Please use this identifier to cite or link to this item: http://197.159.135.214/jspui/handle/123456789/842
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dc.contributor.authorTraore, Sienfoungo-
dc.date.accessioned2024-05-20T16:08:57Z-
dc.date.available2024-05-20T16:08:57Z-
dc.date.issued2023-
dc.identifier.urihttp://197.159.135.214/jspui/handle/123456789/842-
dc.descriptionA Thesis submitted to the West African Science Service Center on Climate Change and Adapted Land Use and Universidade Técnica do Atlântico, Cabo Verde in partial fulfillment of the requirements for the Master of Science Degree in Climate Change and Marine Scienceen_US
dc.description.abstractZooplankton are diverse animals found in the ocean, ranging from microscopic to larger invertebrates, and they are crucial to marine ecosystems. Some zooplankton species migrate vertically towards the oxygen-poor waters during the day, which could affect oxygen consumption and release of dissolved compounds, such as ammonium, into deep water. This study provides an overview of zooplankton distribution in the eastern North Atlantic Ocean. Zooplankton was sampled depth stratified along a transect from Cabo Verde to the English Channel using a 150 μm multinet. An analysis of taxon composition identified 11 taxa. Copepoda and Sagittoidea were the most abundant organisms. Stations located in upwelling areas had high biomasses. Stations sampled at night had higher abundances than those sampled during the day. Hydroacoustic data from the EK80 indicated that organisms migrated vertically between day and night. Biomass in the oxygen minimum zone (OMZ) was high.en_US
dc.description.sponsorshipThe Federal Ministry of Education and Research (BMBF)en_US
dc.language.isoenen_US
dc.publisherWASCALen_US
dc.subjectZooplanktonen_US
dc.subjectDiurnal Vertical Migrationen_US
dc.subjectAbundanceen_US
dc.subjectBiomassen_US
dc.titleVertical Migration and Distribution of Zooplankton along a Latitudinal Transect in the Eastern North Atlanticen_US
dc.typeThesisen_US
Appears in Collections:Climate Change and Marine Science - Batch 3

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