Dispersal models alert on the risk of non‐native species introduction by Ballast water in protected areas from the Western Antarctic Peninsula
Abstract Aim The Western Antarctic Peninsula is challenged by climate change and increasing maritime traffic that together facilitate the introduction of marine non‐native species from warmer regions neighbouring the Southern Ocean. Ballast water exchange has been frequently reported as an introduct...
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crwiley:10.1111/ddi.13464 2024-10-13T14:03:03+00:00 Dispersal models alert on the risk of non‐native species introduction by Ballast water in protected areas from the Western Antarctic Peninsula Dulière, Valérie Guillaumot, Charlène Lacroix, Geneviève Saucède, Thomas López‐Farran, Zambra Danis, Bruno Schön, Isa Baetens, Katrijn Briski, Elizabeta 2022 http://dx.doi.org/10.1111/ddi.13464 https://onlinelibrary.wiley.com/doi/pdf/10.1111/ddi.13464 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/ddi.13464 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Diversity and Distributions volume 28, issue 4, page 649-666 ISSN 1366-9516 1472-4642 journal-article 2022 crwiley https://doi.org/10.1111/ddi.13464 2024-09-17T04:52:05Z Abstract Aim The Western Antarctic Peninsula is challenged by climate change and increasing maritime traffic that together facilitate the introduction of marine non‐native species from warmer regions neighbouring the Southern Ocean. Ballast water exchange has been frequently reported as an introduction vector. This study uses a Lagrangian approach to model the passive drift of virtual propagules departing from Ballast water hypothetic exchange zones, at contrasting distances from the coasts. Location Western Antarctic Peninsula. Methods Virtual propagules were released over the 2008–2016 period and at three distances from the nearest coasts: 200 (convention for the management of Ballast Water, 2004), 50 or 11 nautical miles (NM). Results Results show that exchanging Ballast water at 200 NM considerably reduces the arrival of propagules in proposed marine protected areas of the western side of the Antarctic Peninsula. On the eastern side, propagules can reach north‐eastern marine protected areas within a few days due to strong currents for all tested scenarios. Seasonal and yearly variations indicate that exceptional climate events could influence the trajectory of particles in the region. Ballast water should be exchanged at least 200 NM offshore on the western side of the Antarctic Peninsula and avoided on the eastern side to limit particle arrival in proposed marine protected areas. Focusing on Deception Island, our results suggested that the Patagonian crab ( Halicarcinus planatus ) observed in 2010 could have been introduced in case of Ballast water exchange at 50 NM or less from the coast. Main conclusions This study highlights the importance of respecting Ballast water exchange convention to limit the risk of non‐native species introduction. Ballast water exchange should be operated at least at 200 NM from the coasts, which further limits particle arrival in shallow water areas. This is especially important in the context of a more visited and warmer Southern Ocean. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Deception Island Southern Ocean Wiley Online Library Antarctic Southern Ocean The Antarctic Antarctic Peninsula Deception Island ENVELOPE(-60.633,-60.633,-62.950,-62.950) Diversity and Distributions 28 4 649 666 |
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Open Polar |
collection |
Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Aim The Western Antarctic Peninsula is challenged by climate change and increasing maritime traffic that together facilitate the introduction of marine non‐native species from warmer regions neighbouring the Southern Ocean. Ballast water exchange has been frequently reported as an introduction vector. This study uses a Lagrangian approach to model the passive drift of virtual propagules departing from Ballast water hypothetic exchange zones, at contrasting distances from the coasts. Location Western Antarctic Peninsula. Methods Virtual propagules were released over the 2008–2016 period and at three distances from the nearest coasts: 200 (convention for the management of Ballast Water, 2004), 50 or 11 nautical miles (NM). Results Results show that exchanging Ballast water at 200 NM considerably reduces the arrival of propagules in proposed marine protected areas of the western side of the Antarctic Peninsula. On the eastern side, propagules can reach north‐eastern marine protected areas within a few days due to strong currents for all tested scenarios. Seasonal and yearly variations indicate that exceptional climate events could influence the trajectory of particles in the region. Ballast water should be exchanged at least 200 NM offshore on the western side of the Antarctic Peninsula and avoided on the eastern side to limit particle arrival in proposed marine protected areas. Focusing on Deception Island, our results suggested that the Patagonian crab ( Halicarcinus planatus ) observed in 2010 could have been introduced in case of Ballast water exchange at 50 NM or less from the coast. Main conclusions This study highlights the importance of respecting Ballast water exchange convention to limit the risk of non‐native species introduction. Ballast water exchange should be operated at least at 200 NM from the coasts, which further limits particle arrival in shallow water areas. This is especially important in the context of a more visited and warmer Southern Ocean. |
author2 |
Briski, Elizabeta |
format |
Article in Journal/Newspaper |
author |
Dulière, Valérie Guillaumot, Charlène Lacroix, Geneviève Saucède, Thomas López‐Farran, Zambra Danis, Bruno Schön, Isa Baetens, Katrijn |
spellingShingle |
Dulière, Valérie Guillaumot, Charlène Lacroix, Geneviève Saucède, Thomas López‐Farran, Zambra Danis, Bruno Schön, Isa Baetens, Katrijn Dispersal models alert on the risk of non‐native species introduction by Ballast water in protected areas from the Western Antarctic Peninsula |
author_facet |
Dulière, Valérie Guillaumot, Charlène Lacroix, Geneviève Saucède, Thomas López‐Farran, Zambra Danis, Bruno Schön, Isa Baetens, Katrijn |
author_sort |
Dulière, Valérie |
title |
Dispersal models alert on the risk of non‐native species introduction by Ballast water in protected areas from the Western Antarctic Peninsula |
title_short |
Dispersal models alert on the risk of non‐native species introduction by Ballast water in protected areas from the Western Antarctic Peninsula |
title_full |
Dispersal models alert on the risk of non‐native species introduction by Ballast water in protected areas from the Western Antarctic Peninsula |
title_fullStr |
Dispersal models alert on the risk of non‐native species introduction by Ballast water in protected areas from the Western Antarctic Peninsula |
title_full_unstemmed |
Dispersal models alert on the risk of non‐native species introduction by Ballast water in protected areas from the Western Antarctic Peninsula |
title_sort |
dispersal models alert on the risk of non‐native species introduction by ballast water in protected areas from the western antarctic peninsula |
publisher |
Wiley |
publishDate |
2022 |
url |
http://dx.doi.org/10.1111/ddi.13464 https://onlinelibrary.wiley.com/doi/pdf/10.1111/ddi.13464 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/ddi.13464 |
long_lat |
ENVELOPE(-60.633,-60.633,-62.950,-62.950) |
geographic |
Antarctic Southern Ocean The Antarctic Antarctic Peninsula Deception Island |
geographic_facet |
Antarctic Southern Ocean The Antarctic Antarctic Peninsula Deception Island |
genre |
Antarc* Antarctic Antarctic Peninsula Deception Island Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Deception Island Southern Ocean |
op_source |
Diversity and Distributions volume 28, issue 4, page 649-666 ISSN 1366-9516 1472-4642 |
op_rights |
http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1111/ddi.13464 |
container_title |
Diversity and Distributions |
container_volume |
28 |
container_issue |
4 |
container_start_page |
649 |
op_container_end_page |
666 |
_version_ |
1812819484344320000 |