Diversity and Depth Distribution of Modern Benthic Foraminifera Offshore Brunei Darussalam

Author:

Goeting Sulia1,Ćosović Vlasta2,Benedetti Andrea3,Fiorini Flavia4,Kocsis László56,Roslim Amajida5,Briguglio Antonino1

Affiliation:

1. 1 Universita degli Studi di Genova, Dipartimento di Scienze della Terra dell'Ambiente e della Vita, Corso Europa 26, 16132 Genova, Italy

2. 2 University of Zagreb, Department of Geology, Faculty of Science, Horvatovac 102b, 10000 Zagreb, Croatia

3. 3 Universita degli Studi di Modena e Reggio Emilia, Dipartimento di Scienze Chimiche e Geologiche, Via Campi 103, 41125, Modena, Italy

4. 4 Micropress Europe; al. A. Mickiewicza 30, 30-059 Krakow, Poland

5. 5 Universiti Brunei Darussalam, Faculty of Science, Geology Group, Jalan Tungku Link, BE1410, Bandar Seri Begawan, Brunei Darussalam

6. 6 University of Lausanne, Faculty of Geosciences and Environment, Institute of Earth Surface Dynamics.

Abstract

ABSTRACT The distribution of modern benthic foraminifera is studied from offshore mixed carbonate-siliciclastic settings of Brunei Darussalam located in northwestern Borneo (South China Sea). The sediments were collected from 17 sites (i.e., shallow reefs, sunken wrecks, and two depth transects). A total of 231 species were identified from 8 to 63 m water depth. We conducted several analyses to understand the patterns of faunal composition, including: (1) Cluster analysis and Principal Component Analysis together with correlation to define relation among the sites; (2) Diversity indices, such as Shannon Index and Fisher's Alpha Index to assess diversity patterns at sites; and (3) Foram Index (FI) to determine whether the water quality indicates conditions that support reef growth. The most abundant foraminiferal groups from the reef and most wreck samples are larger benthic foraminifera (LBF), especially Calcarinidae and Amphisteginidae, whereas in the muddier sites the most abundant are smaller benthic foraminifera (SBF) with the genera Pseudorotalia and Asterorotalia. Certain species from the groups have shown patterns that do or do not correlate with depth and clay content.

Publisher

GeoScienceWorld

Subject

Paleontology,Microbiology

Reference79 articles.

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3. Agglutinated Foraminifera from Miocene sediments of northwest Borneo;Bidgood,,2000

4. Neogene to Recent Rotaliid Foraminifera from the Indo-Pacific Ocean, their canal system, their classification and their stratigraphic use;Billman,;Schweizerische Palaeontologische Abhandlungen,1980

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