Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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----Caruthers, A.H., Smith, P.L. and Gröcke, D.R., 2013. [http://www.sciencedirect.com/science/article/pii/S0031018213002344 The Pliensbachian–Toarcian (Early Jurassic) extinction, a global multi-phased event]. Palaeogeography, Palaeoclimatology, Palaeoecology 386, 104-118. | ----Caruthers, A.H., Smith, P.L. and Gröcke, D.R., 2013. [http://www.sciencedirect.com/science/article/pii/S0031018213002344 The Pliensbachian–Toarcian (Early Jurassic) extinction, a global multi-phased event]. Palaeogeography, Palaeoclimatology, Palaeoecology 386, 104-118. | ||
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| + | ==THE MORPHOGROUPS OF FORAMINIFERA FROM THE DEVONIAN CARBONATE COMPLEX OF THE PRAGUE SYNFORM, CZECH REPUBLIC== | ||
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| + | [[Image:PPP_front.gif |left|80px|]]<font size="2"> | ||
| + | Agglutinated foraminifera from the Lower and lower part of the Middle Devonian, predominantly limestones of the Prague Synform (Barrandian area), were classified into five morphogroups ...... The absence of the deep infaunal morphogroups is characteristic. The morphogroup distribution has been strongly affected by oxygen concentration, the energy of the environment, nutrient availability and post-mortem processes. Intervals with diversified and abundant foraminiferal assemblages can be correlated with positive δ<sup>13</sup>C excursions and also with the deposition of nodular limestones. The Devonian assemblages from the Prague Synform were compared with isochronous assemblages from other regions. Though the taxonomical composition of the Early Devonian assemblages from these areas are rather different, the morphogroup composition is highly comparable, and globally indicates similar life and feeding strategies of the Early Devonian foraminifera. | ||
| + | <font size="2">([http://www.sciencedirect.com/science/article/pii/S0031018213002551 ABSTRACT]) | ||
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| + | ----Holcová, K. and Slavík, L., 2013. [http://www.sciencedirect.com/science/article/pii/S0031018213002551 The morphogroups of small agglutinated foraminifera from the Devonian carbonate complex of the Prague Synform, (Barrandian area, Czech Republic)]. Palaeogeography, Palaeoclimatology, Palaeoecology 386, 210-224. | ||
