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Late Eocene through...
Late Eocene through Oligocene calcareous nannofossils from the paleo-equatorial Pacific Ocean – taxonomy, preservation history, biochronology and evolution
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- Blaj, Teodora, 1979- (author)
- Stockholms universitet,Institutionen för geologi och geokemi,Marine Geosciences
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- Backman, Jan, Professor (thesis advisor)
- Stockholms universitet,Institutionen för geologi och geokemi
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- Henderiks, Jorijntje, Associate Professor (thesis advisor)
- Stockholms universitet,Institutionen för geologi och geokemi
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- Raffi, Isabella, Associate Professor (thesis advisor)
- Chieti University, Italy
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- Bown, Paul, Senior Lecturer (opponent)
- Department of Earth Sciences, University College London, UK
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(creator_code:org_t)
- ISBN 9789171558909
- Stockholm : Department of Geology and Geochemistry, Stockholm University, 2009
- English 26 s.
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Series: Meddelanden från Stockholms universitets institution för geologi och geokemi, 1101-1599 ; 334
- Related links:
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https://su.diva-port... (primary) (Raw object)
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Abstract
Subject headings
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- This study aims to unravel the ecological and evolutionary dynamics within the calcareous nannofossil communities at the Eocene/Oligocene (E/O) transition and during the Oligocene time when Cenozoic 'icehouse' conditions were established. The main question this study aims to answer is whether the changes in the nannofossil assemblages were controlled by intrinsic evolutionary trends or if the changes were controlled by environmental factors such as changes in temperature and nutrient availability in the surface water. These questions are addressed with detailed analyses of the taxonomy, biostratigraphy and fluctuations in abundance and diversity of calcareous nannofossil assemblages from a continuous latest Eocene through Oligocene sediment section from the ODP Site 1218 (8°53.38´N, 135°22.00´W), paleo-equatorial Pacific Ocean. An improved nannofossil taxonomy and biostratigraphy has been established. At the E/O transition, changes in the nannofossil preservation mimics changes in calcium carbonate content. A detailed investigation of late Eocene and Oligocene sediments yields age estimates for ten nannofossil bioevents. Morphometric studies of the Reticulofenestra umbilicus-R. hillae show that these cannot be subdivided into two different morphospecies. Based on different morphometry and stratigraphic ranges, the Oligocene Sphenolithus lineage appears to be the result of a combined anagenetic and cladogenetic evolution. A new nannolith species is described: Triquetrorhabdulus longus. High-resolution nannofossil data indicate changes in the composition, abundance and diversity of the mid-Oligocene assemblages. Intervals of high diversity index coincide with Oi-glaciation events. However, visual examination of the variations in abundance of nannofossil taxa do not appear to correlate with changes in either oxygen or carbon isotopes. This presumably indicates that a dynamic equilibrium did not exist between these Oligocene nannoplankton assemblages and changes in surface water temperature or productivity conditions.
Subject headings
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
Keyword
- marine sediments
- calcareous nannofossils
- late Eocene
- Oligocene
- biochronology
- evolution
- morphometry
- taxonomy
- ODP Leg 199 Site 1218
- paleo-equatorial Pacific Ocean
- Historical geology and palaeontology
- Historisk geologi och paleontologi
- Marine Geoscience
- marin geovetenskap
Publication and Content Type
- vet (subject category)
- dok (subject category)
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