container_title Geosciences
container_volume 10
container_issue 11
container_start_page 419
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