Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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| + | ==MIDDLE MIOCENE WARM-TEMPERATE CARBONATES OF CENTRAL PARATETHYS (MT. ZRINSKA GORA, CROATIA): PALEOENVIRONMENTAL RECONSTRUCTION== | ||
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| + | Carbonate deposits from Zrin in the Mt. Zrinska Gora were deposited in the SW part of the Central Paratethys Sea during the Middle Badenian (Middle Miocene). The studied section contains a rich fossil community of non-geniculate coralline red algae (Subfamily Melobesioideae), bryozoans, benthic and planktonic foraminifera, echinoderms, ostracods, molluscs, and calcareous nannoplankton. Based on lithological variations and changes in the biogenic components, four facies associations (FA) are distinguished. Their distribution points to skeletal production and sedimentation on a middle to proximal outer carbonate ramp. The main lithological feature of the section is an alternation of two lithofacies: fully lithified grainstone–rudstone and packstone, and semi-lithified rudstone–floatstone with a carbonate sandy matrix. ...... | ||
| + | <font size="2">([http://link.springer.com/article/10.1007/s10347-012-0327-z ABSTRACT]) | ||
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| + | ----Martinuš, M., Fio, K., Pikelj, K., Aščić, Š., 2013. [http://link.springer.com/article/10.1007/s10347-012-0327-z Middle Miocene warm-temperate carbonates of Central Paratethys (Mt. Zrinska Gora, Croatia): paleoenvironmental reconstruction based on bryozoans, coralline red algae, foraminifera, and calcareous nannoplankton]. Facies, 59(3), 481-504. | ||
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==TRACE ELEMENT POLLUTION - THE CASE STUDY OF THE GULF OF MILAZZO, NE SICILY== | ==TRACE ELEMENT POLLUTION - THE CASE STUDY OF THE GULF OF MILAZZO, NE SICILY== | ||
