@article {2033, title = {A diverse patch reef from turbid habitats in the Middle Miocene (East Kalimantan, Indonesia)}, journal = {Palaios}, year = {Submitted}, author = {Nadiezhda Santodomingo and Vibor Novak and Vedrana Pretkovi{\'c} and Nathan Marshall and Anja R{\"o}sler and Emanuela Di Martino and Elena LoGiudice and Sonja Reich and Juan Carlos Braga and Willem Renema and Kenneth G. Johnson} } @article {2007, title = {Environmental reconstruction of a late Burdigalian (Miocene) patch reef in deltaic deposits (East Kalimantan, Indonesia)}, journal = {Palaeogeography, Palaeoclimatology, Palaeoecology}, volume = {374}, year = {2013}, pages = {110-122}, abstract = {

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.

}, doi = {http://dx.doi.org/10.1016/j.palaeo.2013.01.009}, author = {Vibor Novak and Nadiezhda Santodomingo and Anja R{\"o}sler and Emanuela Di Martino and Juan Carlos Braga and Paul D Taylor and Kenneth G. Johnson and Willem Renema} } @conference {1981, title = {Palaeoenvironmental reconstruction of a Miocene patch reef in East Kalimantan (Indonesia): a close-up on the bryozoan component}, booktitle = {IBA Larwood Meeting }, year = {2012}, month = {31/05/2012}, address = {Brno Czech Republic}, author = {Emanuela Di Martino and Paul D. Taylor and Vibor Novak and Nadiezhda Santodomingo and Anja R{\"o}sler and Juan Carlos Braga and Kenneth G. Johnson and Willem Renema} } @conference {1977, title = {Bryozoans from a Langhian patch reef in East Kalimantan (Indonesia)}, booktitle = {Giornate di Paleontologia XII edizione {\textendash} Catania, 24-26 Maggio 2012 }, year = {2012}, month = {24/05/2012}, address = {Catania, Italy}, author = {Emanuela Di Martino and Paul D. Taylor and Vibor Novak and Nadiezhda Santodomingo and Anja R{\"o}sler and Juan Carlos Braga and Kenneth G. Johnson and Willem Renema} } @article {1626, title = {Hopping Hotspots: global shifts in marine biodiversity}, journal = {Science}, volume = {321}, year = {2008}, pages = {654-657}, author = {Willem Renema and Bellwood, D. R. and Juan Carlos Braga and Bromfield, K. and Hall, R. and Kenneth G. Johnson and Lunt, P. and Meyer, C. P. and McMonagle, L. B. and Morley, R. J. and O{\textquoteright}dea, A. and Jonathan A. Todd and Frank P. Wesselingh and Wilson, M. E. J. and Pandolfi, J. M.} }