Foraminiferal assemblage and statistical analysis of surface sediment samples from the Golfe d'Arguin, Mauritania

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Main Authors: Reymond, Claire E, Mateu-Vicens, G, Westphal, Hildegard
Format: Dataset Open Access
Language:en
Published: PANGAEA 2014
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author Reymond, Claire E
Mateu-Vicens, G
Westphal, Hildegard
author_facet Reymond, Claire E
Mateu-Vicens, G
Westphal, Hildegard
collection Datos científicos de ciencias marinas y ambientales
contents With the growing pressure of eutrophication in tropical regions, the Mauritian shelf provides a natural situation to understand the variability in mesotrophic assemblages. Site-specific dynamics occur throughout the 1200 m depth gradient. The shallow assemblages divide into three types of warm-water mesotrophic foraminiferal assemblages, which is not only a consequence of high primary productivity restricting light to the benthos but due to low pore water oxygenation, shelf geomorphology, and sediment partitioning. In the intermediate depth (approx. 500 m), the increase in foraminiferal diversity is due to the cold-water coral habitat providing a greater range of micro niches. Planktonic species characterise the lower bathyal zone, which emphasizes the reduced benthic carbonate production at depth. Although, due to the strong hydrodynamics within the Golf, planktonic species occur in notable abundances through out the whole depth gradient. Overall, this study can easily be compared to other tropical marine settings investigating the long-term effects of tropical eutrophication and the biogeographic distribution of carbonate producing organisms.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_840556
institution PANGAEA
language en
publishDate 2014
publisher PANGAEA
record_format pangaea
spellingShingle Foraminiferal assemblage and statistical analysis of surface sediment samples from the Golfe d'Arguin, Mauritania
Reymond, Claire E
Mateu-Vicens, G
Westphal, Hildegard
Center for Marine Environmental Sciences; Leibniz Centre for Tropical Marine Research; MARUM; ZMT
With the growing pressure of eutrophication in tropical regions, the Mauritian shelf provides a natural situation to understand the variability in mesotrophic assemblages. Site-specific dynamics occur throughout the 1200 m depth gradient. The shallow assemblages divide into three types of warm-water mesotrophic foraminiferal assemblages, which is not only a consequence of high primary productivity restricting light to the benthos but due to low pore water oxygenation, shelf geomorphology, and sediment partitioning. In the intermediate depth (approx. 500 m), the increase in foraminiferal diversity is due to the cold-water coral habitat providing a greater range of micro niches. Planktonic species characterise the lower bathyal zone, which emphasizes the reduced benthic carbonate production at depth. Although, due to the strong hydrodynamics within the Golf, planktonic species occur in notable abundances through out the whole depth gradient. Overall, this study can easily be compared to other tropical marine settings investigating the long-term effects of tropical eutrophication and the biogeographic distribution of carbonate producing organisms.
title Foraminiferal assemblage and statistical analysis of surface sediment samples from the Golfe d'Arguin, Mauritania
topic Center for Marine Environmental Sciences; Leibniz Centre for Tropical Marine Research; MARUM; ZMT
url https://doi.org/10.1594/PANGAEA.840556