Skip to content. | Skip to navigation

Personal tools

You are here: Home
4408 items matching your search terms.
Filter the results.
Item type



































New items since



Sort by relevance · date (newest first) · alphabetically
Article Reference 'Cleaning the Egyptian sphinx with a toothbrush': one of the largest Neoterebra (Gastropoda: Conoidea) from the Caribbean Sea needs a name
Located in Library / RBINS Staff Publications 2022
Inproceedings Reference 'Tauw' - an unusual yet durable, silicified rock type from the Maastricht type area.
Located in Library / RBINS Staff Publications
Article Reference 'Vertition' of integumental organs in mites revisited: a case of fluctuating asymmetry
Located in Library / RBINS Staff Publications
Article Reference 'Zonnesponzen' uit het Krijt van Luik-Limburg na bijna 160 jaar opnieuw gevonden
Located in Library / RBINS Staff Publications 2018
Article Reference (U-Th)/He Dating of Supergene Iron (Oxyhydr-)Oxides of the Nefza-Sejnane District (Tunisia): New Insights into Mineralization and Mammalian Biostratigraphy.
Located in Library / RBINS Staff Publications 2021
Article Reference . Impact of Age, Season, and Flowing vs. Stagnant Water Habitat on Avian Influenza Prevalence in Mute Swan (Cygnus olor) in Belgium.
Located in Library / No RBINS Staff publications
Article Reference . Introduction to reproductive modes. In: Martens, K. (ed) Sex and parthenogenesis, evolutionary ecology of reproductive modes in non-marine ostracods
Located in Library / RBINS Staff Publications
Article Reference 2.7 First occurrence of Menoethius monoceros Latreille, 1825 in the Gulf of Tunis (Northern Tunisia) [pp. 243-244 in Siokou, I. et al. "New Mediterranean marine biodiversity records (June 2013)"]
Located in Library / RBINS Staff Publications
Inproceedings Reference 3D and Challenging Materials: Guidelines for Different 3D Digitisation Methods for Museum Collections with Varying Material Optical Properties.
Located in Library / RBINS Staff Publications
Article Reference 3D geobody reconstruction and CO2-origin of Pleistocene travertine deposits in the Ballık area (SW Turkey)
The Denizli Basin in the West Anatolian Extensional Province in western Turkey is well-known for its numerous travertine occurrences. A combined sedimentological, diagenetic and geochemical investigation is executed on the Ece and Faber travertines of the Ballık area, the largest travertine site in the Denizli Basin. The first aim of this study is the reconstruction of a three-dimensional geo-model in combination with a detailed sedimentological description from fabric to lithotype, lithofacies and geobody scale, with a focus on integrating pore-typing. The second aim involves the delineation of the CO2-origin of ancient travertine precipitating waters. Peloidal, phyto and dendritic lithotypes dominate the studied travertines and honeycomb and bacteriform shapes and encrusted bacterial or fungal filaments related to their fabrics suggest a microbial influence. The environment of travertine precipitation evolved from dominantly sub-aqueous, as represented by the sub-horizontal and biostromal reed travertine facies, to dominantly sub-aerial in a thin water film, resulting in the cascade, waterfall and biohermal reed travertine facies. A general progradation of the travertine mound is indicated by the occurrence of stacked waterfall travertines. This results in sigmoidal clinoforms inside a general mound boundary configuration. Strontium and oxygen-carbon isotope signatures of the travertines point to a mixing mechanism of palaeofluids with deeply originated, heavy carbon CO2 with lighter carbon CO2 of shallow origin. These deposits can thus be considered as endogenic travertines. Carbonates of the Lycian Nappes acted as main parent carbon source rocks. The relative contribution of the lighter carbon isotopes is most likely to have originated from organic matter or soil CO2. This study provides a unique three-dimensional insight into the Ballık travertine architecture that potentially can be used as an analogue for subsurface travertine reservoirs worldwide and illustrates the importance of the combined use of δ13C and 87Sr/86Sr signatures in the delineation of the CO2-origin of travertine precipitating waters.
Located in Library / No RBINS Staff publications