Cold-water coral habitats of Rockall and Porcupine Bank, NE Atlantic Ocean: Sedimentary facies and benthic foraminiferal assemblages

被引:15
|
作者
Smeulders, G. G. B. [1 ,2 ]
Koho, K. A. [1 ,2 ]
de Stigter, H. C. [1 ]
Mienis, F. [1 ]
de Haas, H. [1 ]
van Weering, T. C. E. [1 ,3 ]
机构
[1] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Netherlands
[2] Univ Utrecht, Fac Geosci, NL-3584 CD Utrecht, Netherlands
[3] Vrije Univ Amsterdam, Fac Earth & Environm Sci, NL-1085 HV Amsterdam, Netherlands
关键词
Carbonate mounds; Bioherms; Cold-water corals; Benthic foraminifera; Fossil assemblages; Sedimentary facies; NE Atlantic; Porcupine; Rockall; CARBONATE-MOUND DEVELOPMENT; MEDITERRANEAN OUTFLOW; DIAGENETIC PROCESSES; ACCUMULATION RATES; TROUGH MARGINS; ORGANIC-CARBON; DEEP; BIOLOGY; GROWTH; WEST;
D O I
10.1016/j.dsr2.2013.10.001
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The extent of the cold-water coral mounds in the modern ocean basins has been recently revealed by new state-of-the-art equipment. However, not much is known about their geological extent or development through time. In the facies model presented here seven different types of seabed substrate are distinguished, which may be used for reconstruction of fossil coral habitats. The studied substrates include: off-mound settings, (foram) sands, hardgrounds, dead coral debris, and substrates characterized by a variable density of living coral framework. Whereas sediment characteristics only provide a basis for distinguishing on- and off-mound habitats and the loci of most prolific coral growth, benthic foraminiferal assemblages are the key to identifying different mound substrates in more detail. Specific foraminiferal assemblages are distinguished that are characteristic of these specific environments. Assemblages from off-mound settings are dominated by (attached) epifaunal species such as Cibicides refulgens and Cibicides variabilis. The attached epibenthic species Discanomalina coronata is also common in off-mound sediments, but it is most abundant where hardgrounds have formed. In contrast, the settings with coral debris or living corals attract shallow infaunal species that are associated with more fine-grained soft sediments. The typical 'living coral assemblage' is composed of Cassidulina obtusa, Bulimina marginata, and Cassidulina laevigata. The abundance of these species shows an almost linear increase with the density of the living coral cover. The benthic foraminifera encountered from off-mound to top-mound settings appear to represent a gradient of decreasing current intensity and availability of suspended food particles, and increasing availability of organic matter associated with fine-grained sediment trapped in between coral framework. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:270 / 285
页数:16
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