Live (stained) benthic foraminifera from the Rhone prodelta (Gulf of Lion, NW Mediterranean): Environmental controls on a river-dominated shelf

被引:92
|
作者
Goineau, A. [1 ,2 ]
Fontanier, C. [1 ,2 ]
Jorissen, F. J. [1 ,2 ]
Lansard, B. [3 ,4 ]
Buscail, R. [5 ]
Mouret, A. [6 ]
Kerherve, P. [5 ]
Zaragosi, S. [6 ]
Ernoult, E. [1 ,2 ]
Altero, C. [5 ]
Anschutz, P. [6 ]
Metzger, E. [1 ,2 ]
Rabouille, C. [7 ]
机构
[1] Univ Angers, Lab Recent & Fossil Bioindicators BIAF, UPRES EA 2644, F-49045 Angers 01, France
[2] Lab Study Marine Bioindicators LEBIM, F-85350 Ker Chalon, Ile Dyeu, France
[3] McGill Univ, Dept Earth & Planetary Sci, Montreal, PQ H3A 2A7, Canada
[4] GEOTOP, Montreal, PQ, Canada
[5] Univ Perpignan, CNRS, Ctr Format & Rech Environm Marin, UMR 5110, F-66860 Perpignan, France
[6] Univ Bordeaux 1, UMR Environm & Paleoenvironm Ocean EPOC OASU 5805, F-33405 Talence, France
[7] CEA CNRS UVSQ, UMR 1572, LSCE, F-91198 Gif Sur Yvette, France
关键词
Live Benthic Foraminifera; Rhone Prodelta; Ecology; Organic Matter; SEDIMENTARY ORGANIC-MATTER; NORTHERN ADRIATIC SEA; CONTINENTAL-SHELF; OF-MEXICO; IN-SITU; INTERANNUAL VARIABILITY; SEASONAL VARIABILITY; MARINE-SEDIMENTS; CARBON BUDGETS; OCEAN MARGINS;
D O I
10.1016/j.seares.2010.07.007
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
In this paper, we investigate the ecology of live (rose Bengal stained) benthic foraminifera collected at 20 stations ranging from 15 to 100 m depth in the Rhone prodelta (Gulf of Lions, NW Mediterranean). These sites were sampled in September 2006, five months after the Rhone River annual flood. Statistical analyses based on foraminiferal communities (>150 mu m) divide our study area into six main biofacies directly related to environmental conditions. Miliolid species are abundant in the relict prodeltaic lobe which is characterised by sand with low organic matter content. Close to the river mouth, the limited oxygen penetration in the sediment combined with important hydro-sedimentary processes constitute stressful conditions for foraminiferal faunas dominated by opportunistic species (e.g. Leptohalysis scottii). With increasing distance from the river mouth, foraminiferal faunas (e.g. Nonionella turgida, Eggerella scabra) adapted to thrive in sediments enriched in Rhone-derived organic matter under more stable hydrosedimentary conditions appear. In the distal part of the Rhone River influence, benthic species (e.g. Valvulineria bradyana, Textularia agglutinans) living in fine sediment enriched in both continental and marine organic compounds emerge. At the deepest stations located in the south-eastern part of our study area, benthic foraminiferal faunas (e.g. Bulimina aculeata, Melonis barleeanus, Bigenerina nodosaria) are highly diverse, underlining stable environmental conditions characterised by marine-derived organic matter supplies and relatively deep oxygen penetration depth in the sediment. We also compare foraminiferal faunas sampled in September 2006 with communities sampled in June 2005, one month after the Rhone River annual flood (Mojtahid et al., 2009). This comparison suggests that opportunistic species (e.g. B. aculeata, Cassidulina carinata, V. bradyana) have responded to organic matter inputs related to marine primary production in June 2005. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:58 / 75
页数:18
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