Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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== JURASSIC VENT FORAMINIFERA == | == JURASSIC VENT FORAMINIFERA == | ||
| − | [[Image:Recurvoides.infernus.jpg|left|80px| ]]<font size="3">''Recurvoides infernus'' sp. nov., one of the oldest representatives of the superfamily Recurvoidacea (Foraminifera), is described from a | + | [[Image:Recurvoides.infernus.jpg|left|80px| ]]<font size="3">''Recurvoides infernus'' sp. nov., one of the oldest representatives of the superfamily Recurvoidacea (Foraminifera), is described from a black claystone overlying the manganese deposits in the Western Tatra Mountains (Poland). These manganese carbonates/silicates were laid down around a shallow−water exhalative submarine hydrothermal vent that was active in the early Toarcian. The microfossils are possibly the first described Jurassic foraminifera associated with hydrothermal vents <font size="2">(from [http://www.app.pan.pl/article/item/app20090082.html ABSTRACT]). |
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<font size="2">Tyszka, J., Jach, R., and Bubík, M. 2010. [http://www.app.pan.pl/article/item/app20090082.html A new vent−related foraminifer from the lower Toarcian black claystone of the Tatra Mountains, Poland]. Acta Palaeontologica Polonica 55 (2): 333–342 [http://www.app.pan.pl/archive/published/app55/app20090082.pdf '''PDF'''] | <font size="2">Tyszka, J., Jach, R., and Bubík, M. 2010. [http://www.app.pan.pl/article/item/app20090082.html A new vent−related foraminifer from the lower Toarcian black claystone of the Tatra Mountains, Poland]. Acta Palaeontologica Polonica 55 (2): 333–342 [http://www.app.pan.pl/archive/published/app55/app20090082.pdf '''PDF'''] | ||
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== GEOCHEMICAL PROXIES IN FORAMINIFERA == | == GEOCHEMICAL PROXIES IN FORAMINIFERA == | ||
