Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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| + | == WHAT HAPPENS WHEN THE OCEAN IS OVERHEATED? == | ||
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| + | [[Image:JFR_cover.gif|left|80px| ]]<font size="2">The global warming and major perturbation of the global carbon cycle that occurred during the Paleocene–Eocene Thermal Maximum (PETM) have been investigated in the lower bathyal–upper abyssal Alamedilla section (Spain). Geochemical anomalies and dramatic faunal changes (including the globally recognized extinction event of deep-sea benthic foraminifera and the rapid evolutionary turnover of planktic foraminifera and calcareous nannofossils) are associated with the PETM at Alamedilla....Significant changes in foraminiferal test size are documented across the PETM. | ||
| + | <font size="2">(from [http://gsabulletin.gsapubs.org/content/122/9-10/1616.abstract?sid=94064967-419e-4184-a942-f8183f09bf3c ABSTRACT]) | ||
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| + | Alegret, L., Ortiz, S., Arenillas, I., Molina, E., 2010. [http://gsabulletin.gsapubs.org/content/122/9-10/1616.abstract?sid=94064967-419e-4184-a942-f8183f09bf3c What happens when the ocean is overheated? The foraminiferal response across the Paleocene–Eocene Thermal Maximum at the Alamedilla section (Spain)]. Geological Society of America Bulletin, Vol. 122 (9/10), 1616-1624. | ||
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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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