@article {2062,
	title = {Shells from seagrass meadows and 	coral carpets: How isotopic signals can help to distinguish palaeohabitats },
	journal = {The Malacologist},
	year = {2013},
	type = {Presentation at the Molluscan Forum, London, UK},
	author = {Sonja Reich and Frank P. Wesselingh and Viola Warter and Willem Renema}
}
@article {2062,
	title = {Faunal composition and isotopic signals of mollusk shells indicate seagrass meadows in the Miocene of Indonesia},
	journal = {Revista de Estudos A{\c c}oreanos, Book of Abstracts},
	volume = {8},
	year = {2013},
	pages = {169},
	type = {Poster at the World Congress of Malacology, Ponta Delgada, Azores.},
	author = {Sonja Reich and Frank P. Wesselingh and Viola Warter and Willem Renema}
}
@article {2062,
	title = {Gastropods indicate seagrass meadows (at San Salvador, Bahamas)},
	journal = {Revista de Estudos A{\c c}oreanos, Book of Abstracts},
	volume = {8},
	year = {2013},
	pages = {350-351},
	type = {Poster at the World Congress of Malacology, Ponta Delgada, Azores.},
	author = {Sonja Reich}
}
@article {2049,
	title = {V Factor: Volunteers as a bridge between museum scientists and the public},
	journal = {Journal of Natural Science Collections},
	volume = {1},
	year = {2013},
	chapter = {48-58},
	abstract = {<p>V Factor is a new programme at the Natural History Museum in London. It offers volunteers\&nbsp;the chance to work in public view alongside Museum scientists on collection-based research\&nbsp;and curation projects, taking them from visitor to proactive volunteer. It aims to involve a volunteers\&nbsp;project manager, scientists, curators, volunteers and the public in the museum\&rsquo;s research.\&nbsp;Volunteers work alongside scientists on a research project whilst benefiting from a unique, informal and fun learning experience. Visitors are able to observe the processing of\&nbsp;samples and interact with those involved. The management of this volunteer programme is\&nbsp;described in this paper. The pilot project was \&lsquo;Throughflow\&rsquo;; an international study of Southeast\&nbsp;Asian fossil corals as a means to describe the high biodiversity of their ecosystem and the\&nbsp;effects of environmental change. Volunteers have successfully assisted with the cleaning of\&nbsp;specimens so that they may be curated. At the same time, they have been discussing with experts project-related information, collections care, and the role of museums today. The programme\&nbsp;has been continuously evaluated and changed as felt necessary. By March 2013, 45\&nbsp;volunteers were involved. Outcomes have included improved volunteer talent and education\&nbsp;management, excellent assistance with scientific work and novel means of attracting the public\&nbsp;to the museum\&rsquo;s work.</p>
},
	author = {Renee Miller and Kenneth G. Johnson and Ali L. Thomas and Lyndsey G. Douglas and Nadiezhda Santodomingo and Yoke Shum Broom and Therese Avedillo and Cassandra Murray and Theresa Sadler}
}
@article {2029,
	title = {Changes in the Indonesian Throughflow and southeast Asian hydroclimate during the Middle-Miocene Climate Transition},
	journal = {Geophysical Research Abstracts},
	volume = {15},
	year = {2013},
	pages = {9123},
	author = {Frigola Boix, Amanda and Prange, Matthias and Schulz, Michael}
}
@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 = {<p>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.</p>
},
	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}
}
