DOI: 10.1016/j.palaeo.2013.01.009
论文题名: Environmental reconstruction of a late Burdigalian (Miocene) patch reef in deltaic deposits (East Kalimantan, Indonesia)
作者: Novak V. ; Santodomingo N. ; Rösler A. ; Di Martino E. ; Braga J.C. ; Taylor P.D. ; Johnson K.G. ; Renema W.
刊名: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182
出版年: 2013
卷: 374 起始页码: 110
结束页码: 122
语种: 英语
英文关键词: Bryozoans
; Coralline algae
; Corals
; Larger benthic foraminifera
; Miocene
; Patch reef
英文摘要: Most studies of Cenozoic shallow-water, mixed carbonate-siliciclastic depositional systems have focused on their sedimentology. To date, however, comprehensive analyses of biotas and biofacies of Indo-West Pacific reefs that developed in mixed carbonate-siliciclastic systems are lacking. This study describes the palaeoenvironment and biodiversity of a late Burdigalian patch reef that developed in a mixed carbonate-siliciclastic depositional system. The studied exposure is located at the northeast margin of the Kutai Basin near Bontang (Indonesia), and is approximately 80. m wide and 25. m thick. Multi-taxon analysis of the most abundant fossil groups, including larger benthic foraminifera, corals, coralline algae, and bryozoans, aims to provide a model for environmental interpretation that will allow comparison with similar deposits of Indo-West Pacific region. Based on fossil content and lithology, five different facies types have been distinguished: foraminiferal packstone (FP), bioclastic packstone with foralgal communities (BP), thin-platy coral sheetstone (CS), platy-tabular coral platestone (CP), and shales (S). Among larger benthic foraminifera, smaller and more robust forms dominate in the FP and BP facies, while larger and flatter forms are the most abundant in the CS and CP facies. Thin-platy corals are dominant in the CS facies and gradually change into thicker platy-tabular forms in the CP facies. Assemblages and growth forms of coralline algae show no major differences between the facies types and are dominated by melobesioids and Sporolithon. The majority of bryozoan species are encrusting and were found only in the CS facies. Light-dependent organisms occurring in the reef indicate low light conditions typical for mesophotic reefs. The relatively small size of this reef complex and quite distinct vertical changes in the facies types, combined with the high siliciclastic content in most of the units, points to strong terrigenous input affecting water transparency as the main factor controlling the reef growth. © 2013 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/69789
Appears in Collections: 过去全球变化的重建
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作者单位: Department of Geology, Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, Netherlands; Department of Earth Sciences, Natural History Museum, Cromwell Road, SW7 5BD London, United Kingdom; Departamento de Estratigrafía y Paleontología, Universidad de Granada, Campus Fuente Nueva s/n, 18002 Granada, Spain
Recommended Citation:
Novak V.,Santodomingo N.,Rösler A.,et al. Environmental reconstruction of a late Burdigalian (Miocene) patch reef in deltaic deposits (East Kalimantan, Indonesia)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2013-01-01,374