Impact of organic matter source and quality on living benthic foraminiferal distribution on a river-dominated continental margin: A study of the Portuguese margin

Type Article
Date 2016-06
Language English
Author(s) Dessandier Pierre-AntoineORCID1, Bonnin Jerome1, Kim Jung-Hyun2, 3, Bichon SabrinaORCID1, Deflandre Bruno1, Gremare Antoine1, Damste Jaap S. Sinninghe2
Affiliation(s) 1 : Univ Bordeaux, UMR EPOC CNRS 5805, Pessac, France.
2 : NIOZ Royal Netherlands Inst Sea Res, Den Burg, Netherlands.
3 : Hanyang Univ ERICA Campus, Dept Marine Sci & Convergence Technol, Ansan, South Korea.
Source Journal Of Geophysical Research-biogeosciences (2169-8953) (Amer Geophysical Union), 2016-06 , Vol. 121 , N. 6 , P. 1689-1714
DOI 10.1002/2015JG003231
WOS© Times Cited 16
Keyword(s) benthic foraminiferal ecology, fluvial influence, organic matter quality, Portuguese margin
Abstract Living (rose Bengal stained) benthic foraminifera were investigated on surface sediments from 23 stations from the river-dominated northwestern Portuguese margin. Samples were collected in March 2011, following the period of the maximum rainfall over the Iberian Peninsula, between 20 and 2000m water depth along five cross-margin transects. Four of them are located off the Douro, Mondego, Tagus, and Sado Rivers and one off the Estremadura coast. The major objectives of this study are (1) to assess the impact of organic matter of various origin and quality on the benthic foraminifera and (2) to investigate the spatial differences of faunal distribution from coastal waters to the deep sea under river influences. To do this, sedimentological and biogeochemical characteristics of the sediments were identified by measuring grain size, oxygen penetration depth, total organic carbon (TOC) content, stable carbon isotopic composition of TOC (C-13(TOC)) and concentration of pigments and amino acids. Based on the principal component and cluster analyses of the environmental data, three major geographical groups are identified: (1) deep stations, (2) coastal and middle slope stations, and (3) shelf stations under river influence. At the deepest stations, species are associated with high organic matter (OM) quantity but low OM quality, where Uvigerina mediterranea, Hoeglundina elegans, and agglutinated species such as Reophax scorpiurus or Bigenerina nodosaria are dominant. All stations off the Sado River, which is the most affected area by the anthropogenic influence, are also characterized by high quantity but low quality of OM with the minimum faunal density and diversity within the study area. Middle slope stations are associated with low OM content and coarse sediments (Q(50)) with the predominance of N. scaphum. Shallow shelf stations close to the Douro and Tagus River mouths show a dominance of taxa (e.g., Ammonia beccarii, Bulimina aculeata, Eggerelloides scaber, Nonion scaphum, Cancris auriculus, and Quinqueloculina seminula) adapted to environments characterized by high OM quality (high fresh chlorophyll (Chl a/Phaeo)) and available amino acids (enzymatically hydrolyzable amino acid (EHAA)/total enzymatically hydrolyzable amino acid (THAA)). The Biotic and Environmental linking analysis suggests that the benthic foraminiferal distribution is mostly controlled by three environmental parameters, i.e., TOC (quantity), EHAA/THAA (quality), and C-13(TOC) (source). Hence, this study clearly highlights that the quantitative and qualitative inputs of OM and its source are the most important factors controlling the living benthic foraminiferal distribution with clear influences between the different rivers. This study also suggests a good tolerance of several species for river discharges where the OM quality is high.
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Dessandier Pierre-Antoine, Bonnin Jerome, Kim Jung-Hyun, Bichon Sabrina, Deflandre Bruno, Gremare Antoine, Damste Jaap S. Sinninghe (2016). Impact of organic matter source and quality on living benthic foraminiferal distribution on a river-dominated continental margin: A study of the Portuguese margin. Journal Of Geophysical Research-biogeosciences, 121(6), 1689-1714. Publisher's official version : , Open Access version :