Holocene relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America
Abstract Predicting coastal change depends upon our knowledge of postglacial relative sea-level variability, partly controlled by glacio-isostatic responses to ice-sheet melting. Here, we reconstruct the postglacial relative sea-level changes along the Caribbean and Pacific coasts of northwestern So...
Published in: | Quaternary Research |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
2024
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/qua.2023.73 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S003358942300073X |
id |
crcambridgeupr:10.1017/qua.2023.73 |
---|---|
record_format |
openpolar |
spelling |
crcambridgeupr:10.1017/qua.2023.73 2024-06-16T07:40:45+00:00 Holocene relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America Paniagua-Arroyave, Juan F. Spada, Giorgio Melini, Daniele Duque-Trujillo, José F. 2024 http://dx.doi.org/10.1017/qua.2023.73 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S003358942300073X en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Quaternary Research volume 119, page 28-43 ISSN 0033-5894 1096-0287 journal-article 2024 crcambridgeupr https://doi.org/10.1017/qua.2023.73 2024-05-22T12:56:16Z Abstract Predicting coastal change depends upon our knowledge of postglacial relative sea-level variability, partly controlled by glacio-isostatic responses to ice-sheet melting. Here, we reconstruct the postglacial relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America by numerically solving the sea-level equation with two scenarios of mantle viscosity: global standard average and high viscosity. Our results with the standard model (applicable to the Pacific coast) agree with earlier studies by indicating a mid-Northgrippian high stand of ~2 m. The high-viscosity simulation (relevant to the Caribbean coast) shows that the transition from far- to intermediate-field influence of the Laurentide Ice Sheet occurs between Manzanillo del Mar and the Gulf of Morrosquillo. South of this location, the Colombian Caribbean coast has exhibited a still stand with a nearly constant Holocene relative sea level. By analyzing our simulations considering sea-level indicators, we argue that tectonics is more prominent than previously assumed, especially along the Caribbean coast. This influence prevents a simplified view of regional relative sea-level changes on the northwestern South American coast. Article in Journal/Newspaper Ice Sheet Cambridge University Press Pacific Quaternary Research 1 16 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract Predicting coastal change depends upon our knowledge of postglacial relative sea-level variability, partly controlled by glacio-isostatic responses to ice-sheet melting. Here, we reconstruct the postglacial relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America by numerically solving the sea-level equation with two scenarios of mantle viscosity: global standard average and high viscosity. Our results with the standard model (applicable to the Pacific coast) agree with earlier studies by indicating a mid-Northgrippian high stand of ~2 m. The high-viscosity simulation (relevant to the Caribbean coast) shows that the transition from far- to intermediate-field influence of the Laurentide Ice Sheet occurs between Manzanillo del Mar and the Gulf of Morrosquillo. South of this location, the Colombian Caribbean coast has exhibited a still stand with a nearly constant Holocene relative sea level. By analyzing our simulations considering sea-level indicators, we argue that tectonics is more prominent than previously assumed, especially along the Caribbean coast. This influence prevents a simplified view of regional relative sea-level changes on the northwestern South American coast. |
format |
Article in Journal/Newspaper |
author |
Paniagua-Arroyave, Juan F. Spada, Giorgio Melini, Daniele Duque-Trujillo, José F. |
spellingShingle |
Paniagua-Arroyave, Juan F. Spada, Giorgio Melini, Daniele Duque-Trujillo, José F. Holocene relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America |
author_facet |
Paniagua-Arroyave, Juan F. Spada, Giorgio Melini, Daniele Duque-Trujillo, José F. |
author_sort |
Paniagua-Arroyave, Juan F. |
title |
Holocene relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America |
title_short |
Holocene relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America |
title_full |
Holocene relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America |
title_fullStr |
Holocene relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America |
title_full_unstemmed |
Holocene relative sea-level changes along the Caribbean and Pacific coasts of northwestern South America |
title_sort |
holocene relative sea-level changes along the caribbean and pacific coasts of northwestern south america |
publisher |
Cambridge University Press (CUP) |
publishDate |
2024 |
url |
http://dx.doi.org/10.1017/qua.2023.73 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S003358942300073X |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Quaternary Research volume 119, page 28-43 ISSN 0033-5894 1096-0287 |
op_rights |
http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1017/qua.2023.73 |
container_title |
Quaternary Research |
container_start_page |
1 |
op_container_end_page |
16 |
_version_ |
1802007736651612160 |