Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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{{Recent Publications on Foraminifera Navigation}}<font size="2"> | {{Recent Publications on Foraminifera Navigation}}<font size="2"> | ||
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| + | ==MIDDLE EOCENE ABYSSAL BENTHIC FORAMINIFERA IN THE EASTERN EQUATORIAL PACIFIC== | ||
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| + | [[Image:Journal_Of_Paleontology_cover.jpg |left|80px|]]<font size="2"> | ||
| + | We report on the faunal transition of benthic foraminifera during the middle Eocene at Site U1333 (4862 m water depth, 3,560–3,720 m paleo-water depth) of Integrated Ocean Drilling Program Expedition 320 in the eastern equatorial Pacific Ocean. ...... Based on Q-mode cluster analysis, four sample clusters were recognized and their stratigraphic distributions were generally discriminated in the lower and upper parts of the study interval. Thus, there was only a small faunal transition in the abyssal eastern equatorial Pacific during the middle to late-middle Eocene. The faunal transition recognized in this study may be related to recovery processes following intense carbonate corrosiveness in the eastern equatorial Pacific during MECO. | ||
| + | <font size="2">([http://www.psjournals.org/doi/abs/10.1666/12-107 ABSTRACT]) | ||
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| + | ----Takata, H., Nomura, R., Tsujimoto, A. and Khim, B.-K., 2013. [http://www.psjournals.org/doi/abs/10.1666/12-107 Abyssal Benthic Foraminifera in the Eastern Equatorial Pacific (IODP Exp 320) During the Middle Eocene]. Journal of Paleontology 87 (6), 1160-1185. | ||
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==MOLECULAR EVIDENCE FOR LESSEPSIAN INVASION OF SORITIDS== | ==MOLECULAR EVIDENCE FOR LESSEPSIAN INVASION OF SORITIDS== | ||
