@article {2075,
	title = {Dating Borneo{\textquoteright}s Deltaic Deluge: Middle Miocene progradation of the Mahakam Delta},
	journal = {Palaios},
	year = {In Press},
	author = {Nathan Marshall and Vibor Novak and Irfan Cibaj and Wouter Krijgsman and Willem Renema and Jeremy Young and Nicholas Fraser and Alexander Limbong and Morley, Robert J.}
}
@article {2056,
	title = {Diversity and paleoecology of Miocene coral-associated mollusks from East 	Kalimantan (Indonesia)},
	journal = {Palaios},
	year = {Submitted},
	author = {Aires Kusworo and Sonja Reich and Frank P. Wesselingh and Nadiezhda Santodomingo and Kenneth G. Johnson and Jonathan A. Todd and Willem Renema}
}
@article {2053,
	title = {Larger foraminifera as environmental discriminators in Miocene mixed carbonate-siliciclastic systems},
	journal = {Palaios},
	year = {In Press},
	author = {Vibor Novak and Willem Renema}
}
@article {2044,
	title = {Age of Neogene fossil localities in the Northern Kutei Basin},
	journal = {Palaios},
	year = {Submitted},
	author = {Willem Renema and Viola Warter and Nathan Marshall and Vibor Novak}
}
@article {2043,
	title = {Paleoecological significance of stable isotope ratios in Miocene tropical shallow marine habitats (Indonesia)},
	journal = {Palaios},
	year = {In Press},
	author = {Sonja Reich and Viola Warter and Frank P. Wesselingh and H. Zwaan and Willem Renema and Lucas Lourens}
}
@article {2042,
	title = {Late Miocene seasonal to sub-decadal climate variability in the Indo-West Pacific (East Kalimantan, Indonesia) preserved in giant clams},
	journal = {Palaios },
	year = {In Press},
	author = {Viola Warter and Wolfgang M{\"u}ller and Frank P. Wesselingh and Jonathon A. Todd and Willem Renema}
}
@article {2040,
	title = {Coralline Algae from the Miocene Mahakam Delta (East Kalimantan, SE Asia)},
	journal = {Palaios},
	year = {In Press},
	abstract = {<p>Miocene crustose coralline algae (CCA) from the South East Asia are poorly known, although the Miocene is the epoch of the onset of the biodiversity hotspot in the region and CCA are crucial to understand the evolutionary history of reef building. To fill this knowledge gap, CCA from Lower and Middle Miocene reefs and related carbonates in the Kutai Basin in East Kalimantan (Borneo, Indonesia) have been studied. The Kutai Basin was dominated by siliciclastic sediments of the Proto-Mahakam delta and only locally carbonate buildups occur laterally to or within the deltaic succession. CCA in the Kutai Basin occur in low-energy shallow-water platform carbonates and in association with coral reefs, encrusting the corals or bioclasts. Two main CCA assemblages have been recognized: 1) A shallow-water assemblage (S-assemblage), dominated by Neogoniolithon spp., thick crusts of Spongites spp., and Hydrolithon spp.; and 2) the D-assemblage, mainly consisting of thin crusts of Lithothamnion spp., Mesophyllum spp., and Sporolithon spp., which grew in darker waters. Light reduction in reefs in the Proto-Mahakam delta was due to increased water depth or higher turbidity by higher siliciclastic input. Assemblages with intermediate composition (I-assemblages) can also be found. Common CCA with large cells fusions and groups of heterocysts, typical features of modern reef CCA, in the S-assemblages in the Middle Miocene of East Kalimantan reflect the initiation of the reef-building CCA flora in the Indo-Pacific region. The occurrence of this kind of CCA confirms the biogeographic differentiation of a tropical reef flora.</p>
},
	author = {Anja R{\"o}sler and Vedrana Pretkovi{\'c} and Vibor Novak and Willem Renema and Juan C. Braga}
}
@article {2038,
	title = {Bryozoan diversity in the Miocene of the Kutai Basin, East Kalimantan, Indonesia},
	journal = {Palaios},
	year = {Submitted},
	abstract = {<p>Miocene bryozoans from the Indonesian Archipelago have been poorly investigated in the past. Several factors combine to explain their poor fossil record, including difficulties in locating good exposures in areas characterized by lush vegetation, dominance of inconspicuous encrusting species, and the adverse effects of diagenesis on fossil preservation. A large collection of samples from the Kutai Basin (East Kalimantan) made during the Marie Curie Initial Training Network \&lsquo;Throughflow\&rsquo; has allowed new insights into the diversity of Miocene bryozoans in this region. The bryozoan assemblage as a whole consists of 123 species, which represents a remarkable increase in diversity compared to previous knowledge. Substrate availability appears to be the main factor controlling bryozoan distribution, the majority of encrusting species being associated with plate-like scleractinian corals. Collecting curves allow sampled sites to be divided into three groups characterized by high, medium and low species richness. The site of highest diversity is a mesophotic reef slope, environment influenced by strong input of terrigenous sediment. Ordination plots show no clear patterns of distribution among sites, with putatively endemic species accounting for most of the discrimination. A similar level of endemism and habitat heterogeneity characterizes modern, tropical bryozoan faunas. However, many more intermediate sites need to be sampled to achieve a fuller understanding of the true pattern of bryozoan species distribution in the Miocene of the Kutai Basin.</p>
},
	keywords = {abundance, growth-forms, preservation, Richness, substrates},
	author = {Emanuela Di Martino and Paul D. Taylor and Kenneth G. Johnson}
}
@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}
}
